^9§ / ^ / THE RESOURCES OF CALIFOMIA: COMPKISINCh |igri.ralttt«, Pirattg, €l:^x^\l €lm\it, fy\mtm, h,, PAST AND FUTURE DEVELOPMENT OF THE STATE. By JOHN S. HITTELL. FIFTH EDITIOiT, WITH AN APPENDIX ON OKEGOS, NEVADA, AND WASHISGTOJf TERRITORY. ^^ . ^'■" 1^ SAX FRANCISCO : A. ROMAN^ AN^D C0MPA:N'Y. NEW YORK : 27 HOWARD STREET. . 1869. £5 Co^^^'A Entered according to Act of Congress, in the year, 1869, by A. Roman & Co., Proprietors, in the Clerk's Office of the District Court of the United States, for the Northen? District of California. By tranef^r frem. fat. Office Lib. April 1G14. M'CUKA k MILLER, BTEEKOTTPEKft. PEEFAOE. I (JNDERTAKE to write tlie resources of a state, wMcli, tliough young in years, small in popiilation, and remote from the chief centres of civilization, is yet known to the furthest corners of the earth, and, during the last twelve years, has had an influence upon the course of human life, and the prosperity and trade of nations, more powerful than that exerted during the same period by kingdoms whose subjects are numbered by millions, whose history dates back through thousands of years, and whose present stock of wealth beo^an to accumulate before our continent was discovered, or our language was formed. I write of a land of wonders. I write of California, which has astonished the world by the great migration that suddenly built up the first large Caucasian community on the shores of the North Pacific ; by her vast yield of gold, amounting within thirteen years to $700,000,000, which has sensibly affected the markets of labor and money in all the leading nations of Christendom ; by the rapid development and great extent of her commerce ; by the greatness of her chief port, which at one time had more large ships at her anchorage than were ever seen together in the harbor of either Liverpool, New York, or London ; by the swift settlement of her remote districts ; by the prompt organization of her government ; IV PREFACE. by the liberality with, which the mines were thrown open. and made free to all comers ; by the rush of adventurers of every color and of every tongue ; by the prices of her labor, and the rates of her interest for mone}^, double those of the other American states, and quadruple those of Europe ; by the vast extent of her gold-fields, and the facility with which they could be worked ; by the auriferous rivers in which fortunes could be made in a week ; by antediluvian streams richer than those of the present era ; by beds of lava, which, after filling up the beds of antediluvian rivers, were left, by the washing away of the banks and adjacent plains, to stand as mountains, marking the position of great treasures beneath ; by nuggets each worth a fortune ; by the peculiar nature of her mining industry ; by new and strange inventions ; by the washing down of mountains ; by filling the rivers of the Sacramento basin with thick mud throughout the year ; by lifting a hundred mountains from their beds ; by six thousand miles of mining ditches ; by aqueducts less durable, but scarcely less w^onderful than those of ancient Eome ;' by silver mines that promise to rival those of Peru; by quicksilver mines surpassing those of Spain ; by great deposits of sulphur and asphal- tum ; by lakes of borax ; by mud volcanoes, geysers, and natural bridges ; by a valley of romantic and sublime beauty, shut in by walls nearly perpendicular and more than three- quarters of a mile high, with half a dozen great cascades, in one of which the water at two leaps falls more than the third of a mile ; by a climate the most conducive to healthy and the most favorable to mental and physical exertion — so temperate on the middle coast that ice is never seen and thin summer clothing never worn, and that January differs in average temperature only eight degrees of Fahrenheit from July; by a singular botany, including the most splendid known group of coniferous trees, of which half a P REFACE. dozen species grow to be more than two hundred and fifty feet high, and one species has reached a height of four hun- dred and fifty feet, and a diameter of forty feet in the trunk ; by a peculiar zoology, composed chiefly of animals found only on this coast, and including the largest bird north of the equator, and the largest and most formidable quadruped of the continent ; by the importation in early years of all articles of food, and then by the speedy development of agriculture, until her wheat and wine have gone to the furthest cities in search of buyers, and until her markets are unrivalled in the variety and magnificence of home- grown fruits ; by the largest crop of grain, and the largest specimens of fruits and vegetables on record ; by a society where for years there was not one woman to a score of men, and where all the men were in the bloom of manhood ; by the first large migration of eastern Asiatics from their own continent; by the first settlement of Chinamen among white men ; by the entire lack of mendicants, paupers, and alms-houses ; by the rapid fluctuations of trade ; by the ac- cumulation of wealth in the hands of men, most of whom came to the country poor ; by the practice, universal in early years, of going armed ; by the multitude of deadly affrays, and by extra-constitutional courts, which sometimes punished villains with immediate execution, and sometimes proceeded with a gravity and slow moderation that might become the most august tribunals. I write of California while she is still youthful, and full of marvels ; while her population is still unsettled ; while her business is still fluctuating, her wages high, her gold abi:Jndant, and her birth still fresh in the memory of men and women who have scarcely reached their majority ; and I write of her while she still offers a wide field for the adventurous, the enterprising, and the young, who have life before them, and wish to commence it where they may have the freest career, Vi PREFACE. in full siglit of tlie greatest rewards for success, and with the fewest chances of failure. The general public are aware that California is a peculiar state, and their attention has often been called to certain prominent points of wonder, like those to which I have just referred ; but hitherto there has been no careful at- tempt to sum up all that is known of her resources and natural history. I have undertaken that task, and the re- sult of my undertaking is in this book placed before the ■••eader. I have been a Californian since 18^9, and expect to be as long as I may live. All the most interesting as- sociations of my life are connected with this state. I arrived in the country while it was still under a territorial government, and more than a year before it was organized as a state under act of Congress. I saw the land in its original wildness, and saw society, order, trade, industry and polity developed ; and I now see about me the begin- ■ nings and promises of science, art, literature, philosophy, and whatever can enrich or honor humanity. I have seen the state grow up, and its history is part of my life. The land-marks of its chorography, and the prominent events of its political, social, and industrial progress, mark epochs in my memory. Many of the happiest days of my life have been spent here, and here I hope to enjoy whatever blessings the future may have in store for me. If then I fail to do justice in my book to California, the failure will not be for any lack of love of her. Neither will it be for any lack of attention or industry. During the last nine years, I have assiduously collected every thing within my reach relative to the industry, resources, natural history and population of the state. I have looked through all the newspapers published between Crescent City and San Diego, and have examined all the books written about the country, Spanish, French and Grerman, as well as English. I have PREFACE. Vll Deen in the extreme north, and the extreme south ; I have gone to both extremities by land and sea ; I have travelled through the centre of her great basin ; I am intimately ac- quainted with her richest agricultural districts ; I know something of her mining and agriculture by experience and practice ; and, finally, I have endeavored to compress into this book all the important attainable facts. Amidst so much information, there are undoubtedly some little errors ; but the fair critic, before condemning and expatiating upon minor faults, will pass judgment upon the'question whether the book is or is not more comprehensive and instructive than any other, or than all others relating to the same subject. Of course, when I quote from the writings of others, I use quotation marks, and give credit according to the rules of honorable authors ; but I have adopted, without quota- tion marks, various passages from articles written by my- self, and published in different newspapers and magazines. Since the work is intended for popular use, and should be free from every thing not intelligible and interesting to the general reader, I have made no references to authorities ; and, indeed, I have drawn my information from so great a variety of sources (in many instances newspapers), that it would have been very inconvenient for me, and cumber- some to the book, to cite the authority for every statement. In case, however, that the accuracy of any statement in the work should be called in question, I think that I can pro- duce in every case credible evidence, and in most cases the conclusive proof While I have drawn my material from many different sources, I claim as much originality as is possible for so comprehensive a collection of facts, in so many and so distinct branches of knowledge. J. S. H. San Francisco, March, 1862. INTRODUCTION TO THE FOURTH EDITION. 18G ^ 1. Preliminary. — Since the first edition of this book was prepared for the press six years have elapsed, and in that time some progress has been made by the industry of California, and some new light has been thrown upon the resources and physical geography of the State. In this introductory chapter, I shall try to state briefly the main points of tlie additional information obtained since 1862. § 2. The Caliform'an Alps. — The State Geological Survey discovered, in the summer of 1864, that the Sierra Nevada, between latitudes 35° and 38°, has the wonderful mountain region of California. Shasta, which towers in solitary grandeur 7,000 feet above every thing in its vicinity, and shows its mantle of eternal snow to a wide area in three States, is no longer our highest peak. Mt. Whitney, in latitude 36° 30', which is surrounded by so many other peaks of nearly equal height as to attract no special attention from a distance, rises to about 15,000 feet, while Shasta is only 14,440. • Not only is Shasta dethroned, but also Switzerland. The Helvetian Republic has, for hundreds of years, had the fame of possessing the great- est area of elevated land, and the largest number of great peaks within the limit of high civilization, but the newly discovered mountain region surpasses that of Sv/itzerland. That country has only four peaks above 13,000 feet, and not more than 150 square miles above 8,000 feet, while we have LOG peaks above 13,000 feet and 300 or more square miles above 8,000 feet. X INTRODUCTION. This Alpine region of California occupies the upper part of the Sierra Nevada, from Castle Peak to Kern Eiver, a distance of 200 miles ; and throughout that distance all the main peaks rise to 13,000 feet or more. The exact height of Mt. Whitney is not known. The surveying party made two trials to get to the summit, but failed. C. R. King reached an elevation of 14,730 feet, and was there arrested by a precipice. He thought there were 300 or 400 feet of elevation above him. The main Fork and the north Fork of Kern River rise on the southern and western slopes of this mountain, and King's River on its northwestern slope. The main Fork of Kern River runs southward for thirty miles through a tremendous canon, in the upper part of which the river falls 10,000 feet within six miles. A mountain whose summit is six miles east of Mono Lake, and 7,000 feet above it — a pretty steep ascent — is called Mt. Dana. A peak further south, with an elevation of 13,700 feet, is called Mt. Grant ; another of 14,500 feet is called Mt. Tyndall; a third is styled Mt. Brewer. From Castle Peak, in latitude 38°, for a distance of 200 miles along the summit of the Sierra, there is no pass known that can be traversed by a wagon, or less than 11,000 feet in altitude. It would not be safe to assert, however, that no lower pass will be discovered. Much of the range has not yet been examined. Throughout all this Alpine region the views are very extensive, and the scenery grand beyond that of Switzerland, though not so picturesque; that is, not sd beautiful in little places. At some future time it will become a place of great resort for tourists and travelers. § 3. The Great DrougJit— The winters of 1862-63 and 1864-65 proved to be unusually dry, the former bringing only 15|- and the latter only 8^ inches of rain at San Francisco, instead of the average of 21 inches. Two such dry seasons coming together proved very disastrous, and there was a general failure of crops, and a great mortality among cattle. It was esti- mated that out of 3,000,000 horses, neat-cattle, and sheep that were in the State in 1862, 800,000 perished by starvation within two years, and most of those which survived had a very narrow escape. The southern coast couniies suffered most severely, some of them losing two-thirds of their cattle, which were the main stock of their wealth. The year 1865 is known as the year of the great drought, and the native Californians say that at no time within forty years had two consecutive seasons passed with so Httle rain. § 4. The EarthquaJce o/ 1865. —On the Sth October, 1865, San Francisco was visited by an earthquake that surpassed in violence any shock felt here within the recollection of the oldest inhabitants. It occurred on INTRODUCTION. XI Sunday at 12:45, P. M., just about the time when the morning services were being closed in the churches. Two-thirds of the front of a new four-story brick building on the corner of Third and Mission Streets (the mortar of which had not had time to dry) was tlxrown down. Parts of the fire- walls and chimneys of two dozen brick buildings were thrown down. The walls of the City Hall, of the old Merchants' Exchange on Battery Street, of California Engine House on Market Street, the Pennsylvania Engine House on Jackson Street, the Market building at the corner of Pine and Market Streets, besides a multitude of others, were badly cracked. Several wooden buildings which were being raised, and were supported on tem- porary scaffolding or blocks, were thrown down and demohshed. The falling cornices and fire-walls filled some of the streets with dust, and fell on four or five persons, some of whom were seriously hurt, though the injuries did not prove fatal in any case. In those churches where the services were not closed, the people rushed for the doors in a very dis- orderly, manner. § 5. Geological Survey. — A geological survey of the State was com- menced in November, 1860, and continued until 1868, under charge of Prof. J. D. Whitney. He has been assisted by "Wm. M. Gabb, in paleontology, W. H. Brewer and H. X. Bolander in botany, J. G. Cooper in zoology, A. Eemond and Clarence King in general geology, "Wm. Ashburner in economical geology, C. F. Hoffman, V. "Wackenreuder, and J. T. Gardner in topography. The expense of the work has so far been about $140,000. Only two volumes of the report have been published, but others are ready for the press. The following are some of the results of the survey. The coast mountains rose from the sea before the Sierra Nevada, and the latter range was for long after much lower than now ; and a vegeta- tion, different from that which now flourishes here, covered the land. Afterward came a series of great volcanic convulsions ; the Sierra Nevada was lifted up on three successive occasions, separated by long intervals A hundred volcanoes poured- out vast floods of liquid fire and of water mixed with ashes. Mounts Shasta and Lassen, Pilot Peak, Spanish Peak, Old Man Mountain, and Castle Peak, and a multitude of others for which we have no names, were all ablaze at once. There were intervals of rest between their periods of activity, and alternate beds of lava and of alluvial gravel or soil exist on the hills as deposited in what were then valleys or the beds of rivers. An area of not less than 20,000 square miles is now covered with lava. The three periods of upheaval were first at the close of the cretaceous era ; second after the deposition of the raiocene tertiary ; xii INTRODUCTION. . and third after the later pliocene. This last upheaval is supposed to be still in progress. After the volcanic epoch came the glacial epoch, in which glaciers, far grander than any that now exist in the Alps, were found in all the large ravines on the high mountains, where their marks still remain, though the rivers of ice gradually disappeared before the gradually increasing warmth of the climate. The auriferous gravel in the ancient river-oeds was deposited in the later pliocene, and it was followed by a great out- break of volcanic energy, which covered the gravel with beds of lava and other eruptive material. The gold deposits of the State lie not in the silurian rocks, which were previou"sly considered to be the basis of all rich auriferous regions, but in the Jurassic or triassic lithological formations of later date. The coal region of California lies not in the tertiary rocks, as was pre- viously supposed, but in the cretaceous, the highest portion of the sec- ondary era. The limits of the Jurassic and cretaceous have been traced with toler- able accuracy over most of the area of the State. All the principal high points of the State, long known, have been as- cended, their geological character examined, and their precise altitude ascertained. A large district, previously unheard of by the public, has been found to rise to a height of eleven thousand feet or more, with a hundred peaks that rise about thirteen thousand feet, and a general elevation, extent, and grandeur of scenery, that surpass those of Switzerland. The Big Tree has been found to exist, not merely in a few isolated groves, as was supposed, but in extensive forests, with tens of thousands of trees, along a considerable portion of the Sierra Nevada. Large bodies of excellent pasturage were found in places previously un- known to the whites. An extensive collection of minerals, vegetables, and preserved or stuffed animals, has been obtained, and will be prepared for exhibition so soon as the State prepares a proper place for it. § 6. Wheat — Within the last three years much larger crops of wheat have been grown than ever before, and during 1867, San Francisco ex- ported wheat and flour equivalent to 600,000,000 pounds of grain, the sale price here being $12,600,000. The production of barley is about the same as it was seven years ago, while tlie area sown in wheat has increased INTRODUCTION. xiii considerably. Of late, many hills which were before untouched by the plow, have been sown in wheat. § 7. Fruit. — There has been a very slight increase in the number "of apple, pear, and peach orchards since 1862, Gherries have been very profitable near San Francisco, and a multitude of trees have been planted in the vicinity of the bay. It has been found that some trees which thrive in the coast valleys do not thrive in the Sierra Nevada. Mr. "Weatherwax, an orchardist at Mud Springs, El Dorado County, has ascer- tained, by trial, that the Benick is the most profitable apple there, and after it come the Red Romanite, the Red Cheek Pippin, Prior's Red, the BeUeflower and Esopus Spitzenberg. The most profitable pears are the Bartlett, Easter Beurre, Yicar of Wakefield and Winter Nellis. Mr. Nick- erson, of Placer County, obtained, as gross receipts from a year's crop on his best trees, eiglit years old, the following prices, viz. : figs, $75 ; pear, peach, apple and plum, each, $60; apricot, $50, and nectarine, $45. § 8. The Grape. — The number of vineyards has increased greatly with- in five years, especially in the counties north of the bay and in the Sierra Nevada. According to the Report of the Surveyor-General of the State, for 1866, in that year 1,312,730 gallons of wine were made, and there were 15,410,077 grape-vines in vineyard. It is not determined yet, by common consent among wine-growers, what are the best wine grapes, but many of the most intelligent viniculturists think that for light white wines, the best grapes are the Golden Chasselas, the Burger, the White Rhenish Musca- tella, the Riessliug, the Chasselas Fontainebleau, and the White Green ; and for red wine, the Zenfenthal, the Black Malvoisie, the Black Burgundy, the Running Burgundy, Black Cabrunet and the Traminer. For the table, the White Muscat of Alexandria bears the best price ; and for raisins, the White Malaga, called also the Fiherzagos, is preferred. In the first and second editions of The Resources, the largest grape-vine of the State was inadvertently passed over without notice. In 1795 Senora Dorainguez, a native of Mexico, and a resident of Santa Barbara County, rode from Monterey to her home, and before starting she picked up a grape-cutting for a switch. When she had ridden twenty miles she saw that her switch was budding, so she took care of it, and after getting to her house at Montecito, she planted it in the garden. The vine grew, and now its trunk is 15 inches in diameter, and its branches are supported by an arbor 114 feet long and 78 feet wide. Its annual yield of grapes is three or four tons. Senora Dominguez, who planted it, died on the 9th Vfay, 1865, at the age of 105 years, after having given more than 300 XiV INTRODUCTION. children, grand-children, great-grand-children, and great-great-grand-ehild- ren to the State. The vine was watered from a mineral spring, and the old lady said the grapes and the wine from it were better than any others in the neighborhood, and that the superior excellence was due to the mineral water. E. M. Smith, in Coloma, has an Isabella vine which is now in its fifth year, and in 1866 it bore 1,500 bunches of grapes, which weighed 420 pounds. He estimated the yield for 186*7 at 2,500 bunches and 1,000 pounds. I visited the vine and started to count the bunches, but gave it up in despair, and determined to accept Mr. Smith's estimate. The value of the wine exported in 1863 was $19,000 ; in 1864, $41,000 ; in 1S65, $89,000; in 1866, $169,000; and in the first half of 1867, $62,000. § 9. Hop. — The cultivation of the hop on a large scale has been estab- lished with profit. Several fields of cotton, of several hundred acres each, were cultivated for two or three years during the war, but now the busi- ness is less profitable, and most of those who engaged in it have abandoned it. In 1866, 198 bales of Californian cotton were brought to San Francisco, from Tulare and Los Angeles Counties. Flax-seed and the castor-oil are both grown in the State now. § 10. Silk - Worjns. — Extensive fields have been planted with the w-hite mulberry, and the breeding of silk-worms has been commenced on an ex- tensive scale, and a silk factory has been erected at San Jose. It is found that the worms thrive wonderfully well in our climate, and are so heavy that it is sufficient to feed them once a day, by giving them a big supply in the morning. § 11. Quartz Mining. — Quartz mining in California is in a very satis- factory and progressive condition. The number of mines being opened and mills being built is much larger than at any previous time ; and, what is more important, the enterprises now in progress are in the hands of men who, as a class, have more learning, more experience, and more prudence, than those who erected quartz mills before the discovery of the Washoe Mines. All the energy and capital of California were concentrated in silver for four or five years, and we are now just getting to study gold- quartz mining as a regular business. Among the principal quartz mines of the State are the following : — The Princeton Mine, which has produced $4,000,000 ; the Pine Tree and Joseph- ine, which together produced $350,000 from the 1st May, 1860, to the 1st May, 1863; the Mariposa Mine produced $84,948 in 18G4. Those four INTRODUCTION. xT mines are in the Mariposa grant, and have all been idle since 1865, because of mismanagement. The New Britain has yielded $52,000; the Sherman, $200,000; the Hite's Cove yields $150 per ton; and the Potts' Mine, $50,000 annually. In Tuolumne County, the Soulsby yields $100,000 annually; the Piatt has paid $40,000 profit ; the Grizzly has produced $125,000; the Excel- sior, $300,000 ; the Sell & Martin, $150,000 ; the Tennessee, $60,000; the Austrian, $100,000 ; and the Sophia, $45,000 ; the total yield of the App, the Rcist, the Ileslep, and the Golden Rule have not been reported, but they are doing a large amount of work, and are all valuable. The Morgan Mine, on Carson Hill, in Calaveras County (according to the statement of Thomas Dear, who is reputed to have better opportunities of knowing than anybody else), produced $2,800,000 from February, 1850, to December, 1851. Mr. Stevenot, however, who claimed an interest in the mine, though he did not succeed in the courts, says the sum was $1,500,000. At any rate, immense masses of gold were found, and the town of Melones, at the foot of the hill, was the largest mining camp in the State for a time. For sixteen years the title was in litigation and the mine in idleness. Work has been resumed lately. The South Carolina has yielded $400,000; the Reserve, $100,000; the Bovee, $600,000; Hil"s Mine, $250,000; and the Cherokee, $100,000. The Hayward Mine, in Amador County, has been reported to be the most profitable mine in the State. About 24,000 tons are crushed in a year, and there are 120,000 tons in sight. The present supply of ore is obtained 1,200 feet below the surface, and 300 feet below the level of the sea. The total yield, according to rumor, which no doubt exaggerates greatly, has been $6,000,000, The Keystone, a mile and a half distant, pays $80,000 a year in dividends. The Oneida, a mile and a half distant in the other direction, has produced very large sums, and has in sight 90,000 tons of rock, expected to yield about $17 per ton. The total expense is about $5 per ton. The Seaton Mine has yielded $100,000. In El Dorado County, the richest mines have been the Pacific, which has yielded $500,000; the TVoodside, which yielded $12,000, in specimens; the Danes and the Shepard. In Placer County, the Harpending, the Green Emigrant, and the Schnable, are the most notable. In Nevada County, the Eureka, reputed to be the best worked mine in the State, has yield $1,500,000; the North Star, $500,000 profit; the Allison, $2,300,000; the Massachusetts Hill, $5,600,000 ; New York Hill, ivi INTRODUCTION. $500,000; Missouri, HiU, $200,000; the Fellows, $1,000,000; Norambagua, $80,000; Gold Hill, $4,000,000; Union Hill $U, 000; Empire, $1,300,000; Hueston Hill, $1,000,000 ; Osborne Hill, $1,000,000 ; Lone Jack, $500,000 ; Gold Tunnel, $1,000,000; Nevada, $400,000; Sneath & Clay, $300,000; Lecompton, §250,000; Wigham, $200,000, and Banner, $200,000. The Sierra Buttes yielded $224,000 gross, and $154,000 net, in 1866; and has three years' supply of ore in sight. This mine has paid more regularly than any other in the State, and if the milling capacity were increased, could be made to surpass any other mine in the State in yield. The Independence, on the same vein, yielded $100,000, in 1866, and has ore in sight to last three years. The Primrose, two miles distant, has yielded $226,000— idle. The Union, one mile from Alleghany, yielded $75,000 in a pocket. In Plumas County, the Eureka has yielded $1,600,000; the Mammoth, $1,000,000; the Crescent, $500,000; and the Whitney, $68,000. In Yuba County, at Brown's Valley, twelve miles from Marysville, and not more than 300 feet above the level of the sea, are the Pennsylvania, which yields 1,000 tons and $10,000 net per month ; the Jefferson, which has paid $250,000 of dividends ; and the Dannebroge, which has yielded $250,000. § 12. Sulphurets. — Most of the quartz mines, and especially the richer ones, have in the rock from one to five per cent, of sulphurets of iron, which contain from $20 to $1,000 per ton of gold. This can not be ob- tained by amalgamation ; and the only resource is to separate the sulphu- rets (the specific gravity of which is 5,) from the pulverized quartz, (the specific gravity of which is 2^). This separation, called concentration, must be done with the assistance of water. The long sluice is now con- sidered the best machine for concentration. The sluice has a grade of 2 or 3 inches to 12 feet; and riffles half an inch thick are introduced gradu- ally as the boxes fill up, the sand being occasionally stirred with a hoe. "When the sand is eight inches deep, the riffles are gradually removed one by one, and the sand again stirred up ; and in this way the sulphurets are obtained in a very clean state. The sulphurets are then roasted and put into a chlorine bath. The chlorine unites with the gold ; the chloride of gold is dissolved in water; and the gold is precipitated by sulphate of iron. This process costs usually about $20 per ton, although one superintend- ent says the expense, exclusive of his own supervision, is only $9. The cost of concentration is $10 per ton of sulphurets where the rock contains one per cent. INTRODUCTION. xvii § 13. Cement Mills. — Cement mills have been brought into use since 1862. At the bottom of some of the ancient channels, the richest pay is found in a stratum of clay and gravel, so cemented together that it will not dissolve in the sluice ; and the only mode of separating the gold from the dirt, heretofore, has been crushing in a stamp mill. Many of these mills are now in use, and their number is increasing rapidly. The gold is usually coarse in the cement. The material is not so hard as quartz, nor is it crushed so fine ; so the crushing does not usually cost over 50 cents per ton. A pan has lately been invented for reducing cement. It is an iron pan, six feet in diameter, and eighteen inches deep, in which four iron rakes, radiating from the center, each with three strong teeth, revolve rapidly. A large stream of water pours in, and the pulverized stuff is carried off through small holes in the bottom. The large stones are dis- charged through a gate. There are two sluices, one to carry off the stones, and the other to carry off the dissolved clay. § 14. Copper Mining. — Copper mining in California began in 1861, and was very profitable for a time, but the price of the metal has fallen greatly within the last year or two, and copper mining in this State has declined. The amount of ore exported in 1862 was 3,660 tons ; in 1863, -5,553 tons ; in 1864, 10,234 tons; in 1865, lt,78t tons; in 1866, 19,813 tons; and in the first half of 1867, 3,542 tons. Besides this ore, about 200 tons of metallic copper have been shipped. The ore exported contained on an average about 14 per cent, of metal. § 15. Coal Mining. — Coal mining, at Monte Diablo, in California, com- menced in 1861, and advanced very rapidly. In 1862, 23,000 tons were produced, and in 1866, 84,000 tons. It was at first supposed that the coal was of very poor quality, and that the supply would soon give out ; but these suppositions have proved to be erroneous. § 16. Borax. — The production of borax was commenced in California in 1865, in which year 1,707 cases, worth $22 per case, were exported; in the next year, 3,171 cases were exported; and in the first half of 1867, 3,671 cases. The borax is obtained from Borax Lake, which covers an area of 200 acres, one mile from the eastern end of Clear Lake, in Lake County. The water of the lake is strong with borate of soda, and the mud at the bottom of the lake is full of crystals of borax, nearly pure. § 17. Other Minerals.— In 1866, 5,000 barrels of California petroleum were produced. Several tons of sulphur were refined near Clear Lake; and several tons of plumbago were refined at Sonora. An opal mine was XVm INTRODUCTION. opened at Mokelumne Hill in 18G5, but proved unprofitable, and the work has ceased. The stones are abundant, but common in quality. § IS. Treasure Trade. — Up to the end of 1S61, the total amount of treasure manifested at the San Francisco Custom House for exporta- tion, as giv^en in section 177, was $551,603,904. Since '61 the following sums have been shipped, viz.: in 1862, $45,561,761; in '63, $46,071,920. in '64, $55,707,201; in '65, $44,984,546; in '66, $56,146,577; in '67,' $48,069,236. Adding these sums to the total of 12 years before, we have $845,346,245. It is well known, however, that large sums were exported in early years without entry at the Custom House, and my estimate of $700,000,000 for the total exportation previous to the 1st January, 1862, has been considered, by business men and bankers, in San Francisco, to be as near correct as any estimate could be, and we may assume that in the last six years and a half the production has been greater by $35,000,000 tlian the exportation; we have a total production of $1,030,000,000 for the coast, up to the 1st January, 1868. This production, however. Las not been exclusively from California. In 1866, "Wells, Fargo & Co.'s Express, which carries all the treasure, the transportation of which is published, received at San Francisco, $24,055,381 from the Northern mines of Cahfornia, $5,415,711 from the Southern mines, $15,215,218 from Nevada, $6,551,284 from the Northern Coast, including Victoria, and $2,369,994 from foreign parts. During 1867 the Northern mines sent us $22,927,309, the Southern mines $4,477,462, Nevada $18,000,000, and the Northern Coast, $5,829,522. The yield of Nevada is rapidly increasing ; that of Idaho,, which supplies most of the gold from the "Northern Coast," is either decreasing since 1864, or else the treasure is sent eastward overland. California supplies about three-fifths of the treasure exported from San Francisco. One of the main causes of the decrease in the gold production of this State is the tax of $4 per month levied on Chinese miners. Not less than ten thou- sand have left the placers of California within the last two years, either for Idaho, Montana, or Nevada. § 19. Shipping. — Previous to 1860 our imports exceeded our exports, and ships came heavily laden, and went away in baUast. The tables are now turned, and ships come in ballast to load with our grain, copper ores, wines, wool, hides, horns, quicksilver, borax, and plumbago. In the first half of 1867, 1,144 vessels, registering 391,000 tons, entered the port of San Francisco, making the annual tonnage of the port about 800,000. I 20. Population. — The population of the State has gained considera- INTRODTJCTION. XIX bly during the last live years, but there is no method of ascertaining the precise increase. The gain by excess of arrivals over departures seaward, was 3,232 in 1853 ; 23,023 in '54; 6,300 in '55; 5,372 in '56; 6,088 in '57; 12,745 in '58 ; 13,402 in '59 ; 16,185 in 'GO ; 16,864 in '61 ; 16,150 in '62; 15,882 in '63 ; 9,773 in '64; 4,759 in '66; and 14,470 in 1867 ; malting a total gain of 165,245 in fourteen years. In 1865 there was a decrease of 3,780, leaving a net gain of 161,405. The increase, by birth has more than counterbalanced the loss by death and by emigration overland to Nevada, Idaho, and Montana. In section 252 I estimated the population at 400,000 ; and if that figure was correct for the 1st July, 1860, and I am inclined to think it was, then the present population of <>alifornia is not far from 500,000. § 21. Manufactures. — Since 1862, there has been a very rapid develop- ment of the manufacturing industry of the country. Mills and factories have been estabhshed, and are now in operation, making cotton goods, powder, linseed and castor oils, ropes of iron and hemp, glass, shot, lead pipe, boots and shoes, and brushes. Additional paper and woolen mills have been buUt. A rolling mill is now in the course of erection. - These manufactures are nearly all at San Francisco, which is likely to become one of the chief manufacturing cities of the Union. Large quantities of turpentine and rosin are made in Butte and Yuba Counties. In 1866, 18 vessels left San Francisco for the codfish banks of the North Pacific, and they brought back fish which when dried weighed 900 tons. Tiiis fishery began in 1864. The production of soap in San Francisco in 1866 was 13,000,000 pounds. § 22. -San Francisco. — The growth of San Francisco has been steady and rapid since 1862. Every year has witnessed great changes and vast additions to the number of buildings. The city is truly metropolitan in its appearance. Montgomery Street, as a fashionable retail street and promenade, has no superior on the continent, save Broadway ; and Kearny Street, which is now being widened, is rapidly advancing to rival Mont- gomery. There are three hotels, which in size and style deserve to take rank with the finest of New York. Five street railroads are ready to take passengers to every part of the city. One of the largest and finest stone dry-docks of the world is nearly completed, at Hunter's Point. The con- struction of a sea-wall, to protect the harbor, has been commenced. Splendid buildings have been erected by the Merchants' Exchange Associ- ation, the Mercantile Library Association, and the Mechanics' Institute. The silver mines of AYashoe, and the principal quartz mines of California, XX INTRODUCTION. are mostly owned here, and their wealth has contributed to beautify and enrich the city. The establishment of a regular line of monthly steamers to China and Japan, and the rapid progress of the Pacific Railway, with the certainty of its speedy completion, have given confidence, attracted population, and induced the investment of capital. Numerous branches of manufacturing industry have been established. The commerce of the city has continued to advance. The average number of houses erected annually, during the last five years, has been about 1,500. It may safely be said that no city shows greater signs of prosperity. San Francisco," in proportion to size, is the busiest seaport in the world. The annual exports are about $70,000,000 and the imports nearly as much; the manufactures are worth nearly $20,000,000; the real estate sales amount to about $12,000,000, and the cash value of land, building, and movable property, is about $200,000,000, although assessed for taxation at only $80,000,000. It sends away about forty tons of silver and six tons of gold every month — the former metal in bars fifteen inches long and five inches square, the latter in small bars about six inches long, three inches wide, and two inches thick. Wagons loaded with the precious metals are seen in the streets nearly every day. Most of the towns of the interior have grown but little during the last five years. Sacramento suffered so severely from the flood that she has not yet recovered. The Central Pacific Railroad, the Sacramento Valley Railroad, and the California Pacific Railroad (from YaUejo) center here; and the Western Pacific, the buildings of which has been long de- layed, is to terminate here. The new State House, to cost more than $1,000,000, will not be finished for a year or two. § 23. Vallejo. — The construction of the California Pacific, and Napa Valley Railroads has given a stimulus to Vallejo, which seems to be on the point of getting the benefit of the natural advantages of its position. Those advantages could do nothing for it without the assistance of rail- roads ; but now that the roads are to be built, Vallejo is certain to be one of the leading towns of the coast. Its exemption from earthquakes, the probability that it will be a brick-built town, the consequent security against great fires, the freedom from a heavy debt, the promise of free wharfage, the certainty that it will be the terminus of the railroads from Humboldt Bay and Oregon, and that it will'attract much of the travel and freight from Sacramento, and the possibility, or as many view it, the probability, that it will be the main western terminus of the Pacific Rail- INTRODUCTION. 2X1 road, are great considerations in its favor. Ttie town is groAivang rapidly now, and land has increased greatly in value. § 24. Legal matters. — Congress has granted to the State of California, Yosemito Yalley and the Big Tree Grove of Mariposa; and has passed an act providing for the sale of the quartz mines, on which work to the amount of $1,000 has been done; and for the sale of the agricultural lands in the mineral districts. § 25. Communications. — In 1862, the only railway in the State was the Sacramento Yalley road, 20 miles from Sacramento to Folsom. Now we have the Central Pacific completed 95 miles, from Sacramento to Cisco; the San Francisco and San Jose road, 50 miles; the Western Pacific, completed from San Jose to Yallejo's mill, 20 mUes ; the Alameda and Hay ward road, 15 miles; the Oakland and Brooklyn road, 4 miles; the Napa Yalley road, 25 miles ; the Oroville and Marysville road, 25 miles ; the Central California road, from Folsom to Marysville (unfinished), 40 miles ; and the California Pacific, from Yallejo to Sacramento (un- finished), 60 miles ; and the Folsom and Shingle Springs road, 40 miles. A monthly line of steamers runs to China and Japan ; another to Mazat- lan ; and a third is to be established to the Hawaiian Islands. There are two lines of telegraph across the continent, placing us in instantaneous communication with the Atlantic States and Europe. § 26. Californian Books. — Considerable contributions to the literature of California have been made during the last five years. Among the books written in or about California, or published by Californians, arc : the first volume of the Geology and volume first of the Paleontology of the State Geological Survey; the Reports of the Pacific Railroad Survey; the History of California, by Franklin Tuthill ; the History and Resources of California (in French), by Ernest Frignet; the Resources, Society, and Industry of California (in German), by Karl Ruehl ; a School History of California, by Lucia Norman ; the Mineral Resources of the Pacific Slope, by J. Ross Browne, U. S. Commissioner of Mining Statistics ; a Treatise on Mining Law, by Gregory Yale ; a collection of California Poems, called " Outcroppings ;" another styled "Poetry of the Pacific;" a volume of poems, by Charles Y^arren Stoddart ; the Jumping Frog of Calaveras, by Mark Twain (Samuel Clemens); Phoenixiana, by Lieut. Derby; the Ad- ventures of James Capen Adams, the Grizzly Bear Hunter, by Theodore H. Hittell ; and Treatises on Grape Culture and Y^ine-making, by A. Har- aszthy and T. H. Hyatt, and a Manual of Silk Culture, by L. Prevost. San Francisco, April 15, 1868, INTEODUCTION THE FIFTH EDITION. 1869 The progress of California within the last year has been remarkable. The rapid advance of the Middle Facific Kailroad, the probability that other transcontinental railroads will soon be commenced, the construction of a number of coast roads, the cultivation of large areas previously unoccupied, the concurrence of large crops of grain with high prices, the doubling of the wool clip within two years, the success of the mulberry plantations, the in- creasing profits of the vineyards, and the discovery of the White Pine mines, have contributed to make this a year of unexampled activity and prosperity. Before this edition goes to press, the Middle Pacific Railroad will have been completed, and the cars will run through from New York to Sacra- mento, a distance of 3,181 miles. Of the Western Pacific, connecting Sacra- mento with Oakland, twenty miles are in running order, and it is expected that the remainmg 104 miles will be completed before the 1st of July, with the exception of a small section at Livermore Pass, where there is a tunnel that will probably not be cut through till August. The CaUfornia Pacific Eailroad between Vallejo and Sacramento, has become one of the main lines of travel in the State. The first section of the Southern Pacific Railroad, from San Jose to Gilroy, thirty miles, the Napa Valley railroad from Adelante to Calistoga, thirty-three miles, and the Central California road from Junction (on the Central Pacific line) to Marysville, are finished. The roads now in the course of construction, are the Marysville branch of the California Pacific, forty-two miles, the Western Pacific from Cosumnes to Oakland, 104 miles, the San Lorenzo road from Santa Cruz to Felton, 15 miles, the road from Los Angeles to Wilmington, twenty miles, and the Petaluma and Santa Rosa road, sixteen miles. Promises have been made that work shall soon be com- menced on roads to connect Suscol with Santa Rosa, thirty miles, Stockton with Paradise, twenty-five miles on the way to Visalia, and Marysville with Chico, on the way to Oregon. It has been discovered that the plains east of the San Joaquin river, long INTRODUCTION. XXlll able quantities of rich argentiferous galena have been smelted out at CeiTO Gordo, near Owen's Lake. The production of quicksilver was larger in 1868 than ever before, the exportation of the year having amounted to 43,000 flasks, or 3,268,000 lbs. The tin lode at Temascal has been well opened, and found to be wide and rich; and preparations are being made to extract the ore in large quantities. The growth of San Francisco has been rapid. The population of the city was 2,000 in July, 1849; 25,000 in December, 1850; 60,000 in December, 1855; 83,000 in August, 1861; 119,000 in August, 1865; 131,000 in July, '1867; 150,000 in July, 1868, and it is 160,000 in March, 1869. In 1868, 59,000 passengers arrived at this port by sea, and 25,000 departed, leaving a net gain of 34,000. The vessels which entered the harbor in the same pe. riod numbered 3,300, and measured 1,000,000 tons. The exports of mer- chandise and domestic produce were valued at $22,000,000. The sale of real estate in San Francisco amounted to $27,000,000, and of mining and other stock to $115,000,000. The mining and other companies incorporated in San Francisco, paid $5,000,000 of dividends. The widening of Kearney street has been completed ; the extension of Montgomery has been com- menced ; the stone Dry Dock at Hunter's Point is in working order, and the city is growing rapidly. Vallejo, Oakland, Sacramento, Stockton and Marys- ville, are all more prosperous than they have been at any time within ten years. IlsTDEX OF CHAPTEES. Chapters. P^S^ I. CnoRoaRAPnY 1 II, Climate 19 III. Geology 47 IV. Scenery *^2 Y. Botany 91 YI. Zoology ^08 YII. Agriculture 151 VIII. I^IINING 238 IX. Other Branches of Int)ustry 304 X. Commerce 326 XI. Constitution and Laws 349 XII. Society. 359 XIII. Topographical Names • 4:22 XIV. The Past and Future Development of the State 431 APPENDIX. Oregon 461 Washington Territory 415 Nevada 492 Index of Sections • 501 HESOUPiCES OF CALIFORNIA. CHAPTER I. CHOROGRAPHY. § 1. General Remarks. — California has a peculiar cho- rography. No other country comprises within so small a space, such various, so many, and such strongly-marked cho- rographical divisions. Mountains the most steep, barren, and rugged; valleys the most fertile and beautiful; deserts the most sterile; spacious bays, magnificent rivers, imparalleled waterfalls, picturesque lakes, extensive marshes, broad prairies, and dense forests — all these are hers. In general shape, California is a long parallelogram, extend- ing from latitude 32° 45' to 42° north, seven hundred miles in length by one hundred and eighty in breadth, the course of the longitudinal axis being north-northwest by south-southeast. The first topographical division of the state may be into the Coast and Interior districts, separated from each other by the main ridge of the Coast Mountains, which runs the whole length of the state, nearly parallel with the ocean, and about fifty miles from it. The Coast district may be subdivided into the Coast 3fou7itains and the Coast Valleys. The Interior district may be subdivided into the Sierra Nevada, the Sac- 1 2 BESOTJKCES OF CALIFORNIA. ramento JBasin^ the Plateau of the Sierra Nevada^ the Kla math Basin^ the Great Basin of Utah^ and the Colorado Desert. § 2. Coast Mountains. — The Coast range, though not so high or so wide as the Sierra Nevada, may be considered the main orographical feature of California, because it alone extends through the whole length of the state. The height of the range is from two thousand to six thousand feet; its width from twenty to forty miles. South of 34° 20' the spurs are short and run at right angles to the course of the main divide, which is the easternmost ridge of the chain; nearly all the spurs, v^alleys, and streams, run to the west- ward. South of 34° 20' a plain from twenty-five to forty miles wide lies between the momitains and the sea ; north of that the spurs make up the greater part of the Coast line, and, where they enter the ocean, form the headlands and capes. The Santa Susanna spur starts from the main ridge in 34° 20' and runs west by south, and is separated by the valley of the Santa Clara River from the Santa Inez ridge, which starts in 34° 30' and runs west ; then continuing our course northward, across the Santa Inez valley, we come to the Santa Barbara ridge, which starts from the main ridge in 34° 40' and runs west-northwest. The Cuyama valley separates the Santa Barbara from the Santa Lucia ridge, which branches off at 35° in a northwestern direction, and forms the southern bound- ary of the Salinas valley, whose northern boundary is the Gab- ilan ridge, starting in 36° 10' and running north-northwest; which is separated from the Contra Costa ridge, rising in 37° 10' by the Santa Clara valley, and the Contra Costa ridge is separated from the main divide by the Amador and San Ramon valleys. The Gabilan ridge forms the back-bone of Santa Cruz, San Mateo, and San Francisco counties, each of which gives its name to that portion within its borders. The ridge is cut in two on the southern border of Santa Cruz county by the Pajaro River, and the Alameda Creek breaks through the Contra Ctosta ridge. North of the Golden Gate, CnOROGRAPH Y. 3 the Gabilan ridge reappears, and is separated by Petaluma valley from the Sonoma ridge, that by Sonoma valley from the Carneros ridge, and that by Napa valley from the main Coast ridge. Farther north the spurs are so numerous, and con- nected so closely together, that they are scarcely distinguished by names ; and a large portion of the coast, from the main ridge westward, is a mass of mountains. The Coast Moun- tains are steep, rocky, rugged, and brown; north of 38° they are covered with timber and brush ; south of that the ridges nearest the ocean have some timber, those farther inland are nearly bare. The main ridge near the head of the Sacramento valley is called the Trinity ridge ; near Mount Diablo it is called the Diablo ridge, or the Bolbones ridge ; south of 34° it is called the San Bernardino ridge, and in one place the Cuyamaca Mountain. § 3. Coast Peaks and Passes. — The principal peaks of the main ridge are Mount Linn, in 40° 10' ; Mount St. John, in 39° 25'; Mount Ripley, 7,500 feet high, in 39° 08'; Mount St. Helena, 3,700 feet high, in 38° 40' ; Mount Diablo, 3,876 feet high, in 37° 50'; Pacheco's Peak, 2,700 feet high, in 36° 57'; Mount San Bernardino, 8,500 feet high, in 34° 20' ; and Mount San Gorgonio, 7,000 feet high, in 33° 48'. In the Gabilan ridge are the following peaks : the Chupadero, in 36° 35'; the Gabilan, in 36° 50'; the Loma Prieta, 4,040 feet high, in 37° 08' ; and Table Mountain, or Tamalpais, in 37° 53'. The prin- cipal passes in the main ridge are south of the outlet of the Sacramento basin, and are — Livermore's Pass, 686 feet high, in 37° 42'; Pacheco Pass, in 37° ; the Pass de los Robles, in 35° 20'; the Cajon de Tenoco, in 34° 40'; the 'Pass of San Francisquito, 3,437 feet high, in 34° 35'; Williamson's Pass, 3,164 feet high, in 34° 30'; the Cajon Pass, 4,676 feet high, in 34° 10'; the San Gorgonio Pass, 2,808 feet high, in 33° 55'; and Warner's Pass, 3,780 feet high, in 33° 10'. The Santa Mar- garita Pass, with an altitude of 1,350 feet, leads across the Santa Lucia ridge, in 35° 20' ; and the San Fernando I*ass, 1,956 feet high, crosses the Santa Susanna ridge, in 34° 20' 4 EESOURCES OF C A L I F O E JS^ I A. Having thus considered the mountains, let us look into the valleys of the coast. The flat land west of the San Bernardino Mountains, south of 34°, is rather composed of plains than of valleys, though watered by the San Gabriel, Los Angeles, Santa Ana, and other rivers. There are two of these plains : the lower one about two hundred and fifty feet above the sea, and skirting the coast ; the other one thousand or twelve hun- dred feet high, nearer the mountains. On the lower plain are Los Angeles, Anaheim, and San Pedro ; on the upper are San Fernando, San Bernardino, Cocomongo, Jurupa, Temescal, and Temecula. Northward of 34° we find long, flat, narrow, fertile valleys, shut in by steep, rugged hills. We have already mentioned the names of many of these valleys, as dividing cer- tain ridges of the Coast Mountains from each other. South of the Salinas all these valleys open upon the ocean, save the Cuyama valley, the river of which runs in a caiion through mountains as it approaches its mouth. The Pajaro River breaks through the Gabilan Mountains, and makes a small but rich valley. The average width of these coast valleys is five miles at the mouth, with a length of from ten to forty miles, narrowing to a point near the head in the mountains. The Salinas valley, the .largest of all the coast valleys, is ninety miles long, and from eight to fourteen wide. Three terraces are distinctly traceable on each side of the river. The first and lowest is about four miles wide, with a sort of a rich, sandy loam ; the second rises with an abrupt edge, is eleven feet higher, has about two miles of width on each side, and has a coarser, poorer soil ; the third terrace is less regular in height and width, and has a coarse, gravelly soil, scarcely fit for cultivation. This terraced formation, with its variations in richness of soil, is a strongly-marked feature of many valleys in the state. Ordinarily, the coast valleys are separated from each other by steep, rugged mountain-ridges, but there are occasional exceptions. Thus, there is a low plain between Russian River and Santa Rosa valley, which opens into Sono- ma and Petulama valleys; and again, the Santa Clara and CHOEOGKAPHY. 5 Pajaro valleys are separated from each other by hills not more than two hundred and fifty feet high ; and the valleys of the Pajaro and the Salinas open into each other. So also the divide between San Ramon and Amador valleys is so low as to be scarcely noticed by the traveller ; and Amador valley is connected, by a level road through a caiion, with Sunol valley, and that by another caiion with the plain at San Jose Mission. North of San Francisco Bay, the valleys of Suisan, Yaca, Pu- tah, and Cache Creek, lie eastward from ISTapa valley. The valley at the head of Putah Creek is sometimes called Berre- yesa valley ; and that at the head of Cache Creek, Clear Lake valley. North of Russian River there is little level land, and that little is found in Eel River valley, about the shores of Humboldt Bay, and about Crescent City. § 4. Coast Rivers. — The rivers of the Coast Mountains have necessarily but a short course. Those south of the bay of San Francisco are the San Lorenzo, Pajaro, Sahnas, Cuyama, Santa Inez, Santa Clara, Los Angeles, San Gabriel, Santa Ana, Santa Margarita, San Luis Rey, San Diegaito, and San Diego. Some of these are large streams in wet winters ; but, in the drought of autumn, all those south of the Salinas are swallowed up in the sands before reaching the ocean. Most of them are con- stant streams to within ten or fifteen miles of their mouths. The Santa Ana, the largest river on the southern coast, rises in Mount San Bernardino, and is in its meanderings nearly one hundred miles long, yet only in very wet seasons, once in six or eight years, succeeds in getting to the sea. The San Gabriel River sinks before reaching Monte, in Los Angeles county, and, after passing three miles under ground, rises again. Tlie intervening space, where there is no river, is very moist, sandy ground, through which the water spreads and soaks. W. H. Emory, in his report as member of the Mexican Boundary Commission, writes thus ; "The point at which water ceases to flow is quite variable ; its more usual upward limit being marked at or near the pas- sage of the stream from the first rocky ranges into the tertiary 6 RESOURCES OF CALIFORNIA. formation. The point, however, as before stated, is by no means a fixed one : thus, during the night it extends farther downward than in daytime ; in cloudy weather, for the same reason, its course is more prolonged than under a clear sky. In the stream-beds themselves, however dry, water is gener- ally found a short distance below the surface. " The descent of these streams in the rainy sea,son may be either a gradual process in the progressive saturation of their sandy beds, or, the saturation being accomplished by previous showers, the irruption may be sudden. A fine example of this sudden appearance was observed in the San Diego River, in December, 1849 ; when, after a rainy night, by which its sandy bed was completely saturated, the upper stream suddenly ap- peared in the form of a foaming body of water^ moving onward at the rate of a fast walk, curling round the river-bends, ab- sorbing the pools, and soon filling its bed with a brimming, swift current. An instance of the more gradual descent was seen in the following season (December, 1850), when, from the absence of local rain, its downward progress was slow and interrupted." The only navigable stream south of San Francisco Bay is the Salinas, and that but for small vessels, and near its mouth. North of San Francisco the main streams rising in the Coast Mountains are the Russian, Eel, Elk, Mad, and Smith Rivers, all permanent, but none navigable. § 5. Coast Lakes. — The only large lake in the Coast district is Clear Lake, which lies about eighty miles northward from San Francisco. It is twenty miles long, and varies in breadth from two to ten miles. Surrounded by a small valley of fer- tile land, it lies in a deep basin bounded by high mountains, with an outlet to the eastward, where its surplus waters are carried off by Cache Creek to the Sacramento. The water of Clear Lake is limpid; the vegetation on its banks abundant and vigorous ; the scenery beautiful and romantic. In Ama- dor valley, twenty-five miles eastward from San Francisco, there is a small lake, covering a couple of hmidred acres. It CHOROGKAPHT. 7 lies in the course of the Alameda Creek. In the San Francis- quito Pass, forty-five miles northward from Los Angeles, there was a lake called Lake Elizabeth, covering several hundred acres, but it has dried up of late. These are the only lakes of note in the Coast district. Pre- vious to 1860, there was a lake called the *'Laguna Sal," six miles long and three wide, near Alamo, San Diego county; but it entirely dried up in that year. The water had a strong taste of alkali and sulphur. According to report, the lake was formed about the year 1820. § 6. Capes. — CaUfornia has two capes : Cape Mendocino, in 40° 25'; and Point Conception, in 34° 25'. The former is reputed to be the stormiest place on our coast ; the latter is the southern limit of the cold fogs and cool summers. § 7. Islands. — About forty miles westward from San Fran- cisco are the Farallones, seven little islands of bare rocks, the largest with an extent of a couple of acres, and of no signifi- cance save as a danger to shipping, and as a point where a large lighthouse is maintained. All the other islands of Cali- fornia lie between 32° 50' ?,nd 04° 10', the farthest one being about sixty miles from the mainland. They are named Santa Cruz, Santa Catahna., San Clemente, Santa Rosa, San Nicolas, Anacapa, and Santa Barbara. They are all hilly, rocky, bar- ren, and of little value. Santa Cruz, the largest and best of them, has good water and a few trees. It is twenty-one miles long, with an average width of about three miles. All these islands appear to be peaks of submerged mountain-ridges. Be- tween them and the mainland lies the Santa Barbara channel. § 8. Bays and Harbors. — California has four land-locked bays — Humboldt, Tomales, San Francisco, and San Diego. All of them are comparatively long and narrow, and separated from the ocean by narrow peninsulas, their general course being parallel with the coast. Humboldt Bay is twelve miles long, from two to five miles wide, and is separated from the ocean by two tongues of land, which are covered by high and dense timber, and ofier an 8 KESOTJRCES OF CALIFORNIA. excellent protection against the strong winds of the coast. The mouth of the bay, in latitude 40° 44', is a mile across, but has breakers on each side ; and between them is a channel, a quarter of a mile wide, with about eighteen feet of water at loAV tide. The greater part of the bay is shallow, but there is an abundance of deep water, with good anchorage and perfect safety for shipping. The entrance is considered dangerous, and a steam-tug escorts nearly all sailing-vessels in and out. Tomales Bay is fourteen miles long and two miles wide, separated from the ocean by a strip of land a mile and a half wide. Its mouth is in 38° 15'. Its course is southeastward, and it is open to the northwest winds. The water is about twelve feet deep. Tomales Bay is surrounded by hiUs, and is of little value for commerce. San Francisco Bay, one of the finest bays in the world for the purposes of commerce, is about eight miles wide and fifty long, reaching from 37° 10' to 38°. Its entrance, called the Golden Gate, or Chrysopylis, is a mile wide, between 37" 48' and 37° 49'. The peninsulas which separate the bay from the ocean are from six to fifteen miles wide. The water on the bar is thirty feet deep at low water ; inside much deeper, with excellent holding-gromid, and room for all the shipping of the world. Connected with this bay are those of San Pablo and Suisun, lying farther inland, on the course of the outlet of the waters of the Sacramento basin. San Pablo Bay is nearly round, about ten miles in diameter, and lies north of San Francisco Bay, with which it is connected by an unnamed strait, about three miles wide. Suisun Bay, about four miles wide by eight long, lies eastward of San Pablo Bay, with which it is con- nected by the strait of Carquinez, which is a mile wide. Both bays are deep, but the water in the strait is only sixteen, feet deep at low tide, and large vessels cannot ascend beyond it. Benicia, on the bank of the strait, is the head of navigation, and aspires to be the main port of the coast, but in vaia. Yal- lejo, seven miles from Benicia, still has hopes of that kind. CHOEOGEAPHT. 9 The harbor of Yallcjo is excellent, lying between Mare Island and the mainland. It is half a mile wide, by three miles long, with four fathoms of water at low tide, excellent holding- ground, and perfect protection against all winds. The bay of San Diego is twelve miles long, from one to two miles wide, and crescent-shaped, running from the entrance, and then turnmg to the southeastward. A channel, thirty feet deep and half a mile wide, extends more than half the length of the bay from the entrance. The holding-ground is good; the protection from the winds perfect. There is no difficulty in entering at any time, but it is not safe for sailing- vessels to go out during gales from the southeast. In latitude 34° 38', thirty-five miles southeastward from Los Angeles, is a land-locked estuary about eight miles long and from half a mile to a mile wide. It has not been surveyed, and its value for commerce is not known, but there has been some talk lately of using it as a port for some of the adjacent towns. The entrance is not more than ten feet deep, and probably not so deep as that. Of the open harbors, that of Crescent City is the most northern, in latitude 41° 44'. It lies on the southern side of a rocky point that juts out about half a mile in a westward direction, at right angles to the general line of the coast. The harbor is small and shallow, with a bottom of sand and rocks. Vessels drawing twelve feet of water lie nearly half a mile from the shore. The harbor is safe while the wind blows from the north and northwest, but Tcry dangerous when it blows from the southward. The harbor might be made much more safe by a breakwater, at a cost of one or two millions of dollars, but the trade of the place would never justify such an expenditure. Trijiidad, in 41° 03', is a very small harbor, open to the south, with deep water and excellent holding-ground. Bodega Bay, in 38° 18', has nine feet of wtttdi, and opens to the southward, so that the anchorage is secure only while the wind blows from the north. Tomales Bay, just opposite. 10 EESOUKCES OF CALIFORNIA. opens into the southern part of Bodega Bay, and is only five miles distant from the Bodega anchorage ; and, as one is secure against nortliern and the other against southern winds, vessels are safe in all weathers, because they can easily run across to whichever may prove the sheltered side. The bay of Sir Francis Drake, in latitude 38°, is small, open to the south, and of no value to commerce. Half Moon Bay is a small roadstead, eighteen miles south of the Golden Gate. Santa Cruz Harbor, on the northern side of Monterey Bay, in 36° 57', is small, has four fathoms of water, a sandy bottom, and is open to the south. Twelve miles ftirther south is the mouth of the Salinas River, which is about two hundred yards wide, and has seven feet of water. It is entered by small schooners, with the help of a steam-tug. Eight miles farther to the southward is the harbor of Mon- terey, which is large and deep, and has good holding-ground. It is open to the north. San Simeon Harbor, in 35° 38', has a good anchorage, and is safe while the wind blows from the north, but it offers no protection against storms from the southward. The bottom is sandy. San Luis Obispo Harbor, in 35° 10', has a good anchorage, safe at all times, except during storms from the southward. Santa Barbara, in 34° 24', has an open harbor, exposed to the south winds. The water is deep, and the bottom hard. San Pedro, in 33° 43', is open to the south, but probably might be made secure by a breakwater, to cost one million of dollars. The bottom is hard. The difference between extreme high tide and extreme low tide is about nine feet at Crescent City, and seven feet at San Diego. At San Francisco, tiie establishment of the port is ten hours. § 9. Sacramento Basin. — The low land of the Sacramento basin, bounded on the west by the Coast Mountains and on CHOEOGEAPHY. 11 the east by the Sierra Nevada, which ranges meet both at the north and the south, is the heart of the state, four hundred miles long by fifty wide, reaching from latitude 35° to 40° 30'. It is drained by two rivers : the Sacramento, running from the north ; and the San Joaquin, from the south. They meet and unite in the centre of the basin, at 38°, and break throuo-h the Coast range to the Pacific, forming the bays of Suisun, San Pablo, and San Francisco, on their way. The mountains rise steeply from the edge of the valley, which is nearly level, about thirty feet above the level of the sea at the junction of the rivers, and two hundred feet higher where they issue from the mountains. Part of the Sacramento valley shows terraces, the farthest from the river being a coarse gravel. The richest soil is on the immediate bank. The great body of the valley is bare of trees. Its even surface is broken in only one place, by the " Buttes," a range of volcanic hills, six miles wide by twelve long, with three peaks, about two thousand feet high, which rise in lonely abruptness from the middle of the plain, in 39° 20'. The general course of the two main rivers of the basin lies nearly midway between the two mountain-chains, but almost all their tributaries come from the Sierra Nevada, which, Uke the Coast range, has most of its wealth on its western slope. In the four hundred miles from Tejon to Shasta there are a dozen creeks marked on the map as flowing eastward from the Coast range to the San Joaquin and Sacramento ; but during the summer, three-fourths of them are swallowed up in the sands before reaching their mouths. Not one south of 38° is a permanent stream. From the Sierra Nevada a num- ber of rivers run westward. Beginning at the north, we have the Pit, Feather, Yuba, American, Cosumnes, Mokelumne, Calaveras, Stanislaus, Tuolumne, Merced, San Joaquin, King's, White, and Kern Rivers — all of them considerable streams, though some of those in the southern part of the Sacramento basin are swallowed up in the sands, in the dry seasons, before reachmg their mouths. The San Joaquin River does not rise at the extreme southern end of the basin, but one hundred 12 RESOURCES OF CALIFORNIA. miles northward from it, in the Sierra Nevada. After running westward to the middle of the valley, it turns northward. From its bend southward, the valley discharges no water to the ocean during the summer ; but in wet winters there are continuous sloughs, or pieces of marsh-like ground, from the Tejon to the San Joaquin. In the dry season, no channel is visible for the escape of the waters of Tulare and Kern Lakes. § 10. Bivers of the Sacramento Basin. — The rivers flow- ing down from the Sierra Nevada are about one hundred and twenty miles long on an average, following their courses. The upper half of their length is in the mountains, where they are torrents, falling five thousand feet in fifty miles. Their beds are in deep canons ; after reaching the plain their currents are gentle, and they meander between low banks, fringed with oaks, sycamores, cotton wood, and willows. In the south- ern part of the Sacramento basin there are several large streams, which, soon after issuing from the mountains, divide into a number of channels, as do some large rivers which have deltas near their entrance to the sea. King's River, which is about eighty yards wide where it leaves the mountains, divides into seven or eight channels, which all unite again. The Ca- huilla or Pipiyuma River, also a large stream, divides into a number of channels, which irrigate " the Four-Creek country," and render it one of the most fruitful parts of the state. The Sacramento River is navigable for steamers drawing three feet of water, to Sacramento City, and to Red Bluff for boats drawing fifteen inches. The Feather River is navigated by steamers drawing fifteen inches, to Marysville, seventy-five miles from Sacramento ; and boats have ascended to Oroville, twenty-five miles farther. Steamers drawing five feet can run regularly to Stockton, on the San Joaquin, a distance of one hundred and thirty miles from San Francisco ; and in times of higrh water, a boat drawino^ about fifteen inches ascends to Fresno City, one hundred and fifty miles farther. A number of sloughs or tide-water creeks, navigable for small vessels, open into the bays of San Francisco, San Pablo, and Suisun. CHOEOGRAPnT. 13 The most notable of these are the Alviso or Guadalupe slough, at the head of San Francisco Bay ; the San Antonio slongh, opposite San Francisco city ; the Petaluma, Sonoma, and Napa sloughs, opening into San Pablo Bay; and Suisun and Pacheco sloughs, opening into Suisun Bay. § 11. Tide-Land. — Along the borders of these bays, and of the Tulare and Kern Lakes, and of the Sacramento and San Joaquin Rivers, there are extensive tracts of swamp-lands, usu- ally called "tule-lands," from the tule^ a species of rush which grows on them. Nearly all the tule-land west of Sacramento and Stockton, to which points the tides extend, are salt marsh- es ; but north of Sacramento, and south of Stockton, the tule- lands are fresh-water swamps. The extent of this marshy land varies in different seasons ; but at my estimate, there are eighty square miles on the borders of San Francisco Bay, eighty on San Pablo Bay, sixty on Suisun Bay, two hundred on the Sac- ramento River, one hundred on the San Joaquin, two hundred on the Tulare Lake, and the slough leading from it, and one hundred and twenty south of Tulare Lake — making eight hundred and forty square miles in all. § 12. Bierra Nevada. — The Sierra Nevada is four hundred and fifty miles long (in California) and seventy wide, with a height varying from five thousand to eight thousand feet above the sea-level. Nearly its whole width is occupied with its western slope, which descends to a level of three hundred feet above the ocean ; whereas the slope on the eastern side is only five or six miles wide, and terminates in the Great Basin, which is itself from four thousand to five thousand feet above the sea. Nearly all the snows and rains that visit the Sierra Nevada fall on its western slope, which has all the large rivers. These rivers run westward, at right angles to the course of the chain, and cut it into steep hills and deep ravines, canons, and chasms. The valleys are all small, and it is rare to see a hundred acres of level, tillable land, even on the banks of the largest moun- tain-streams. The greater pnrt of the Sierra Nevada is cov- ered with timber. The oak, manzanita, and nut-pine, grow to 14 EESOURCES OF CALIFORNIA. about twenty-five hundred feet above the sea ; and then the coniferous trees appear, and are found in dense forests to a height of six thousand feet. § 13. Peaks and Passes of' the Sierra. — Mount Shasta, which rises, in 41° 30', high into the region of perpetual snow, the loftiest peak in the state, may be treated as belonging to the Sierra Nevada, though in fact it stands midway between that range and the Coast Mountains, and is connected by high mountain-ridges with both of them. Its height is given by Wilkes (Exploring Expedition, vol. v., p. 240) at 14,390 feet. Kearly a perpendicular mile of it is always covered with snow, and it is visible in every direction for more than a hundred miles, presenting to the traveller the most prominent landmark of the state. It is of volcanic origin, and still emits sulphure- ous vapors from its summit. Several parties have ascended to its top. The other most notable peaks in the Sierra Nevada are — Lassen's Peak, 9,000 feet high, in 40° 22', also of vol- canic origin; the Donnieville Buttes, 8,500 feet high; Pilot Peak, 7,300 feet high, in 39° 50; Castle Peak, 11,000 feet high, in 38° 10' ; and Mount Breckenridge, 7,500 feet high, in 35° 20'. Mount Shasta is the only mountain which has snow on its southern and southwestern slopes throughout the year ; the other-mentioned peaks lose all their snow in September and October, except in deep, shady ravines on their northern slopes. The most notable passes in the Sierra Nevada are the fol- lowing: Lassen's, 7,000 feet high, in latitude 41° 50'; Fredo- nyer's, 5,667 feet high, m 40° 47'; Beckworth's, in 39° 50'; Kenness's, in 39° 30'; Truckey, 5,636 feet high, in 39° 25'; Johnson's, 6,752 feet high, in 38° 50'; Carson's, 7,972 feet high, in 38° 43'; Sonora, 10,132 feet high, in 38° 15'; Walk- er's, 5,302 feet high, in 35° 40' ; Hum-pa-ya-mup, 5,356 feet high, in 35° 35' ; Tehachepa, 4,020 feet high, in 35° 10' ; Tejon, 6,285 feet high, in 35° ; and Cajon de las Uvas, 4,256 feet high, in 34° 50'. The last five passes are in the Sierra Nevada, south of its bend, where it turns westward to meet the Coast range. CHOROGRAPHT. 15 Tlie Johnson Pass is used by most of the travel and traffic between Sacramento and Utah ; the Henness Pass lies east of jNIarysville, and is used by the people of that neighborhood ; and the Cajon de las Uvas is used by travellers between the San Joaquin valley and the Los Angeles district. § 14. Lakes of the Sierra. — The Sierra Nevada has few lakes. The most notable one is Lake Bigler, about twenty miles long and ten wide, and six thousand feet above the level of the sea, in latitude 39°, and on the eastern border of the state. Part of the lake is in Utah. Its waters flow eastward into Truckey River. In the eastern part of Nevada county there is a group of two dozen lakes, called the Eureka Lakes ; the largest are three miles long and a mile wide. § 15. Plateau of the Sierra Nevada. — About latitude 40°, the Sierra Nevada seems to divide or to fork — one branch run- ning northward, in the line of the main chain ; the other north- westward, to Mount Shasta. Between these two branches, and between 40° and 42°, is a high table-land or plateau, about one hundred and twenty miles long, and five thousand feet above the ocean-level. This plateau is an independent basin, and its waters never leave it, but flow into a few lakes, where they are swallowed up in the sands. The district bears a strong resemblance in many of its features to the Great Basin of Utah, with which it should perhaps be classed. The main stream is Susan River, which, after a course of forty miles in an eastward direction, empties into Honey Lake, which is twelve miles long by five wide — or was, for in 1859 the lake dried up, and again dried up in 1860. The lake, when full, was shallow, with thick, yellowish water, of a saline taste. Northwestward from Honey Lake, and distant thirty miles from it, is Eagle Lake, about half the size of the other. The land is barren, and the vegetation scanty. Pit River starts in the northeastern corner of the state, and breaks through the plateau. North of the river are Wright Lake and Rhett Lake, within five miles of the Oregon line ; and Goose Lake and Low- er Klamath Lake, partly in Oregon and partly in California. 16 EESOUECES OF CALIFOKXIA. The largest is Goose Lake, ten miles long and five wide. All are destitute of large tributaries, sweet water, and valuable adjacent land. § 16. Klamath Basin. — North of latitude 41° lies the basin of the Klamath River, which rises in Oregon, crosses the Cali- fornian line about eighty miles from the sea, then turns south- westward, and, after a course of about one hundred and fifty miles, empties into the Pacific in 41° 33'. The basin of the Klamath is very rugged, particularly that part of it within forty miles of the ocean. Along the main river there is no valley, or bottom-land ; its whole length is between steep hills and mountains, and through rocky caiions. Its largest tribu- taries, the Trinity and Salmon, run through a country almost as rugged as that bordering the main stream. Scott and Shasta Rivers, which are the only other notable tributaries of the Kla- math — they all flow from the southward — have valleys of bottom-land, about five miles wide and forty long. §17. TItah Basin. — A prominent feature of the North American continent is the Great Basin of Utah, a triangular district of country, bounded on the north by the basin of the Columbia, on the southeast by the basin of the Colorado, and on the southwest by the Sierra Nevada and San Bernardino Mountains. This Great Basin — an elevated tract of laud, most of which is four thousand or five thousand feet above the sea- level, mountainous, barren, and cheerless, with no outlet for its waters — extends into California, including a district about two hundred miles long and one hundred wide, in the south- eastern portion of the state. The Californian portion of the Great Basin is one of the driest and most sterile parts of the earth's surface, cut up by numerous irregular ridges of bare, rocky mountains, with intervening valleys of sand and volcanic scoriae, and occasional springs and little streams which termi- nate in lakes, presenting a Avide extent of muddy salt water after heavy rains, and, in the dry season, wide beds of dried and cracked mud, covered with a white alkaline efflorescence. The chief stream in the Californian portion of the Great Basin CHOROGRAPHY. 17 is the Mojave, which rises on the northern slope of Mount San Bernardino, and, after running about one liundred miles in a northeastward direction, sinks in the sand. The Mojave re- ceives no tributaries after it leaves the side of Mount San Ber- nardino. After sinldng, it rises again ; or rather pools of water are found in the low places of its bed, the water evidently- soaking through the sand and following the bed of the stream. The next stream in importance is Owen's Kiver, which runs southward seventy-five miles along the foot of the Sierra ISTe- vada, and terminates in Owen Lake, which lies in latitude 36° 25', and is fifteen miles long by nine wide. Northward, one hundred miles from Owen Lake, is Mono Lake, eight miles long and six wide, sometimes called " the Dead Sea of Califor- nia." No fish can live in the water, which is so heavy with saline substances, that the human body floats in it very lightly ; thongh it is so strongly alkaline, that it scalds the skin. In the midst of the lake is an island, several miles long. While the greater part of the Utah Basin is high above the level of the sea, there is a portion of it, called " Death Valley," three hundred and seventy-seven feet below the sea-level ; and, not- withstanding its great depth, it is one of the driest and most desolate parts of that basin of deserts. § 18. Colorado Desert. — A district, about seventy miles wide by one hundred and forty long, on the southeastern bor- der of the state, belongs to the basin of the Colorado River. It is usually called the " Colorado Desert," because of its bar- ren, sandy soil, and scanty vegetation. In some places the soil is composed of sand, packed together firmly, with a hard and smooth surface, which reflects light like a mirror ; in other places are niountains of loose sand, which are continually shift- ing. In latitude 33° 20', and longitude 115° 50', is a district, thirty miles square or more, which is seventy feet below the level of the sea. It is supposed that at one time the Gulf of California extended several hundred miles farther north than it now does ; and that the Colorado River, in long ages, depos- ited so much alluvium as to make banks down to the present 18 EESOUECES OF CALIFORXIA. head of the gulf, thus cutting off from its connection with the ocean that part of the gulf now dry. The evaporation in this desert far exceeds the fall of rain ; so it was not long before this lake was dried up. When the Colorado River is very- high, it breaks over its banks about forty miles southward from Fort Yuma, and sends a large stream, called New River, northwestward a distance of a hundred miles or more, to the lowest portion of the desert. A proposition has been made to cut a canal from the river to the low ground ; so that the land, which is said to be of excellent quality, might be irri- gated and cultivated : but no accurate survey has yet been made of a route for the canal, or of the district to be irrigated. The Colorado River is navigable to Fort Yuma, a distance of seventy-five miles from its mouth. The average depth is ten feet, but there are shoals which have not more than two feet at low water ; the tide rises ten feet. The channel is crooked, and the bottom is of sand, which is constantly changing posi- tion. The banks of the river are low and muddy. The aver- age current runs at the rate of two and a half miles per hour. The river is high in July, when the snows of the Rocky Moun- tains (in latitude 3 8°-44°) melt, and then the flood covers the low bottom-land along the river-banks. § 19. Area of the State. — The total area of the state amounts to about 155,000 square miles, of which there are, at my esti- mate, 42,000 in the mountains and valleys of the coast, 40,000 in the Sierra Nevada and its plateau, 20,000 in the low land of the Sacramento Basin, 30,000 in the Great Basin of Utah, 15,000 in the Colorado Desert, and 8,000 in the Klamath Basin. In the 42,000 square miles of the coast slope, 16,000 may be put down as valley and 26,000 as mountain. CM.IMATP.. 19 CHAPTER II. CLIMATE. § 20. General Remarks. — The climate of California is nn- lite that of every other country, and particularly dissimilar to that of the American states east of the Rocky Mountains. In general character it resembles the climate of western Europe. Its chief peculiarities, as distinguished from the Eastern states, are, that the winters are warmer ; the summers — especially at night — cooler ; the changes from heat to cold not so great nor so frequent ; the quantity of rain less, and confined principally to the winter and spring months ; the atmosphere drier ; the cloudy days fewer ; thunder, lightning, hail, snow and ice, and the aurora borealis, rarer ; the winds more regular — blowing from the north for fair weather, and from the south for storms ; and earthquakes more frequent. The state reaches through nine and a quarter degrees of lati- tude, from 32° 45' to 42°, San Diego being as far south as Charleston, and Crescent City as far north as Providence. Much of the Golden state has the winter of South Carolina, and the summer of Rhode Island. The orange, the lemon, the oUve, the fig, the pomegranate, the vine, the peach, the apple, wheat, and barley, all find most congenial climes in Califor nia. . The state, indeed, has many climates : one for the western slope of the Coast range between Point Conception and Cape Mendocino ; another for the low land of the Sacramento Basin ; 20 RESOTTECES OF CALIFORNIA. another for the Sierra Nevada and Klamath Basin ; another for the Great Basin of Utah ; another for the coast south of Point Conception ; and still another for the Colorado Desert. The causes of these peculiarities of climate are chiefly to be found in the position of the country — a narrow strip on the western side of the continent, bounded on the east by a high range of mountains that shuts the coast ofi* from all the influ- ences of the interior; bordering on the w^ide Pacific Ocean, washed by a warm current flowing across from the China Sea ; with a shore line that runs nearly north and south, and is ex- posed in all its length to the strong winds constantly blowing southeastward over the ocean. § 21. Temperature of the Middle Coast. — On the coast, between latitudes 35° and 40°, there is little diflerence in the temperatures of winter and summer. San Francisco is in the same latitude with Washington and St. Louis, but knows nei- ther the cold winters nor the hot summers which afflict those places. Ice is rarely formed in the Californian metropolis, and never more than an inch in thickness ; and the thermometer never stays at the freezing point twenty-four consecutive hours. The lowest point which the thermometer has ever reached in San Francisco, since observations have been taken, was 22° Fahrenheit in January, 1862 ; and previous to that time it had never fallen below 25° ; while in St. Louis it goes down to 12° every winter, and remains near that figure for many consecu- tive days. The lowest figures which the mercury reached in the daytime at San Francisco, in January of the years 1851, '52, '53, '54, and '55, were respectively 30°, 35°, 41°, 25°, and 33°, showing that in thi-ee Januaries out of five no ice at all was formed in the daytime ; and when the therm(^meter fell to 25° in 1854, the weather was declared to be colder than it had ever been before, " witliin the memory of the oldest inhabit- ant." During nine years' residence in the citA', I never have seen ice formed here half an inch thick, and never saw the slightest film of it formed on water in a house. Snow some- times falls, but I have never seen the streets dressed in white. CLIMATE. 21 In St. Louis, the winter months rarely have a day which is really comfortable in the open air ; while at least half the sea- son is so in San Francisco, the sky being clear, the sun warm, and the breezes gentle, so that the weather bears a strong re- semblance in temperature to the Indi.^n summer in the upper Mississippi basin. Our coldest winter days, at noon, are as warm as the warmest in Philadelphia. On the other hand, the summers are cool or cold. In No- Tember, 1854, the lowest figure reached by the thermometer in San Francisco, was 47°, while in July of the same year it was at 46° — showing that at no time in the former month was it so cold as at one time in the latter. The mean temperature of July is 57°, twenty-one degrees lower than in Washington city. There are not more than a dozen days in the year when the thermometer rises above 80° — at which figure heat first begins to be oppressive — while in St. Louis and at Washing- ton there are in every year from sixty to ninety days that see that height. No matter how warm the day at noon, the even- ings and mornings are always cool, and blankets are necessary — at least a pair of them — as a bed-covering, every night. Although the mean temperature of summer differs little from that of winter, yet there are sometimes very warm days, which jnay be succeeded immediately by very cool nights. San Fran- cisco never sees more than three hot days in succession. When the sun has had an opportunity to rage for so long a period, the air in the interior of the state becomes so hot, that it rises rapidly ; and the ocean-winds, which must rush to supply the place, never fail to bring cool weather to the vicinity of the Golden Gate. Thus the mercury has risen (and that was its highest) to 97°, and it often f dis in July to 46° ; and such a change of fifty degrees might occur within twelve hours. The average range of the thermometer in July and August is about twenty degrees — from 50° to 70°. Yet, as the mornings and evenings are invariably cool, and the noons are not always warm, " summer clothing ' is seldom worn by men, and never for twelve consecutive hours. The common custom is, to wear 22 EESOURCES OF CALIFORNIA. woollen coats and trousers of th^ same thickness in suminer and winter. The persons who visit San Francisc6 during the summer, from the interior of the state, where the climate from May to October is much warmer, and where summer clothes are worn, are much bothered at having to bring their winter clothes with them. The editor of a Stockton paper, disgusted with the climate of the metropolis in July, expressed himself somewhat after this manner : " You go out in the morning shivering, notwithstanding the fact that you are dressed in heavy woollen clothing and under-clothing, and have a thick overcoat buttoned up to your throat. At 8.30 you unbutton two of the upper buttons; at 9 you unbutton the coat all the way down; at 9.30 you take it off; at 10 you take off your woollen coat, and put on a summer coat; at 11 you take off all your woollen and put on light summer clothing : at 4 it begins to grow cool, and you to put on your woollen again ; and by 7 o'clock your overcoat is buttoned to the chin, and you shiver until bedtime." The coolness of the summer is caused by the winds and fogs which blow in from the ocean, whose temperature at the Farallones never varies more than a degree or two from 42°. A strong wind blows along the coast from the north and north- west during almost the whole year ; and it blows strongly upon the land for several hours after eleven o'clock in the morning and after five in the evening, and not unfrequently it continues the whole twenty-four hours. The common prevalence of this wind during the afternoon renders the mornings the pleasant- est part of the summer weather in San Francisco ; and tlie more delicate and fashionable ladies habitually make their calls and allow their children to go into the street only before mid-day. In June, July, and August, heavy, wet, cold mists come up from the sea at six in the evening, and continue until eight or nine in the morning. In the winter, fogs are rarer, and do not commence so early in the evenings, and the winds arc not so strong ; so that, in these respects, the whiter is the plcasanter season of the year. CLIMATE. 23 Dr. H. Gibbons, speaking of the mists and fogs at San Fran- cisco, says : " It is curious to observe the conflict between the absorbing power of the air and the supplying power of the ocean, in re- gard to moisture. Toward noon, w^hen the w^ind rises, huge columns of mist may be seen piled along the coast, three or four miles west of the city, and pouring in like a deluge upon the land. But the air of the land, w^iich is always thirsty, drinks it up Avith astonishing avidity; so that the impending wave, though in a current moving from thirty to fifty miles an hour, makes slow progress. By the middle of the afternoon it is within a mile or tw^o of the city ; and there it stands, like a solid mass of water several hundred feet in depth, rolling and tumbling toward you (not without grandeur and majesty), and threatening to overwhelm you in a few seconds. You await its coming, but it comes not ; it even recedes, to return and recede again. Not until the sun has lost his calorific power does the atmosphere reach the ^^oint of saturation ; and then, toward sunset or later, every thing is submerged by the va- pory flood. In the course of the evening the wind falls. Dur- ing the night the mist is gradually dissolved and disappears from the lower stratum of air, while it forms a heavy cloud above. About the middle of the forenoon the cloud is dis- persed by the rays of the sun. The dispersion is rapid, tlie sky often becoming entirely clear in less than half an hour. " If it be possible to distinguish between fog and mist — re- garding the former as impalpable, and the latter as composed of palpable particles of moisture — I may remark that mist be- longs only to the summer and fog to the winter climate of San Francisco. There is no mist in winter, and no fog in summer. At all seasons the drying tendency of the atmosphere is ob- servable. You notice none of those phenomena which in other climates depend on an excess of water in the air, and on sud- den changes of temperature. The moisture does not condense on your window^s, nor on the plastered walls ; salt does not liquify, nor even exhibit the slightest dampness ; and the house- 24 PvESOUECES OF CALIFORNIA. wife has no trouble in drying her clothes, provided it should not rain. In fact, the atmosphere of San Francisco, in spite of sea winds and mists, is a dry atmosphere." The mean temperatures of spring, summer, autumn, and win- ter, are 54°, 57°, 56°, and 50° respectively, showing a difference of only seven degrees between the average of winter and sum- mer ; whereas a similar comparison in the climate of New York city shows a difference of thirty-nine degrees. There is a range of two degrees more in San Francisco by taking the months separately — January, the coldest month, having a mean tem- perature of 49°, and September, the warmest, a mean of 58°. October is as warm as July, and in some years it has been warmer. The mean of the whole year is 54°, a temperature that requires heavy woollen clothing for comfort. For vigor- ous, industrious men, the climate of San Francisco is the health- iest and most agreeable in the Avorld. I prefer it to all others. But, to enjoy it, a man should have warm blood, full veins, and active habits ; if he is weak or idle, he w^ill find it too cool for him. It is a climate that allows a person to be out in the open air all the time ; no hour is lost because of either exces- sive heat or excessive cold. Women do not like the climate so well as men ; it is too cool for their less vigorous constitu- tions and sedentary habits. San Francisco does not lie immediately on the ocean, but only six miles from it, and where there is a great gap to let in the winds and fogs. The nearer the Pacific, the denser and more frequent the fogs, the stronger the winds, the warmer the winters, and the cooler the summers. The great ocean is a powerful equalizer of climate : as you advance into the inte- rior, the range of heat and cold becomes greater. In the coast valleys you can choose your distance. San Rafael is ten miles from the Pacific, Petaluma twenty, Sonoma thirty, Napa thir- ty-five, Suisun forty-five, and Vaca valley fifty. Sonoma valley has a delightful climate, free from fogs and cold winds, and yet blessed with a sea-breeze which tempers the heat of every summer day to the precise degree necessary to the perfect CLIMATE. 25 happiness of a man who wishes to take life easy, and do noth- ing. Indeed, all the valleys embosomed in the Coast Moun- tains, from Humboldt Bay to Santa Barbara, have beautiful climes, which will compare favorably, I think, with the best of Italy. The summer days are always warm, rarely hot ; the mornings and evenings are clear and pleasant ; in winter, ice never forms over two inches in thickness, and if snow falls, it never lies twenty-four hours. § 22. Clear Days. — On an average, there are two hundred and twenty perfectly clear days in a year, without a cloud ; eighty five days wherein clouds are seen, though in many of them the sun is visible ; and sixty rainy. Italy cannot surpass that. New York has scarcely half so many perfectly clear days. From the first of April till the first of November, there are in ordinary seasons fifteen cloudy days ; and from the first of November till the first of April, half the days are clear. It often happens that weeks upon weeks in winter, and months upon months in summer, pass without a cloud ; that is, at a distance of thirty miles from the ocean. Near the shore, coast- clouds are frequently blown up from the sea, but they disap- pear after ten o'clock in the morning. § 23. TJie Sirocco. — One case, and only one, is on record, of a sirocco, or burning-hot wind, visiting the coast. This one was felt at the town of Santa Barbara, in latitude 34° 20', on the ocean-shore, on the 17th of June, 1859. The Gazette news- paper of that place, published six days afterward, said : "Friday, 17th June, will be long remembered by the inhab- itants of Santa Barbara, from the burning, blasting heat expe- rienced that day, and the efiects thereof Indeed, it is said that, for the space of thirty years, nothing in comparison has been felt in this county, and, we doubt, in any other. The sun rose like a ball of fire on that day ; but though quite warm, no inconvenience was caused thereby until two o'clock, p. m., when suddenly a blast of heated air swept through our streets, followed quickly by others ; and shortly afterward the atmo- sphere became so intensely heated, that no human being could 2 26 EESOUBCES OF CALIFORNIA. withstand its force : all sought their dwellings, and had to shut doors and windows, and remain for hours confined to their houses. The effect of such intense and unparalleled heat was demonstrated by the death of calves, rabbits, birds, etc. The trees were all blasted ; and the fruit, such as pears and apples, literally roasted on the trees ere they fell to the ground, and the same as if they had been cast on live coals. But, strange to say, they were only burned on one side — the direction whence came the wind. All kinds of metal became so heated, that for hours nothing of the kind could be touched with the naked hands. The thermometer rose to nearly fever-heat — in the shade. Near an open door, and during the prevalence of this properly-called sirocco, the streets Avere filled with impene- trable clouds of fine dust, or pulverized clay. Speculation has been rife since to ascertain the cause of such a terrible phe- nomenon ; but, though we have heard of many plausible theo- ries thereon, we have not been fully convinced yet : however that might be, we see its terrible effects all around us, in blighted trees, ruined gardens, blasted fruit, and almost a gen- eral destruction of the vegetable kingdom here. We hope we will never see the like again." A correspondent of a San Francisco paper wrote thus : " At one o'clock in the afternoon of the 17th instant, a burning wind came upon us from the northwest, and smote us with terror. At two o'clock, the thermometer exposed to this wind rose to 133° of Fahrenheit; at five o'clock, it had fallen to 122° ; and at seven o'clock, it stood at 77°, where it had been in the morning. During the whole time of this visitation, every om3 stayed in the house, taking good care to keep doors and win- dows closed. A fisherman who was out at sea came back with liis arms all blistered. Many calves, rabbits, and birds, died of suffocation. The greatest losses are among the vegetables. The fruit-trees are all burned ; the peai's and apples have been iiterally cooked." No similar case is mentioned in history or tradition, nor is there any explanation of this- CLIMATE. 27 § 24. Temjperatxire of the SoutherJi Coast. — The high moun- tain-spur which projects into the ocean at Point Conception seems to protect the coast south of it from the fogs, which are much rarer and warmer at Los Angeles than at San Francisco. But though the former is in latitude 34°, it is at times as cold in winter as the latter (in 37° 48'), because it is farther from the ocean, and is in sight of Mount San Bernardino and other high mountains, some of which wear snow-caps during a large part of the year. In summer, however, it is much warmer, even oppressively hot. The nights are sometimes so warm, that a sheet is as much covering as is necessary for comfort; but blankets are usually required. The coast north of latitude 40° is much colder and cloudier in summer, and has more rain than any other part of the state. § 25. Sacramento Basin. — The climate of the Sacramento Basin differs from that of San Francisco in having no fogs, faint sea-breezes, winters four degrees colder, and summers from six- teen to twenty degrees warmer. The greater heat of summer is owing to the want of ocean winds and fogs ; the greater cold of winter is caused by the distance from the Pacific, and the prox- imity of the snow-covered Sierra Nevada. While at San Fran- cisco the thermometer usually stands at 70° at mid-day, it is at 86° in Sacramento city at the same moment ; and these six- teen degrees make a vast difference, for they change comfort into oppression. And Sacramento city, lying near the great gap in the Coast Mountains, is cooler in summer than either end of the basin ; for the upper portions of both the Sacra- mento and San Joaquin valleys, nearly every summer, see days when the thermometer stands at over 100° in the shade. The county assessor of Fresno countj stated, in his annual report for 1857, that the mean temperature at Millerton during the three summer months Avas 106°. The Stockton Argus spoke thus of a great heat that was felt in Stanislaus county on the 23d of June, 1859: "The thermometer was 113° in the shade. The wind was avoided, as it was heated so, that it felt as if actually burning 28 KESOUECES OF CALIFOKNIA. the flesh — as if rushing from a hot oven. In one team of ten horses, three fell in the road, from heat ; two died, but the other recovered by pouring sweet oil in its throat. The ani- mal's throat was closed so that it could not drink, when the oil was used so as to soften the throat and open it, that it could swallow water, when it recovered. The two that died expired before such aid could be used with them. At Burton's public house, at Loving's Ferry, birds flew into the bar-room to the pitcher to get water, so tame w^ere they made by the thirst caused by extreme heat. Birds were seen to fall dead ofi" the limbs of trees in the middle of the day, from the heat, as if they were shot. The w^ind was of that burning heat never before witnessed by the settlers there since their arrival in the state." In the Sierra Nevada, the heat of the summer at mid-day is about the same as in the Sacramento valley ; but the winter is cold, and the amount of rain greater in proportion to the altitude above the sea. In places three thousand feet above the ocean-level, ice forms five and six inches thick, and snow deep enough for sleighing lies several weeks nearly every win- ter. In towns six thousand feet above the sea, the snow falls from five to ten feet deep, and covers the ground four or fivfr months in the year. In the Great Basin, the winters are cold and the summer days very hot ; but there too the nights are always cool. The Colorado Desert has exceedingly hot summer days and -warm winters, but occasional frosts in the spring and fall as w^ell as in the winter. § 26. ComjKirative Tables.— The follow^ing table shows the mean temperature of every month, and the average of the w^hole year, at San Francisco, Benicia, Sacramento, Fort Mil- ler, Fort Reading, Fort Yuma, and also at various places in other parts of the world, some of them (such as Funchal, Na- ples, Honolulu, and Mexico) being famed for the beauty and equability of their climates. In addition to the temperature, the latitude of each place is given ; CLIMATE. 29 t-t ►^ ^ > K ^! tH t> '^ o ^ o AVER- PLACES. g cr p I 1 •^ p ♦^ aq o p AGE. LATITirOE. Sau Fraucisco . . . 49 51 52 55 55 56 57 57 58 57 54 51 54 37° 48' "47 45 52 48 53 51 57 59 59 67 67 73 66 73 64 66 62 64 54 52 47 45 58 59 58 03 38 34 Sacramento 67 71 Fort» Miller 47- 53 56 62 68 83 90 83 76 67 55 48 66 37 Fort Reading . . . 44 40 54 59 65 77;82 79 71 62 52 44 62 40 28 Fort Yuma 5G 58 66 73 76 87 92 90 86 76 64 55 73 32 43 New York 31 30 38 47 57 67 73 72 66 55 45 34 51 40 37 New Orleans 55 58 64 70 75 81 82 82 78 70 62 55 69 29 57 JSteilacoom SS 40 40 54 42 42 61 48 46 63 55 53 66 60 58 65 64 62 65 63 62 64 57 57 64 52 50 60 45 44 55 39 40 52 50 49 60 47 10 51 29 19 26 London 37 52 City of Mexico . . . Naples 46 47 51 56 64 70 76 76 69 61 53 49 60 40 52 Funchal 60 60 62 63 64 67 70 72 72 67 64 60 65 32 38 Honolulu 71 72 72 74 76 77 78 79 78 76 74 73 75 21 16 Jerusalem 47 53 60 54 66 71 77 72 72 60 58 47 62 31 47 Canton 52 55 62 70 77 81 83 82 80 73 65 57 69 23 08 Nagasaki 43 44 50 61 69 77 80 83 78 66 53 47 62 32 45 By the study of this table, we can form an excellent idea of the temperature of the different portions of the state, as com- pared with each other, and as compared with those of some other countries. So far as we know, San Francisco has the most equable and the mildest climate in the world. Within the tropics there are, no doubt, many places which have a more equable temperature, but it is the equability of intense heat. Funchal, on the island of Madeira, has probably the mildest climate in the world, but in equability it is inferior to San Francisco. Benicia is thirty miles from the ocean, and has a warmer summer and a colder winter than the immediate coast. Sacramento has the climate of Naples and Jerusalem through- out the year : its summer being the same as that of Xew York, but its winter fourteen degrees warmer. Fort Reading and Nagasaki have nearly the same figures. Fort Yuma, in the Colorado Desert, in latitude 32° 45', is warmer than New Or- leans, in 29° 57'. A j-ailroad, one hundred and eighty miles long, running eastward from Oakland, a suburb of San Francisco, passing 30 EESOTJKCESOFCALIFOENIA. through Stockton and Sonora, near the Mammoth Grove of Mariposa and the Yosemite valley, to the summit of the Sierra Nevada, would enable the people near the line to place them* selves, every summer's day, in any tolerable degree of heat or cold. Fourteen miles west of Oakland is the ocean-beach, where a chilling wind blows without ceasing. Going from the coast, the traveller would gradually get into a warmer clime, until, in Stockton, he would find the thermometer indicating 100°, most of the summer noons ; and proceeding up the sides of the Sierra, he would gradually rise into greater cold, to the eter- nal frost on the summit. A branch road running south to Fort Yuma would enable the traveller to enjoy almost as great a variety of temperature in the winter. § 27. Rain. — Nearly all the rain in California falls between the first of November and the first of June — the period called the " rainy season," as contradistinguished from the " dry sea- son," which occupies the remainder of the year. Those names, however, when applied to any special season, do not signify an unchangeable number of months, but rather the term dur- ing which the rain falls or the dry weather lasts. Thus, we say that the rainy season of 1858-59 began in October, be- cause in that month the first heavy rains fell ; the rainy season of 1855-56 did not begin until December ; the dry season of 1857 began in March; and so forth. The rainy season is so called, not because the rain falls then continuously, but because it does not fiiU at any other time. There are occasional show- ers in June, July, August, and September, but they are rare and light. The following table gives the average amount of rain, in inches, which falls during the four seasons of spring, summer, autumn, and winter, at various places in California, as com- pared with the amount which falls in other places in the United States CLIMATE. 31 San Francisco . . Sacramento . , . . Fort Readinp:. . . Fort Humboldt . Fort Miller Fort Yuma. . . . San Diego Astoria Portland, Maine New York citj. Xew Orleans. , , St. Louis Rome Paris Liverpool SPUING. BUMMER. ATTTUMX. WINTEK. TEAK. 6.Gi 0.13 3.31 11.33 21.41 7.01 0.00 2.61 12.11 21.73 11.30 0.39 4.89 12.44 29.02 i:!.51 1.18 4.87 15.03 34.56 9.57 0.02 2.80 9.79 22.18 0.27 1.30 0.86 0.72 3.15 2.74 0.55 1.24 5.90 10.43 16.43 4.00 21.77 44.15 86.35 12.11 10.28 11.93 10.93 45.25 11.69 11.64 9.93 10.39 43.65 11.29 17.28 9.62 12.71 50.90 12.86 14.09 8. 71 6.29 41.95 7.27 3.39 10.89 9.31 30.86 5.53 5.92 6.51 4.68 22.64 6.19 9.78 10.81 7.32 34.10 From this table it appears that the amount of rain is about one-half as gieat^in San Francisco as in any of the American states east of the Mississippi. Here, all the rain falls in the winter and spring; there, the amounts are nearly the same in the four seasons. They have as much rain in their summer and autumn as we in our winter and spring. We have less rain than Liverpool and Rome, and about the same amount with Paris. San Diego has only one-half and Fort Yuma one- seventh the rain-fall of San Francisco, which latter place is surpassed nearly seventy-five per cent, by Humboldt Bay. At Fort Yuma, and all through the Colorado Desert, the rain comes not in the rainy season of California, but chiefly in the summer and fall, synchronous with the wet season of North- western Mexico. Unfortunately, we have no statistics of the rain-fall in the Sierra Nevada, or in the Great Basin, within the limits of this state. The least rain in San Francisco, during any rainy season since 1852, has been 19 inches; the largest amount, 24 inches. I obtain the following figures from statistics kept in this city by Mr. Thomas Teimant, from 1850 to the present time: The average rain-fall m January is 3.52 inches. The most notable departures from that average were in 1858, when there 32 EESOUECES OF CALIFORNIA. were 9.40; in '59, only 1.28; in '60, 1.64; and in '62, 24.36 inches. The average of February is 3.67 inches ; but in 1853, the fall was 1.42 ; in '54, 8.04 ; in '56, 0.50 ; in '57, 8.59 ; in '58, 1.83 ; in '59, 6.32 ; in '60, 1.60 ; in '61, 3.72 ; and in '62, 7.53 inches. This shows a remarkable alternation. In only one year did the amount approach the average; in the others (excluding the last), the rains were very heavy and very light by turns. A dry February, after a wet December and January, is one of the pleasantest months of the year in California. The average rain-fall of March is 3.38: in 1857, the amount was 1.62; in '58, 5.55. The average of April is 2.63: in 1855, the amount was 5 inches; in '57, nothing; in '58, 1.35 ; and in '59, 0.27. The average of May is 0.63 : in 1857, the amount was 0.05 ; and in '60, 2.86. The average of June is 0.08 ; of July, 0.02 ; of August, 0.03 ; and of September, 0.15. There are no large rains recorded in any of these months. The average of October is 0.66 : but in 1854, the amount was 2.41 ; and in '58, 2.74 ; in '55, nothing. The average of November is 2.50 : in 1854, the amount was 0.34; in '59, 7.28; and in '60, 0.58. The average of December is 4,49 : in 1854, the amount was 0.81 ; in '57, 8.08 ; in '59, 1.57 ; in '60, 6.16 ; and in '62, 9.54. The rainy season of 1854-55 did not commence, it may be said, until January; for although there were 2.41 inches of rain in October, yet the amount was .only 0.34 in November, and 0.81 in December: so that the moisture from the October rain did no good to either the farmer or the miner, having been completely dried out from the earth before the rains of January came. Let us now examine the rainy seasons since 1050, and see in what months more thau three inches of rain fell. In 1851- '52, these months were December and March ; in '52-'53, De- cember, January, and March; in '53-54, January, February, CLIMATE. 33 March, and April ; in '54-55, January, February, March, and April; in '55-56, December and January; in '56-'57, De- cember and February; in '57-'58, December, January, and March; in '58-59, December, February, and March; in '59- '60, November, March, and April; in '60-'61, December and February; and in '61-62, from ISTovember to February, in- clusive. The rain of California usually comes with gentleness, and falls perpendicularly. The coast, above Humboldt Bay, re- ceives a greater amount of rain than any other part of the immediate shore ; and in this respect it resembles the humid clime of Western Oregon. At Fort Yuma the amount of rain is from one-fifth to one-seventh that at San Francisco, and it all falls during the spring and summer ; for the rainy season of the Colorado Desert does not come at the same time with that of the remainder of the state, but is synchronous with the rainy season of Northwestern Mexico. The rain along the middle coast of California usually comes slowly, and falls gently and perpendicularly. Here it is very seldom that two inches of rain fall in a day, and three inches have not fallen within twenty-four hours in ten years ; while in the Eastern states the former figure is reached frequently, and the latter every year — where also the rain is generally accompanied with violent and long-continued storms of wind. The rains of the Sierra Nevada are far more abundant in quan- tity, and fiercer in the manner of their coming, than those about the bay of San Francisco. It is established that the amount of rain, and its equivalent snow, increases on the west- ern slope of the Sierra Nevada with the elevation ; but our statistics are not sufficiently extensive to enable us to deter- mine whether the increase is in regular ratio to the altiti»le, or what the proportions are between the snow and rain at difier- ent heights. It is, however, an unquestioned fiict that, in or- dinary seasons, the amount of rain at Sonora, two thousand five hundred feet above the sea, is from twice to thrice as great as in Stockton, only seventy miles distant, at the sea-level; 3'i EESOUKCES OF CALIFORNIA. and the same difference is observed between Nevada and Mar rysville, wliich bear similar relations of distance and elevation to each otlier. The statistics given in the preceding part of this section relative to the amount of rain-fall at San Francisco, are intend- ed to represent ordinary years, such as all those between 1847 and 1860. But the winter of 1861-62 proved to be an ex- traordinary season, the amount of rain being double that which has fallen in any other winter since the American conquest. The average rain-fiill during the winter months at San Fran- cisco is about 12 inches; whereas, between the 1st of Novem- ber, 1861, and the 1st of February, 1862, 37 inches fell in San Francisco, and during the same period 101 mches fell in So- nera, Tuolumne county. During the four months from the 1st of November, 1861, to the 28th of February, 1862, inclusive, 45.53 inches of rain fell in San Francisco, viz. : 4.10 in Novem- ber ; 9.54 in December ; 24.36 in January ; and 7.53 in Feb- ruary. This rain caused a great flood, which did much damage along most of the rivers, and especially in the Sacramento Basin, where Sacramento City, Stockton, Marysville, and nu- merous minor towns, were completely inundated, and the whole central part of the basin, including an area one hundred and fifty miles long and twenty miles wide, was converted into a great lake, which covered the land to a depth varying from two to ten feet for more than a month. The long dura- tion of the flood, its great height, and the vast damage which it did, will render it an epoch in the history of the state, and make it well worthy of study, especially so for as relates to the Sacramento Basin, where the most serious injury was done — that basin extending north and south from Mount Shasta to the Tejon Pass, a distance of four hundred and flky miles ; and east and west from the summit of the Coast Range to that of the Sierra Nevada, a distance of one hundred miles. These two ranges unite at the two ends of the basin, w^hich has its outlet in the middle, where the Sacramento from the north and the San Joaquin from the south, having united their waters in CLIMATE. 35 blitude 39°, break through the Coast Mountains to reach the Pacific. It may be said that the waters of these streams, aftei their union, pass through three straits: one at the Golden ihite, one hundred feet deep and a mile wide ; one at the straits of Carquinez, fifteen feet deep and three-quarters of a mile wide, thu'ty-five miles from the ocean ; and one near the ^ head of Suisun Bay, half a mile wide and ten feet deep. The Golden Gate and the straits of Carquinez afi:brd an abundant outlet for all the water from the interior, but not so with the pass at the head of Suisun Bay. The land at this place is low — not more than six or eight feet above low-water mark — for a width of three miles, beyond which there are hills, which prevent the spreading of the water to a greater distance. The river is shallow and crooked ; the banks lined with bushes and covered with tules, which obstruct the passage of the water in time of flood. During the flood of January, 1862, there was very little perceptible increase in the height of the water in San Fran- cisco and Suisun Bays above the level of ordinary high tide. But there was no flow of the tide ; a continual ebb of thick, muddy water, poured out at the Golden Gate for weeks to- gether, discoloring the sea to a distance of forty miles from land. In the bays the water became almost fresh, and the planted oysters were killed by it in their beds near Oak- land. We may presume, since thirty-six inches of water fell at San Francisco from November to January inclusive, of 1861- '62, that the same amount fell in all the low lands of the Sac- ramento Basin, nearly one-half of its area. We may presume further that the amount which fell at Sonora is a fair repre- sentation of the amount which fell on the Sierra Nevada, one- half of the area of the basin. But possibly snow, which has not yet melted, formed one-third of the snow and rain which fell on the Sierra Nevada. It is not, therefore, necessary to take any account of that third, in this consideration of the flood of 1862 — written, as it is, before the waters have g;one down. 36 EESOUUCES OF CALIFOENIA. There was, then, a f^ill of three feet of water over an area of about twenty-two thousand five hundred square miles, and a fall of eight and a half feet over an area of fifteen thousand square miles. This would give us an average of five and one- fourth feet over an area of thirty-seven thousand five hundred square miles. The first foot was absorbed by the sand and earth, dried during a very arid summer and fall; and then there were four feet of water to escape through an outlet half a mile wide, from an area nearly as large as England, or the state of Ohio. The outlet proved insufficient: the waters heaped them- selves up in the lowest part of the Sacramento Basin, the size of wliich low portion I have already given as one hundred and fifty miles long and twenty wide, or an area of three thousand square miles. Now, four feet of water over an area of thirty- seven thousand five hundred square miles, Avill, if collected within three thousand square miles, form a body forty-eight feet deep ; and that figure represents the amount of water that had to escape through the Sacramento River, below the mouth of the San Joaquin. It is to be observed that, as the outlet of the Sacramento Basin is in its centre, so the freshets come simultaneously from the north and from the south. The rains fall along the whole length of the Sierra Nevada at the same time ; and as the mountain-streams are short and swift, they pour down their floods immediately and all together. Such are the circumstances which contributed to the great flood of 1862, and may contribute to other floods in the future. During January, 1862, 24.36 inches of rain fell in San Fran- cisco, according to records kept by Thomas Tennant, Esq. ; 8.66 inches fell in Sacramento, according to Dr. T. M. Logan ; 37.79 inches fell at Downieville, according to Dr. T. R. Kibbe ; and 33.79 inches fell in Grass Valley, according to Mr. Atwood. I presume that all these figures are correct save those for San Francisco ; and while I admit the care and accuracy of Mr. Tennant, I must suspect that somebody played tricks with his gauge, upon which he could not keep a constant watch. CLIMATE. 37 Between the 1st of November, 1861, and the 1st of Febru- ary, 1862, 37 inches of rain fell in San Francisco; 75.69 in Grass Valley; 79.28 in Downieville ; 101 in Sonora; 42 hichei^ of rain and 50 feet of snow (the snow probably equalling 60 inches of water) on the summit of the Sierra Nevada at Hcn- ness Pass ; and 34 feet of snow and a great amount of rain (not measured) on the summit of the same range at the Big- Tree Road. The observations at the Ilenness Pass were kept by Mr. S. R. Dunham; those at the Big-Tree Road by Mr. Richey. There have been " rainy seasons" in California which passed without rain; and the grass, receiving no moisture in winter, spring, or summer, has remained brown for a period of eigh- teen months. But no drought — more fearful than the worst of floods — has visited the country during the last twenty years, nor have we any accurate information about those that are re- ported to have happened before that time. So long as the wind blows from the north, we expect fair weather ; when it veers to the south, rain may be expected, usually within forty-eight hours. Sometimes, after a rain, the clouds near the earth move toward the south, while those higher up are going in the contrary direction : in such case, more rain may be expected. In no part of Europe or the Atlantic states can the state of the weather be predicted or guessed with so much reasonable confidence as in California. Here it is almost a certainty that nineteen days out of twenty in summer and fall, and that ten out of twenty on an average in winter and spring, will be clear and warm. Many circum- stances of value, in furnishing grounds for predicting the state of the weather in other regions, are of no use here. In the Mississippi valley, for instance, three consecutive frosty morn- ings are considered as an almost certain indication of rain ; but in California, frosts have no such significance : for a dozen may occur successively in the coast valleys or foot-hills of the Sierra Nevada, and nobody expects rain the more on that account. 88 EESOURCES OF CALIFORNIA. § 28. Dryness of Climate. — The small amount of rain dur- ing the winter, the entire want of it during the summer, the warmth of the sun, and the great number of cloudless days, render the climate a very dry one. As one conseqence or ac- companiment of our dry climate and clear sky, it may be worth while to observe that near the ocean the clouds are rarely pic- turesque or sublimely beautiful. The magnificent sunsets, where the god of light goes down amid curtains of gold and crimson — those high-piled banks of clouds which adorn the heavens before and after thunder-showers, in thp Mississippi valley — are never seen near the coast. Dew is very rare or slight over a great part of the state. Durmg the summer and autumn, many of the rivers sink in the sand soon after leaving the mountains in which they rise ; the earth is dry and baked hard to a depth of many inches or even feet ; the grass and herbage, except near springs, or on swampy land, are dried up, and as brown as the soil on which they grew. It has been said that very hot days are less oppressive in California than equal heat in the Eastern states, because the cool nights serve to invigorate the system, and the extreme dryness of the chmate favors the evaporation of sweat, and thus keeps the body cooler than in districts where the earth is always moist. Evaporation is so rapid, that a beefsteak hung up in the air wiU dry before it can commence to putrefy. A dead rat thrown into the street, where its body is crushed by wagon-wheels so that its viscera are exposed to the air, will " dry up," and its stiff hide and meat will lie during a whole summer in a mumray-like condition. In many places, steel may be exposed to the night air for weeks without getting a touch of rust. It is common to ascribe the effects of the dryness of the atmosphere to the "purity" of the air; but it is rather the absence of moisture. I know no reason for supposing that, apart from its dryness, the air in California is purer than in any other part of the continent. It may be, however, that the CLIMATE. 39 constant decomposition of animal and vegetable manner, lying on wet ground, under a hot sun, causes the air in other states to be filled with such gases as are not set free to an equal extent here. In May and June, all California " dries up" — the rivers, the brooks, the springs, the ditches, the vegetation — and, with them, many of the resources of the country. § 29. Length of Days. — ^The shortest day in the year, the 20th of December, measures nine hours and four minutes be- tween sunrise and sunset at Crescent City, and ten hours at San Diego ; while the longest day, the 20th of June, measures fifteen hours and seventeen minutes on the southern border, and fourteen hours and nineteen minutes on the northei-n bor- der of the state — or, measuring from the beginning of twilight in the morning to the end of twilight -at night, the day meas- ures nineteen hours and forty-seven minutes on the Siskiyon Mountains, and seventeen hours and forty-three minutes at Fort Yuma. § 30. Thunder- Storms. — Thunder-storms are very rare iu California. Lightning is not seen more than three or four times a year at San Francisco, and then it is never near, but far off, playing about the peak of Mount Diablo. Thunder is still more rare. Indeed, many persons have been here for years, and cannot say that they have ever seen the one or heard the other. During eleven years' residence in the state, I have never seen a brilliant flash of lightning or heard a loud clap of thunder. Thunder-storms are sometimes witnessed high up in the mountains, and in the Great Basin ; very rarely in any of the low land of the state. In May, 1860, a house in Sonora was struck by lightning; and in February, 1861, three vessels in Humboldt Bay were struck in the same manner: and, though there were persons in the house and on all the vessels, no serious injury was done to either person or prop- erty in any case. On the 25th of May, 1860, a Chinaman was 40 P.ESOURCES OF CAJ^IFORNIA. killed by lightning near the Lexington House, on the Coloma road, in Sacramento county. The weather never has that peculiar condition which isolates everybody electrically, and then fills them with electricity. In New York, on a dry winter evening, a man dressed in wool- len and shod in w^oollen slippers, after sliding along on the carpet a few steps, will accumulate so much electricity, that when he thrusts his finger at another person, a visible spark will fly off, and he can light gas with it ! But this amusing experiment, common as it is in the Eastern states, never has been successful, and probably never will be often practised, here. § 31. ITail. — Hail is a rarity; and instead of falling in July and August, as is usual in the Eastern states and Europe, it is seen in California only, between February and May. On the 10th of May, 1856, a storm of hail-stones, some of them weigh- ing twelve pounds each, visited a small district at Butte Creek, in Shasta county. It has several times happened that hail- stones more than an inch in diameter have fallen in the Sacra- mento valley. The Aurora Borealis is seldom seen in California, perhaps not more than half a dozen times w^ithin the last ten years. The aurora of the 28th of August, 1859, seen over a great part of the world, was plainly visible in this state. § 32. Earthquahes. — Earthquakes are common in some parts of California, and especially at San Francisco, Los An- geles, and near the Tejon Pass, at the southern junction of the Sierra Nevada and Coast Mountains. They are rare at Sacra- mento, Marysville, Vallejo, and Napa. As a general rule, they are less frequent and less severe in the northe'-n than in the southern part of the state. The vicinity ot Humboldt is more often shaken than any other |)lace north of the bay of San Francisco. About a dozen earthquakes are felt in a year at difierent places in the state ; not so many at one place. Most CLIMATE. 41 of the shocks are so sliglit as to pass unnoticed by a great majority of the people; and there are j^erj-ous who have i-e- sided six or eight years in San Francisco, and many wlio have resided ten years in other parts of the state, and say they have never felt an earthquake. No person has been hurt, nor has any strongly-built house been injured, by an earthquake in California, north of latitude 35°, since the American conquest. Several brick walls have been cracked in San Francisco, but they were weak structures, built on "made ground," and would perhaps have cracked by settling, of their own weight. On three or four occasions, large four-story houses have been so much shaken, that the inmates have run out in great alarm ; but on examination it was found that the buildings were unin- jured, even in the slightest perceptible manner. On one such occasion, a friend of mine, who thought his life in great danger, and ran to save it, observed before he left his room that the water was splashed out of his basin by the movement of the house. The basin was of earthen ware, about fifteen inches in diameter at the top, six inches deep, half full of water, and it stood on an ordinary wash-stand. He sup- posed that, with another such a shock or two, the building must be in ruins ; and he was very much astonished the next morning to find that there was not the slightest crack in the plastering. His room was in the fourth story of a biick hotel. It seems that the whole building had moved together. The fear of earthquakes prevents the erection of high struc- tures for show ; and, for this reason, there is not a tall steeple in San Francisco. The largest churches have been commenced on such a plan that they might be crowned with lofty spires, but it was thought more prudent to leave them with low tow- ers. The same motive induces many wealthy families to reside in wooden houses, which are considered better fitted to resist the shocks of earthquakes. These wooden houses, it must be kept in mind, are not "framed" with mortices and tenons, as large wooden houses are usually erected in the Atlantic states, but are "Cliicago frames," held together with nails. This 3* 42 EESO URGES OF CALIFOKIilA. styl-fj of building, though introduced solely because of its cheapness and simplicity, is considered by far the most secure against earthquakes. No earthquake felt at San Francisco since 1846 has been more severe than one which visited Buffalo, New York, in 1857, as described in the America7i Journal of Science and Art for Se|)tember, 1858. On the 10th of July, 1855, an earthquake cracked the walls of twenty-six houses in Los An- geles; but no wall was thrown down, nor was any person injured. Most of the earthquakes of California are confined to very email districts. Thus, not more than one in ten of those felt in San Francisco is perceived in Sacramento. The most ex- tensive Californian earthquake of which we have any record was that of January 9th, 1857. It shook the earth from Fort Yuma to Sacramento, a distance of live hundred miles, being most severe at Fort Tejon, about half way between these two points. Loud noises, either rumbling or like explosions, were heard to accompany the shock at Tejon, San Bernardino, Visa- lia, and in the Mojave valley. The waters of the Mokelumne liiver were thrown upon the banks so as almost to leave the bed bare in one place. The current of Kern River was turned up-stream, and the water ran four feet deep over the bank. The water of Tulare Lake was thrown upon its shores ; and the Los Angeles Kiver was flung out of its bed. In Santa Clara valley the artesian wells were much affected : some ceased to run, and others had an increased supply of water. Near San Fernando a large stream of water was found run- ninsT from the mountains, where there was no water before. In San Diego, and at San Fernando, several houses were thrown down ; and at San Bueneventura the roof of the Mis- sion Chui-ch fell in. Several new springs Avere formed near Santa Barbara by the shock. In the San Gabriel valley the earth opened in a gap several miles long ; and in one place the river deserted its ancient bed, and followed this new open- ing. In the valley of the Santa Clara liiver there were large CLIMATE. 43 cracks in the earth. A large fissure was made in the western part of the town of San Bernardino. At Fort Tejon the shock threw down nearly all the buildings ; snapped off large trees close to the ground, and overthrew others, tearing them up by the roots; and tore the earth apart in a fissure twenty fee C wide and forty miles long, the sides of which rent then came together with so much violence, that the earth was forced up in a ridge ten feet wide and several feet higli. At Reed's ranch, not far from Fort Tejon, a house was thrown down, and a woman in it killed. In September, 1812, on a Sunday, an earthquake threw down the Mission Church at San Juan Capistrano, in latitude 33° 20', and thirty persons were killed. The church at Santa Inez, in Santa Barbara county, was thrown down on the same day; but the shock, according to report, was an hour later than that at San Juan Capistrano, and there was nobody in the church when it fell. At the same time the sea receded a lono- distance from the ordinary place of the water's edge on the beach of Santa Barbara ; and the people there, knowing that it would soon rush upon the shore, fled to the higher ground, and by that means alone saved their lives. These reports made about this earthquake of 1812, to Dr. J. B. Trask, by old residents, have never been contradicted, though published six or eight years ago. The old Mission Church at Santa Clara was thrown down by an earthquake in 1818. On the 15th of May, 1851, a severe shock was felt in San Francisco. Windows were broken ; mer- chandise was thrown down from shelves in stores ; and vessels in the harbor rolled heavily. On the 26th of November, 1858, nenrly every brick building in San Jose was injured by an earthquake. On the 3d of July, 1861, Amador valley, in Ala- meda county, was severely shaken. Adobe houses were seri- ously injured, chimneys toppled down, furniture was flung from side to side of the houses and much broken, and men in the fields were thrown down. A severe shock of an earthquake was felt at Fort Yuma and 44 EESOUECES OF CALTFORXIA. vicinity on the 29th of Xovember, 1852. The low grounds near the Colorado cracked open with long, wide fissures, from which water, sand, and mud, spouted up. The fissures were in some places so large, that they turned the river from its course ; and the change was so sudden, that great multitudes of fish were left to die in the mud. At the same time, the mud-volcanoes of Lower California, distant forty-five miles south westward from Fort Yuma, resumed their activity; for, although there is no record of their pre\'ious action, yet they probably existed before. A pool of hot, sulphurous water had been observed at the place by Americans since 1849. Imme- diately after the shock of 1852, the officers at Fort Yuma saw a great body of steam shoot up at least one thousand feet in the desert to the southwest ; and when, soon afterward, some of them went out to examine into the cause of it, they found the mud-volcanoes on the site of the old pool, throwing up steam, boiling water, and mud, very much like the salses far- ther north. Earthquakes, according to the common theory of Califor- nians, are electrical in their origin, or closely connected with electrical influences. Many of the strongest shocks have been preceded by a condition of the atmosphere vei-y similar to that which precedes thunder-storms in other lands. When the weather is sultry and oppressive in San Francisco, people say, " Look out for an earthquake !" And it usually comes — per- haps so faint as to be barely perceptible, and sometimes not until several hours after a change in the weather. The frequency of earthquakes in California has caused a number of persons, perhaps a hundred or more, to leave the state, and return to their former homes on the Atlantic side of the continent. And yet there they are in more danger from lightning than here from earthquakes, for there are fifty killed by lightning in the Mississippi valley for one killed by an earthquake in California. A year rarely passes that a dozen persons are not struck by thunderbolts within three himdred miles of St. Louis. [See A^ypendix, p. 464.] CLIMATE. 45 § 33. Sand- Storms. — In the Colorado Desert, and in some other districts in the southern part of the state, sand-storms, similar to the simooms of Africa, but not so dangerous, occa- sionally occur. The sand, which forms the greater portion of the soil, unprotected by sod, vegetation, or moisture, is swept away in dense clouds by every high wind, and carried many miles, a terror to man and beast. The storm stops the trav- eller, because he dare not open his eyes to the little liinty par- tides; nor can he eat, for the dust covers his food and fills his mouth: and even in the most tightly-built houses the sand penetrates and fills the air. A newspaper correspondent speaks thus of a Colorado sand- storm : "Should the traveller happen to encounter a sand-storm, however, he may not get along so smoothly. A huge, black cloud, rising from the western horizon, warns him of its ap- proach. Rapidly it spreads over the sky, darkens the sun, and the fine particles of sand are swept before the gale in a dense and sufibcating cloud ; even the larger gravel and peb- bles are sometimes lifted from the plain and carried like hail before the force of the blast. The horses are blinded, para- lyzed with fear, and no urging can induce them to go forward. Were it otherwise, to go on would be folly ; the road and sun are hid from view ; no landmarks by which to be guided — safety bids you remain. The traces are unhitched, and the horses tethered to the wagon ; the only course is to securely fasten down the sides to the wagon-top, and wait with what patience one can command until the storm has passed, which will be, doubtless, in from six to ten hours. "Once the stage encountered a sand-storm while within three hundred yards of a station ; the horses could not be in- duced to move, and there was no remedy but to stay by them till the gale had spent its force, though the station was even in sight. " T have found such a storm sufiiciently disagreeable while housed by the river-side, the fine sand penetrathig everywhere, 46 KESOUECES OF CALIFORNIA. and have no ambition to encounter one upon the central des- ert. Luckily, they are not very common in the severest aspect ; in summer, quite rare." Note. — The chief writers upon the Meteorology of CaUfornia have been, Dr. Henry Gibbons, of Alameda, and Dr. T. M. Logan, of Sacramento, whose writings have been published in the books of the Smithsonian Institute, and in the newspapers of San Francisco and Sacramento. GEOLOGV, 47 CHAPTER III. GEOLOGY. § 34. General Geological Character. — California, geologi- cally considered, belongs chiefly to the paleozoic and tertiary epochs. The carboniferous rocks are wanting, or then* exist- ence in the state is confined t,o a very small district, and has not been demonstrated even there. A tertiary sandstone, some of which is metamorphic, having lost its original stratification under the influence of intense heat, underlies the valleys of the Sacramento, the San Joaquin, and the coast, and is seen in the Coast Mountains, the Great Basin, and the Colorado Desert. Granite occupies the higher portions of all the mountainous districts, and considerable portions of the Great Basin and the borders of the Colorado Desert, The scarcity of stratified rocks is plainly discoverable by the traveller in the number and ruggedness of the mountains; only primary, eruptive, and metamorphic rocks make such steep hill-sides. The thinly- stratified rocks, with intervening layers of clay, are soon worn down by the water mto gentle slopes, and covered with fertile soil, every foot of which may be turned over by the plough, and with profit. Such is not the character of California, nearly all of which is primary or metamorphic. Many rocks besides granite and tertiary sandstone appear in irregularly-distributed patches. About Mounts Shasta and Las^jon, Castle Peak, the Marysville Bnttes, in the plateau of the Sierra Xevada, tlie Great Basin, and the Colorado Desert, there are considei-able tracts of basalt, lava, trap, and trachyte; and in other places there are small tracts. Some very remark- able hills of basalt, cnlled "Table MouTitainB," are found in the 45 RESOURCES OF CALlFORIiriA. Sierra Nevada, The largest of these is in Tuolumne county, about three thousand feet above the sea, and one hundred miles eastward from San Francisco. It is thirty miles long, three hundred to eight hundred feet high above the surround- ing country, and about a quarter of a mile wide, in many places less. The basaltic formation is evident at a distance, from the perpendicularity of the sides near the top, and the flatness of its summit, gently descending toward the west. Along the sides of the Sierra Nevada, near the line of separation between the sandstone of the valley and the granite of the higher parts of the Sierra, are found various other rocks, among which slate, quartz, and limestone, are prominent. The slates are usually soft, their cleavage often perpendicular to the horizon. Limestone is abundant about two thousand feet above the sea, between latitudes 37° 30' and 39°. It is all metamorphic, and some of it is a fine marble, which may prove of value for stat- uary. Most of it is gray in color. Metamorphic limestone is also found near Santa Cruz, near New Almaden, at Monte Diablo, and in Shasta and Siskiyou counties. It is said that some stratified secondary limestone has been found in Shasta county, but this is a matter of doubt. No secondary coal has been found in tlie state. Tertiary coal, much of it a lignite, has been found at various places in San Diego, Santa Clara, Alameda, San Francisco, San Mateo, Contra Costa, and So- noma counties, and much money has been spent in opening veins. § 35. Diluvium. — The Sacramento and San Joaquin valleys are covered with a diluvium from four hundred to fifteen hun- dred feet deep. It is composed of alternate layers of sand, gravel, and clay. The most complete information w^hich we have as to the nature of this diluvium is given in the report of the boring of an artesian well, one thousand feet deep, at Stockton. This is, I believe, the only artesian well in the Sac- ramento Basin ; at least, it is the most notable one. An at- tempt was made to bore an artesian well in Sacramento, but the auger struck a stratum of boulders about four hundred feet GEOLOGY. 49 from the surface, and was unable to pass through it. The fol- lowing is a statement of the different strata encountered in the Stockton well, and the thickness of each in feet, beginning at the surface : Black loam, 6 ; red clay, 6 ; dark-red clay and sand, 18 ; blue clay, mica, and sand, 10; blue clay, hard, highly stratified, 4; blue clay, mica, and sand, 3 ; blue clay, hard, and highly strati- fied, 4 ; green sandstone and clay, very hard, 29 ; blue clay, sand, and gravel, slightly impregnated with gold, 2 ; blue clay, sand, and gravel, 18 (100) ; green sandstone, clay, and mica, hard, 15; fine gravel, 5; gray quicksand, 15; blue clay, 8; gray sand and clay, 27; dark-blue clay and sand, 33 (203); coarse gravel and pebble-stone, 27 ; blue clay, 7 ; gray sand, 13 ; blue clay and sand conglomerated, 12 ; light-gray sand, 3 ; blue clay, 6 ; light sand, 9 ; blue clay, 1 ; fine gray sand, 12 ; dark clay, 2 ; fine gray sand, 7 (302) ; clay and sand, 10 ; coarse gray sand, 1; hght clay, 19; coarse sand, 14. (Note. — At 340 feet, in this stratum of sand, a red-wood stump was found, and a stream of water ascended to within three feet of the surface.) Light clay, 8; fine gray sand, li; light clay, r.O^ ; coarse gray sand, 20 ; clay, very hard, 4 (400) ; gray sand and clay, 5; clay, 20; coarse gray sand, 3; light clay, 15; line gray sand, 4 ; light clay and sand, 1 ; coarse gray <.and and clay, 1 ; light-blue clay, 11 ; gray sand and clay, 7; light blue clay, 15; fine gravel, 1; light-blue clay and gravel, IP (496); fine gravel, 25 ; clay and sand, 2 ; sand and clay, o : coarse gray sand, 7 ; fine blue clay, 8 ; fine gray sand, 42. /'Fote.— At 560 feet, in this stratum of sand, obtained a strean; of water, rising five feet above the surface.) Gray sand and ciay, 15 (600) ; light clay and sand, 6 ; fine gray sand, 24 ; clay and sand, 3 ; fine sand, 9 ; fine gravel, 3 ; fine gray sand, 5 ; coarse sand, 2; blue clay and sand, 8; gray sand and clay, 8; ciay and sand, 5 ; fine gray sand, 10 ; clay, 5 ; coarse gray sand, 2 ; fine light-blue clay, 4 ; hard, chocolate-colored clay, 2 ; blue day, 2 (698) ; fine gray sand, 30 ; clny and sand, 8 ; gray r^and, 4 ; light clay, 10 ; coarse sand, 6 ; blue clay, 4 ; dark clay, very 50 EES0T7RCES OF CALIFORNIA. hard, 2 ; gray sand, 4 ; blue clay, 14 ; liglit-drab clay, 3 ; very fine gray sand, 24 (807) ; light-drab clay, 1 ; light-gray sand, very fine, 27; dark-gray clay, 17; light-blue clay, very hard, 22 ; light clay, 11 ; dark, chocolate-colored clay, very hard, 10 ; light clay, very hard, 15 (910) ; fine gray sand— a good stream of water, 2 ; clay and sand, 11. (Note. — A large stream of - water was obtained in this stratum, rising seven feet above the surface.) Fine sand and gravel, 10; blue clay, 20; sand and gravel, 6 ; blue clay, 27 ; clay, gravel, and mica, 14 (1,000) ; in sand, 2. The depth of the well is 1,002 feet. The temperature of the water, as it issues from the well-surface, is 77°, the atmosphere beinc: 60° Fahrenheit. The water rises eleven feet above the surface of the plain, and nine feet above the established grade of the city. The quantity of water discharged is about sixty thousand gallons in twenty-four hours. The diluvium in the coast valleys bears a strong general re- semblance, in its material and stratification, to that of the San Joaquin valley. In many places where artesian wells have been sunk, fossil wood and bone have been found three hun- dred and four hundred feet below the surface of the ground, and two hundred feet or more below the present level of the sea. In the mountains there are also large bodies of diluvium, but the material is coarser than in the valleys, being usually a gravelly clay, deposited in distinctly-marked layers, with inter- vening strata of sand and boulders. § 36. Gold. — Gold is found in nearly all parts of California, but is most abundant on the western slope of the Sierra Ne- vada, between two thousand and six thousand feet above the sea, from latitude 37° to 40° — a district two hundred and twenty miles long by forty wide. This may be called the Sac- ramento district. It is drained by the Feather, Yuba, Ameri- can, Cosumnes, Calaveras, Stanislaus, and Tuolumne rivers. The next district in importance is in the northwestern corner of the state, including that part of the Sacramento Basin west of Shasta, and the lower portion of the Klamath valley. Next GEOLOGY. 51 is the Kern River district, including White River between 35° and 36° on the western slope of the Sierra Nevada. There are gold diggings on the San Gabriel and Santa Anita Rivers, and in the San Francisquito caiion in Los Angeles county. In the Colorado valley, fifty miles above Fort Yuma, gold has been found. IsTearly every one of the coast counties has more or less gold : it has been found in the valleys of Russian River, Putah Creek, Sequel Creek, Coyote Creek, the Salinas River, and in the earth in wdiich the city of San Francisco is built. § 37. Auriferous Lodes. — Gold is found fastened in stony veins, and loose in earthy matter : the latter called placer dig- gings, the former auriferous quartz lodes. It is the accepted theory among geologists that all gold was once enclosed in quartz lodes, and that the gold in the placers Avas obtained from the disintegration or breaking up of the lodes. The surface of the earth w^as once all rock* the earthy matter was formed by the action of air and w^ater on this rock. The earthy matter was then deposited in diluvium, among which was the gold that had existed in the rock pre- vious to its disintegration. Gold is sometimes found in granite, syenite, limestone, slate, and other rocks ; but the auriferous lodes, regularly worked, are all of quartz. Most of the quartz veins run parallel with the main divide of the Sierra — that is, north-northwest and south-southeast — are from a line to thirty feet thick, and are nearly perpendicular, dipping to the eastw^ard. They are be- tween two thousand and six thousand feet above the sea. The general color of the rock is white, occasionally bluish, fre- quently reddish-brown, the color of iron-rust, derived from the decomposition of iron pyrites. In some veins the rock is com- pact, and then it is usually very white ; in others it is full of cracks and crevices, and ready to break into small pieces with a little pounding. Most of the veins have gold in them; only a few have enough to pay for w^orking. The gold is in par- ticles of irregular shape, but with some regularity of size, scat- tered through tlie rock. The particles are seldom larger than 62 EESOURCES OF CALIFOENIA. a pea, never weigh more thnn an ounce, and often are so fine as to be invisible to the naked eye. A lode has usually a peculiar kind of particles, either large or small. Most of the gold in a lode is usually in a rich streak, near the " foot wall" or lower side, as if the metal had settled down by its gravity. The rock near the '• hanging wall" or upper side of the lode is poorest. Occasionally several rich streaks will be found in a lode — one streak with coarse par- ticles of gold, another with fine. All parts of a lode are not equally rich ; but the gold is found in spots. A lode which is very rich in one place may be very poor in another not far ofi"; indeed, there is no auriferous vein in the state known to be regularly rich for a long distance on the surface. The gold is found in streaks or pockets ; the rich streak nins downward, and has a regular dip in the lode. It is a matter of very great importance to the miner to ascertain the direction of this dip, and here is the rule : Take out some of the vein stone, and examine the wall rock carefully. In most veins it will be found that the wall has little furrows, as though the lode had been pushed upward. These farrows indicate the direction of the dip of the rich streaks. Pockets may be considered as interrupted streaks ; and when one rich pocket is discovered, others may usually be found by going down into the vein in the proper direction, and that is ascertained in the same man- ner as for continuous streaks. This is an important rule, and it is now published for the first time. I am indebted for it to J. E. Clayton, Esq., mining engineer. § 38. Placers. — The placers are of two kinds — diluvial^ or those deposited under large bodies of water, as if in a deluge; and alluvial^ or those deposited under the influence of streams of water, such as the present rivers and brooks of the country. It is evident, from an examination of the mining districts, that large tracts of auriferous ground have been deposited under diluvial influences. The same strata are found extending over wide areas, and the deposition is difTerent from that made by a river. The gold, being nineteen times heavier than water, GEOLOGY. 53 and from six to eight times heavier than the clay and stones with which it is found, has sunk to the bottom of the dikivium. Tlie best diggings are therefore near the "bed-rock." The dirt in which the gold is found is usually a stiff clay, with gravel and large stones intermixed. The common phrase " golden sands" may mislead. Pure, fine sand rarely has any gold in it ; and the richest deposits of the precious metal are in a clay so tough as to give the miner much trouble to dis- solve it, with stones in it weighing from a pound to several hundred weight. The character of the pay-dirt varies greatly. A hill of diluvium may be three hundred feet deep, with a dozen strata of different material, and all of them auriferous in different degrees. In some places the pay-dirt is full of boul- ders, weighing several hundred pounds or more ; in other places the stones are all about as large as a man's head ; in others, as large as a hen's egg. In one stratum the dirt is red, in another blue, in another brown. In some places the dirt was deposited in basins of rock, four or five miles across, and from ten to fifty feet deeper at the centre than at the rim. The placer-diggings are all found in a very rough, mountain- ous country. The gold has not been carried far ; its weight has anchored it near its mother-vein. There may be much gold in the Sacramento valley ; but if so, it is deposited be- neath one thousand feet of diluvium, and nine hundred feet below the level of the sea, where it will never be disturbed. The diluvial placers are in what are called hill and flat dig- gings; the alluvial, made by streams running through the diluvium, are in rivei'-beds, bars, ravines, and gullies. The alluvial placers, as a general rule, are richer than the diluvial. The streams have carried away much of the dirt, and left nearly all the metal. Most of the gold of the rivers comes from gullies. There is a gully on a mountain : it is dry, ex- cept during heavy rains ; it has steep sides. The rain comes ; the water pours down its sides, fiercely sweeping clay, gravel, and gold along. Tlie bed of the ravine is not so steep as the Bides ; most of the gold stops there ; the dirt is carried away 54 EESOUKCES OP CALIFORNIA. into the river, with a little gold. A thousand such gullies, contributhig each a little gold, make a river rich. The heav- ier particles are deposited in the middle of the river-bed ; many of the smaller particles are deposited at the sides. The richest spots in gullies are usually where the bed-rock is full of crev- ices, as where slate, with perpendicular strata, crosses the gully. In those parts of a gully where the bed is very steep, there is usually less gold than in spots nearly level. In rivers, the richest spots are usually just below canons, where bars are formed. Wherever there are eddies at times of high water, there the gravel, clay, and gold will be deposited; and when the river falls, a bar is exposed. The richest bars of California ^A)2i\Q been found at the mouths of canons. /y/^ § 39. Mineralogy of Gold. — The particles of gold in quartz ' are usually very rough in sha])e, but sometimes they are in octahedral crystals, and at others in smooth, leaflike sheets. "Very rarely specimens of crystals are found, clustered together so as to resemble pieces of coral. Placer-gold, called " gold dust," is fine and coarse. The fine is in scales^ grains^ flour^ shot^ and icire. Flour-gold is very fine dust. Grain-gold is in particles about as large as the end of a pin. Scale-gold is in scales from a sixteenth to an eighth of an inch across, and as thick as heavy wrapping-paper. Shot-gold is in roundish particles, the size of a pin-head. Wire-gold is in small wires, from an eighth of an inch to an inch long, and as thick as a pin. Sometimes the wires are fluted, or hollow on one side ; and sometimes they are knotted together. Coarse gold is coarse-shot, pea, bean, moccasin, cucumber- seed, pumpkin-seed, large wire, and miscellaneous coarse. The pea, bean, cucumber-seed, and pumpkin-seed varieties of gold, have particles resembling in shape the seeds whence they derive their names. The coarse-shot is in particles re- sembling coarse shot in shape and size. Moccasin-gold is in pieces resembling a low shoe or moccasin in slinpe, ar.d about GEOLOGT. 55 half an inch long. Large wire-gold is in wirelike pieces, about a sixteenth of an inch thick, and from a quarter of an inch to an inch long. Miscellaneous coarse gold is in pieces of very irregular shape and size. Fine gold is often found without any admixture of coarse ; coarse is rarely found without some admixture of fine. The difierent varieties of gold are often found separate from each other. One gully will have scale gold, another fine wire- gold, another moccasin-gold, another pumpkin-seed gold, and so on. These difierent varieties of gold are frequently found very near to each other : a cucumber-seed gully will not be more than a hundred yards from a pea gully. There is a small hill in El Dorado county ; all the gold on one side is fine, all on the other coarse. The gold as it originally comes from the quartz is rough, but by friction among the gravel and sand it becomes smooth. Where all the pieces of gold are rough, it has not moved far from its maternal lode ; where all the par- ticles are small and smooth, the presumption is that it has moved a considerable distance. The larger the stream, the finer and smoother its gold, as a general rule. Most of the gold now obtained is miscellaneous coarse ; the little gullies which yielded the delicate varieties are now nearly all exhausted. Most of the placer-gold is coarse, in pieces worth half a dol- lar or more. Pieces worth five dollars are very common, and numberless nuggets worth one hundred dollars or more have been found in California. The largest nugget of gold on rec- ord was found at Ballaarat, Australia, on the 9th of June, 1858 ; it weighed two hundred and twenty-four pounds Troy, of nearly pure gold, and was called " The Welcome Nugget." The next, weighing one hundred and ninety-five pounds Troy, was found in Calaveras county, California, in November, 1854. The third, called " The Blanche Barkly Nugget," weighed one hundred and forty-five pounds Troy, and was also found m^- Australia. Smaller lumps are too numerous to mention^^x^^f placer-gold is called " dust," but the particles of the -da^are 56 BESOUKCES OF CALIFORNIA. sometimes pretty large. No satisfactory explanation has been given of the fact that placer-gold is usually in particles so much larger than that found in quartz. Gold is fine and coarse mechanically — that is, in the size of its particles — and chemically in its composition. Most metals are found in ores, combined chemically with non-m,etallic sub- stances which hide them. The ores have usually neither the color, the specific gravity, the strength, nor the other peculiar features of the metals. Native gold is never found as an ore ; it is always in a metallic form. The reason of this is, that it does not rust on exposure to the air, nor is it dissolved by any of the simple acids. And yet it is never found pure, but always mixed with silver, in nearly all possible proportions. Fre- quently copper and lead are also found in native gold. The amount of other metal in gold is designated by figures of fine- ness, estimated according to thousandths. Perfectly pure gold is 1,000 fine; gold containing one-tenth of its weight in silver is 900 fine; that is, 900 parts in 1,000 are gold, and 100 are silver. In gold 600 fine, 400 parts in 1,000 are of other metal. The native gold in California varies in fineness from 500 to 990, averaging about 880. One large piece, found at Downie- ville, was 992 fine. In Mariposa, Fresno, and Buena Vista counties, and at Mono Lake and Walker's River, east of the Sierra Nevada, the fineness is very low. The gold of the Col- orado is very fine. In other districts there are great variations in the fineness within small distances. One has gold 900 fine ; another, one hundred yards distant, has gold only 800 fine. Ordinarily, all the gold in a gully or in a river-bar is of the same fineness ; so also all the gold in a quartz-lode is of the same fineness. But there are the same differences of fineness between the gold taken from different quartz-lodes as in that taken from difterent gullies. For these differences there is no satisfactory explanation. Let us now run through the list of the principal mining dis- tricts of the state, giving the fineness of the placer-gold of each : GEOLOGY. 57 Tlie gold found in the bars and beds of the Klamath and Sabnon Rivers is in coarse particles, averaging 868 fine, and mixed with iridium. The gold of Scott River is coarser and poorer. That of the South Fork of Scott River is about 815 fine, and coarse. The gold on Trinity River, near Weaverville, is in small particles, from 885 to 940 fine. Twenty miles below Weaverville, on the same river, the gold is poorer — from 865 to 810. Still farther down, iridium becomes so abundant, that the gold is worth a dollar or a dollar and a half per ounce less than it would be if clear of that metal. In the gullies and hills near Weaverville there are rich dig- gings of coarse gold, from 890 to 960 fine. At Gold Blufi"the gold is 950 fine. The gold found at Yuba is coarse, in rough, flat particles, from 820 to 830 fine. In some lumps from Yuba little pebbles have been found hidden in their centre. The gold of most of the creeks near Yuba is from 845 to 850 fine. McAdam's Creek, near Shasta, yields gold from 875 to 885 fine. Cottonwood Creek, near the Oregon line, yields gold of the same fineness. At Oro Fino, near Yuba, the gold is in wires, and, like all w^iry gold, is of poor quality, from 760 to 780 fine. The Shasta gold is generally coarse, ranging fi-om 865 to 925 fine, except at French Gulch, where it is only 830 fine. The Pit River gold is coarse and poor, 830 fine. The Feather River gold is all good, from 890 to 920 fine. At Oroville it is from 920 to 940 fine. At La Porte, Gibsonville, and Pine Grove, in Sierra county, the diggings are deep, and the gold coarse, and from 915 to 970 fine. At Poor Man's Creek, the gold is coated with some- thing like an enamel, the color of iron-rust. When the gold is pounded, this enamel breaks off. 3 '"^ >»^' 58 KESOUECES OF CALIFORNIA. The Downieville gold is coarse, and from 895 to 925 fine. At Goodyear's Bar the fineness varies from 850 to 885. At Foster's Bar, and farther down, from 890 to 900. At Slate Creek and Canon Creek, from 900 to 910. At Forbestown, in Yuba county, the gold is 890 fine. At Camptonville, the fineness is from 920 to 970, except in one hill, which has wiry gold, 870 fine. The gold of the Middle Fork of the Yuba River is fine, from 885 to 890. That of the creeks and ravines tributary to that stream is still finer— from 900 to 920. At North San Juan the fineness is from 960 to 965. At French Corral it is 920 fine. The ffold of the Southern Fork of the Yuba River is from 890 to 900 fine. Every hill about the town of Nevada has a quality of gold difiei'ing from that of other places in the vicinity. Some of it is very good, but the general character is poor, from 800 to 850. Most of it is rough. The Grass Valley gold is poor, from 800 to 840. At Rough and Ready the gold varies as at Nevada. The gold of Yuba county is good, from 940 to 970. The Timbuctoo gold in Yuba county is 950 fine. The gold of Park's Bar is 910 fine. The North Fork of the American River has gold from 915 to 920 fine; the Middle Fork from 865 to 900; the South Fork from 915 to 920. At Iowa Hill, the gold is 900 fine ; at Michigan Blufi*, 930 ; at Forest Hill, 900; at Yankee Jim's, from 890 to 910; at Auburn, 860 ; below Auburn, and near Ophir, 820 ; and at Secret Ravine, 780. All these placers are in Placer county. At Gold Hill, in Placer county, iridium is found fastened in with the gold; the only place on the coast where the two metals are found fastened together. Next we come to El Dorado comity. The Coloma gold is good, about 915 fiu.ej' aod ^ome of the hill gold m the vicinity GEOLOGY. 59 of the town is from 920 to 930 fine. The Georgetown gold is course, and from 890 to 920 fine. At Kelsey's Diggings the fineness is 860. At Placerville the range is from 870 to 970. Coon Hollow, near Placerville, produces gold 970 fine. At Diamond Springs the fineness varies from 870 to 900. The El Dorado or Mud Springs gold is 860 fine. The gold of the Cosmnnes River varies from 865 to 875. The gold along the American River, in Sacramento county, is from 915 to 920 fine. Most of the gold in Amador county is poor, from 865 to 920. The gold about Volcano averages 870 ; Jackson, 865 to 868 ; the Buttes, near Jackson, 920. The gold of the Mokelumne River, above Mokelumne Hill, varies from 850 to 910. At the hill, some of the gold has been 980 fine. At Campo Seco the fineness is 900. Along the Mo- kelumne River are many placers where the gold is in coarse, wiry pieces, and poor in quaUty. At Vallecito, the fineness is 915 ; at San Andres, 920 ; at Murphy's, 885 ; at Douglas Flat, 890; at AngeFs, 890; at Jesus Maria, from 858 to 860; and at Carson, from 890 to 920. The gold found along the Stanislaus River is from 875 to 880 fine. Columbia, in Tuolumne county, is the best place for good gold in the state ; it ranges from 930 to 970. There are many other places where gold equally fine is obtained, but none which produces so much gold of a high fineness, with so small a proportion of poor gold. The average of the Sonora gold is 900 ; Jamestown, 870 ; Montezuma Flat, 900 ; ravines at Chi- nese Camp, 950 ; the river and creek claims at Chinese Camp, 860 ; Don Pedro's Bar, 880 ; Big-Oak Flat, 800 ; and Garote, 810. La Grange, in Stanislaus county, has gold 885 fine ; that of the Merced River is from 845 to 860 fine. The gold of Mariposa county is poor, and much of it wiry, ranging from- 700 to 820 fine, averaging about 760. Some of the gold of Mariposa county is coarse, and resembles that of 60 KESOUKCES OF CALIFOENIA. high fineness from other districts, but, on assaying, it proves to be poor. The gold from the San Joaquin River is in small scales, and about 800 fine. The Kern River gold is 630 fine. The Colorado gold is 930. The Walker's River gold is 560 ; the Mono gold 600. The above figures of the fineness of gold from various dis- tricts refer only to the placer-gold. The gold from diff*erent quartz-lodes also varies. As a general rule, the quartz-gold is not so rich as the placer-gold; but some of the gold taken from quartz is nearly as rich as any from the placers. § 40. Silver. — A large amount of silver is found in Califor- nia. One-tenth in weight of the gold-dust is silver. But it was n'ot until 1860 that valuable veins of argentiferous ore were discovered in the state. As gold predominates on the western side of the main divide of the Sierra Nevada, so does silver on the eastern side. The Washoe mines are not in Cali- fornia ; but the Esmeralda and Coso districts are. Esmeralda is in latitude 38° 15', about two hundred and fifty miles in a direct line from San Francisco in an eastward direc- tion, and just within the limits of the state, as is generally siip- posed, though some persons assert that it is in Utah. The country is mountainous ; the rock is porphyry and trap. The argentiferous veins are of a bluish-white quartz, containing sul- phuret of silver. The principal vein of the district runs north and south, and this has very little gold ; many other veins, containing considerable quantities of gold mixed with the sil- ver, run east and west. The main vein is about twenty feet wide. The ores assay from thirty to fifteen hundred dollars per ton, but the latter figure was only obtained from picked specimens. Timber suitable for firewood is abundant, and there is sufficient water to supply the wants of a small town. The Coso silver district is about one hundred and fifty miles northward from Los Angeles, one hundred miles eastward from Visalia, and twenty miles southeastward from Owen's Lake. GEOLOGY. 61 Wood and water are very scarce. Little is known about the district as yet. The Coso and the Esmerelda districts are both in the Great Basin of Utah, and about five thousand feet above the level of the sea. It is said that rich silver-mines have been discovered in the valley of the Mojave River. In the Coast Mountains, in Monterey county, a silver-mine called Allisal has long been known to exist, but it is not rich enough to pay. Similar veins are found in the Coast Moun- tains, in Santa Cruz county. Veins of silver ore are also found in Nevada county. § 41. Platinutn. — Platinum, iridium, and osmium, are three white metals resembling steel, often found in the placer mines of California. They usually occur together ; and are found more abundantly in the lower part of the Klamath valley than in any other part of the state. In many districts tliey are entirely lacking. Platinum is found in lumps by itself; iridi- um and osmium are found united, and are then called irid- osmium. These metals are found in small particles, usually fine scales ; the largest piece was of irid-osmium, found on the Lower Klamath, and weighed an ounce and a quarter. They are not found separate from the gold, nor are they ever the main object of search ; they are obtained in small quantities only, and are rarely bought and sold in the state ; they have no fixed market price. When mixed with gold-dust, they mjure its value, and prevent its reception at the mint on de- posit. § 42. QuieJcsilver. — There is probably no country in the world so rich in quicksilver as California. That metal is ob- tained only from its sulphuret or cinnabar, of which extensive deposits are found in Santa Clara county, about sixty miles southward from San Francisco, and fifteen miles from San Jose. There are three mines here — the New Almaden, the Enriqueta, and the Guadalupe. The ore is found between trap on one side, and metamorphic limestone on the other. The mines are about one thousand feet above the level of the sea. 62 KESOUKCES OF CALIFORNIA. The gangue or vein-stone is quartz. The ore varies in rich- ness from 5 to 70 per cent. : the ore of the Ahnaclen mine averages 18 per cent. ; that of the Enriqueta mine is about the same; that of the New Idria mine is about 8 per cent. The lodes are extremely irregular ; sometimes there will be a mere thread, which will widen out into a mass forty feet in breadth, twenty high, and seventy long, of rich ore, and then diminish again to a thread. The total annual production of the state will probably amount to three million seven hundred thousand pounds, of which two million four hundred thousand at least will come from New Almaden. The New Idria mines, in the Coast Mountains, about seventy-five miles southeastward from 8an Jose, furnish about three hundred and fifty thousand pounds per annum. In Napa county, on the slopes of Mount St. Helena, and in Sonoma county, in the Geyser Mountains, west of Clear Lake, cinnabar has been found, and companies are now at work opening the mines. Whether they will prove to be of value is as yet a matter of doubt. It is a singular fea- ture of the cinnabar veins in these two last-mentioned places, that they are accompanied by a porous limestone w^hich is full of pure quicksilver ; and when the stone is shaken or struck, the liquid metal flies out in minute globules. There have been rumors of discoveries of cinnabar in other parts of the state, but they are not well authenticated. § 43. Copper. — Copper ore has been found near Crescent City ; at Copper Canon, in the southwestern corner of Calave- ras county ; in San Diego county ; in Napa county ; six miles below Grizzly Flat, in El Dorado county; near Svveetland, in Nevada county ; and in Shasta county. Sulphuret of copper, or copper pyrites, is found in auriferous quartz-lodes in nearly all the mining counties. Near Sweetland, Nevada county, there is a claim in which so much copper is found with the gold, that the dust is w^orth only eleven dollars per ounce. No copper has been smelted in the state; the only attempts to mine for the ore have been at Copper Canon, and on the bank of the Cosumnes River, below Grizzly Flat. Some of GEOLOGY. 63 the Copper Caiion ore has been exported. There are rich veins of copper-ore near Crescent City, in Del Norte county ; but, with the present high prices of labor and coal, they cannot be profitably wrought. Vitreous copper is found at William- son's Pass, sixty miles from Los Angeles. § 44. Coal. — The old red sandstone and the " true carbon- iferous" rocks, as they are called, are wanting in Cahfornia ; and it was long supposed that no valuable coal would ever be discovered in the state ; but within the last year some veins of a very good quality have been found near Mount Diablo. The mineral belongs to the tertiary epoch, but contains far more solid combustible matter and less incombustible material than most tertiary coal. In the strict geological meaning of the terms, it is not " coal," but " hgnite," belonging to a later date than the true coal, and lying in a different formation. The rocks are sandstone and shale, of the upper tertiary or pliocene age, and were formed by alternating depositions in salt and fresh water. The coal-veins are situated on the north- eastern slope of Mount Diablo, are from two to nine feet in thickness, dip to the north at an average of 30°, and open on the southern declivities of the hills. A chemical analysis of some of the best specimens showed 50 per cent, of carbon, 46 per cent, of volatile bituminous substances, and 4 per cent, of ashes. The coal is bituminous in character, breaks readily, shows a bright surface where fractured, and burns with a brilliant flame. The quantity is large, and it can be profitably supplied in San Francisco at eight dollars per ton, whereas imported coal has hitherto cost twice as much. § 45. Asphaltum. — Bituminous springs are numerous near the coast, from the northern line of Monterey county to San Diego. They throw up a dark, pitch-like fluid, of a strong odor, which on exposure to the air grows thick, and finally solid. It collects in great masses about the sprimis, and in some places covers several acres of ground. After being ex- posed to the air for some time, it is called " asphaltum," which is very hard in cold weather, but grows soft at about 75°, and 64 EESOtTPvCES OF CALIFORNIA. becomes liquid at 85°. Some springs of it rise in the sea, near San Diego, and others near Santa Barbara ; and masses of the asphaltum are seen floating many miles from shore. The air at sea is even scented with it, and on several occasions frights on siiipboard have been caused by its odor, which was sup- posed to come from some hidden fire. The principal places in which these springs of asphaltum are found are the following: 1. In the Santa Cruz Mountains, in the southeastern part of Santa Clara county. A tract of twenty-five acres is here cov- ered by the hardened asphaltum. 2. In San Luis Obispo valley. The asphaltum covers thirty acres. 3. The Napoma ranch, in San Luis Obispo county. The springs are small, and yield but little. 4. On the ranch of La Purissima, in Santa Barbara coun- 5. A place six miles west of the town of Santa Barbara. The deposit of asphaltum covers three hundred acres from two to eight feet thick. 6. Rincon of San Buenaventura, Santa Barbara county. I. A place near the San Buenaventura River, twelve miles from its mouth, in Santa Barbara county. 8. A place near the Santa Clara River, eighteen miles from its mouth, in Santa Barbara county. 9. A place in the Sierra Santa Susanna, in Los Angeles county. 10. In Los Angeles valley, Los Angeles county. II. The San Pedro Hills, in Los Angeles county. 12. San Juan Capistrano, Los Angeles county. One of the deposits in Santa Barbara is so near the sea, that the mineral might be thrown w^th a shovel into a shute which w^ould carry it into the hold of a vessel at anchor. A spring of mineral oil has been found in Mattole valley, Humboldt county. This is probably the same material with that of the asphaltum springs of the southern coast. GEOLOGY. 65 Tlie asphaltum generally comes up through sandstone. The springs of Santa Barbara seem to have ceased to flow, while those in Los Angeles county are still active. It is supposed that the amount lying on the surface at the various deposits is not less than five thousand tons. § 46. Other Minerals, — Iron pyrites, or the sulphuret of iron, is found with gold in many of the quartz-veins. Iron is found also in a number of chalybeate springs. Iron-ore con- taining, it is said, 83 per cent, of metal, has been found near Auburn, in Placer county ; and the assessor of Shasta county, in his report for 1857, said "rich iron-ore" had been found in that county. Magnetic iron-ore is found in the Canada de las Uvas, and at Williamson's Pass. Tin-ore, of the kind called " tin-stone," of a rich quality, has been found in a large vein at Temascal, in San Bernardino county ; and it is reported that another lode of similar charac- ter has been found in the valley of White River, Buena Vista county. Galena has been found in Humbug valley, Siskiyou county ; in Tuolumne county ; and on the banks of the Cosumnes River, in El Dorado county. Plumbago has been discovered near Columbia, Tuolumne county. Cobalt is found, in various ores, in many counties in the state. At San Emidio, about twenty miles westward from Tejon Pass, is a rich and large lode of sulphuret of antimony ; the vein is from four to twelve feet thick, and is about six thou- sand feet above the level of the sea. Arsenic exists in many of the lodes of auriferous quartz, in the argentiferous lodes at Esmeralda and Coso, and in the an- timonial ore of San Emidio. Sulphur is abundant in California. It exists in large beds near the Geysers, in Sonoma county; near Clear Lake, in Napa county ; in San Diego county, thirty miles northward from the town of that name, and twelve miles from the sea; near the sea-shore, fifteen miles eastward from Santa Barbara; 66 EESOUECES OF CALIFOENIA. in the valley of Santa Clara "River, near its head ; and near San Juan Bautista, Monterey county. The most abundant and most accessible supply is that near Clear Lake. Alum is found in Santa Clara county, eastward of San Jose ; near Lancha Plana and Campo Seco, in Calaveras county ; at the Geysers, and at Owen's Lake. At the two last- named places there are hot alum-springs. Three miles above the forks of Clear Creek, in Shasta coun- ty, there are twenty salt springs. Springs stronj> with sulphate of magnesia, or Epsom salts, are found at the Geysers. Chalk is found in Amador county and in Sonoma county. Suisun marble, the most beautiful form of sulphate of lime, is found in Solano county. Gypsum is found in Santa Cruz and Amador counties. Fine specimens of alabaster have been obtained in El Dorado and Monterey counties. Fine varieties of porcelain clay exist in many of the mining counties, particularly in Tuolumne. Clay, suitable for making lire-bi"ick, m:i-y be obtained, near Richmond, in Honey Lake valley. Chromium is found on the bank of Feather River, near the mouth of Nelson Creek ; near the town of Nevada ; on the bank of Bear River, above Anson's Ferry ; and on the ridge between the North and Middle Forks of the American River. Chrome iron is found in Monterey county. During the summer and fall, in many parts of the state, a saline efBlorescence covers the earth, or those low parts of it where water collects during the rains of winter. This efflo- rescence is composed chiefly of carbonate and borate of soda, mixed with various other salts. The largest deposit of this kind is probably found at Soda Lake, at the sink of the Mojave River. California is very rich in borax, and the day is probably not flir distant when we shall supply a large amount of it to com- merce. It is found in springs in Tehama county, and in springs and lakes in Napa county. One of these lakes covers a hun- GEOLOGY. 67 clred and fifty acres of ground, and is strong with the sohition In the mud at the bottom of this lake, the borax is found crys- tallized in large quantities. Boracic acid has been discovered ill the sea-water near the coast, § 47. Artesian Wells. — There are a great number of art(?- sian wells in California. In Santa Clara county, within a dis- trict six miles wide by fifteen long, there are three hundred and eighteen — more than are to be found in any other district of equal size in the world. Their water is nearly all used to irrigate land; some for manufacturing purposes. They supply about two million gallons in twenty-four hours. The wells aie from fifty to four hundred feet deep ; the bore varies from six to nine inches. Only a small portion of Santa Clara valley yields artesian water ; the artesian district lies north of a line commencing at Mountain View ; thence running nine miles with the road through the town of Santa Clara to San Jose ; and thence southeast to the mountains. South of this line no artesian water is found. It is supposed that the water comes from certain subterra- nean streams. One well has abundant water at one hundred feet ; another, not more than one hundred yards distant, has no water short of three hundred feet. The wells throw up living fish and shell-fish, which are of difierent species in dif- ferent wells. Some wells throw up soft-shell clams good to eat, and of a kind not found in the superterrene waters of the state, before the opening of these artesian supplies. One well throws up a snail, with a long spiral shell ; another has snails with flat shells; 4nd others have blind fish, evidently of a spe- cies that has lived long in subterrene waters, and lost its eves because it had no use for them. Like the fish of the Mammoth Cave, in Kentucky, these artesian fish have the eye-socket and a blind eye in it. The wells that produce these fish and shell- fish are mostly shallow, not more than one hundi-ed and fifty feet deep. If put into water fresh from wells two hundred and fifty or three hundi'ed feet deep, they soon die, as do su- perterrene fish ; either, it is supposed, because the water is 68 RESOURCES OF CALIFORXIA. too warm, or because it has not enough air in it. The deeper the well, the warmer tlie water. Many of the wells have gone dry — "been drained by other wells," as people say ; but yet how can one well " drain" an- other, the mouths of both being on a level with each other ? The wells whose mouths are at a lower level may take water from those farther up the valley ; but the theory that the water deserts one well, to flow out of another of equal or higher elevation, is not sound. There is very little difference of elevation, perhaps ten feet, between San Jose and Alviso ; and the wells near the latter place throw their water about five feet higher above the surfoce than do those of the former. One cause of the failure of the wells may be the filling up of tlie pipes. From many of them great quantities of sand, gravel, and stones half a foot in diameter, have been thrown up ; and if a large stone should happen to lodge crosswise in the l^ipe, other smaller stones and gravel might soon stop it up entirely, or break the force of the current so that the water could not rise to the top. In many cases the pipe has not been driven down to the foundation ; and the water, whirling round at the bottom of the pipe, has torn away the earth and made an excavation, thus preparing the way for a caving in of tbe ground, and filling up of the well. It is tiie general opinion in Santa Clara valley that the arte- sian wells have drained away the surface-water, and the soil is much drier than it was before the wells were bored. In 1849, Dr. Bascom found water west of Santa Clai-a by digging three feet ; and since then he has been going deeper every year, un- til now his surface-well is fifty feet deep. In Pellier's garden, at San Jose, the surface-water was six feet below the surface in 1849 ; now it is fourteen. Ten years ago, there was a con- stant stream of water along the Alameda, between Santa Clara and San Jose ; but that ditch has been entirely dry for several years. A multitude of such observations are mentioned ; yet there is no conclusive proof that the artesian wells have taken avray the surface-water. It seems that the soil began to get GEOLOGY. 69 dry before these wells were bored. The artesian wells cannot draw the water from the soil immediately around them, for they throw their waters above the earth ; it may be, however, that their supplies are derived from the soil in the upper part of the valley — supplies which, if the wells were not there, would not be drained away into subterranean channels, but would go to moisteif the whole valley. It is to be observed that, at the very time when the soil of the Santa Clara valley was becoming so dry, a similar disappearance of the surface- water was noticed far beyond the influence of the artesian wells — Honey Lake, on the plateau of the Sierra Nevada, and Lake Elizabeth, in the Great Basin, both disappearing about the same time, in 1859; and several other little lakes and ponds in other parts of the country following their example, soon after. There are artesian wells at various places in the state besides Santa Clara valley, but they offer nothing new in a geological point of view, § 48. Paleontology. — It is a general rule, that the animals of former geological eras, in any given district, appear to have been the gigantic ancestors of those of the present time. Thus the kangaroo and emu of Australia, found in no other part of tlie world, were preceded by gigantic kangaroos and emus, whose fossil remains are found in New Holland only. So, too, South America, in antediluvian times, had gigantic sloths and tapirs, akin to the animals now found within her limits. Each continent has a fauna of its own, to which its antediluvian ani- mals were nearly akin. Every continent has several zoological districts ; and the ancient and modern fauna of these districts are sometimes as clearly related to each other, and as distinctly separate from those of other parts of the continent, as arc the fauna of different continents from each other. But the ante- diluvian animals of California possessed no peculiar relation- ship to the animals now indigenous in the state : the former fauna was totally distinct from that of the present age ; the fossil bones found are not numerous, and no large and valuable 70 EESOUKCES OF CALIFOKNIA. skeletons have been brought to light — only fragments here and there. Of quadrupeds, we have the remains of a mastodon, an elephant, and a new species of horse. Of birds and reptiles, nothing noteworthy has been found. We have no entire fossil hshes, but a few teeth. Dr. W. O. Ayres found near Pit River the teeth of a shark, of tlie genus Lamna — a genus now extinct on this coast. There are luinierous beds of marine shells, the most remarkable being on the shores of San Pablo Bay, on the sides of Mount Diablo, and on the slopes of the Sierra Nevada. In the bluffs of the coast, near the Lake House, are sliells iden- tical with those now^ found alive in the vicinity. All our fossils are of the tertiary period, save a few ammonites of the second- ary era, found in the northern part of the state. § 49. Relics of Early Humanity. — In May, 1859, an Indian arrow-head was found, eighty feet below the surface of the earth, at Buckeye Hill, Nevada county. About the same time, another arrow-head was found three feet deep, in undisturbed alluvium, near Freeman's Crossing, in the same county. In April, 1859, the skeleton of a man was found sixteen feet deep, at Tehaehepe, in Los Angeles county. In October, 1855, two stone mortars, such as were used by the Indians for grinding acorns and grass-seeds, were found near Diamond Springs, El Dorado county, at a depth of one hundred feet below the surface. In October, 1854, the skeletons of two men were found at Rattlesnake Bar, fourteen feet below the surface, and under ancient strata, which had apparently not been disturbed from the time of their deposition. These are a few only of the fossil evidences that California has been inhabited by men many thousands of years. § 50. Mineral Springs. — Mineral springs are very numer- ous in California. The greatest number are found in the coast valleys, from latitude 40° southward to 32°. Nearly every little vale has one or more; many of them warm or hot. The most common temperatures range from 60° to 120°. Some of these springs yield a large quantity of water, and are in ro- GEOLOGY. 71 mantic sites, destined to become places of fashionable resort when our pojnilation grows dense. There are so many of these springs in the state that there is not room here to men- tion them all. In San Bernardino valley there are a number of warm springs. Their temperatures are thus reported: 108°, 128°, 130°, 166°, 169°, and 172°. The heat of the springs at Aguas Cahentes, in San Diego county, is thus given: 58°, 74°, 130°, 136°, and 140°. Near Warner's ranch, in San Diego, is a spring with a tem- perature of 135°, rising from a cleft in the granite rock. § 51. Cortes Shoal. — About one hundred miles west of San Diego is Cortes Shoal, twenty miles long and three miles wide, with a depth of only fifteen feet in one place. This shoal is evidently the summit of a submarine ridge of moun- tains, parallel with the other ridges of tlie coast. The shoal was discovered in December, 1852, by Captain Cropper, of the steamship Cortes, who asserted that there was evidently a sub- marine volcano in operation there. The water was in violent commotion, and at intervals was thrown up into the air in col- umns ; there was an escape of steam, and he suddenly found the depth of water change from forty-five to nine fathoms. He saw also light and smoke, and at one time the place looked as though it were a ship on fire. The general opinion is, that he saw only the Avaves breaking upon the Bishop Rocks, as the rocks at the shallowest place are called ; but some persons ad- here to his opinion of a submarine volcano. XoTE. — The chief writers upon the Geology of CaHfornia are W. P. Blake, J. S. Newberry, an l Jules Marcou, in the United States Pacific Railroad Sur- vey reports, and Dr. J. B. Trask's reports to the state legislature, and Jules Marcou's book on the Geoloary of North America, For the chemical fineness of the gold in the various mining districts, I am indebted to Henry Van Yalk- eaburg. 72 KESOUKCES OF CALIFOEXIA, CHAPTER IV. SCENERY. § 52. Introductory. — California has much beautiful scenery. The atmosphere is remarkably clear, giving the eye a wide range. The mountainous character of the state not only pre- vents monotony and secures a rich variety of landscapes, but gives them extent and grandeur. The large rivers, the high snow-peaks and ridges, wide bays, forests of the largest and most graceful evergreens, parks of majestic oaks, natural mead- ows covered in the spring with brilliant grasses and flowers, are all magnificent in their kind. The valleys are mostly bare of timber, with here and there a grove of oaks, and lines of trees and bushes along the water courses. The coast val- leys are very beautiful, and in the course of ten or fifteen years, when ornamented with thorough cultivation, will be as pretty as any places in the world. Sonoma, Napa, Amador, San Ramon, and Sunol valleys may be made as beautiful as any part of the world. § 53. Coast Valleys. — Napa valley, which is now the most beautiful of these valleys, because most thickly settled and most thoroughly cultivated, is thirty miles long, five miles wide at its mouth, gradually growing narrower toward the head. Napa River, a small stream, runs through the whole length of the valley, which is of level land, bounded on both sides by steep mountains, about two thousand feet high. These moun- tains, brown near the foreground and blue in the distance, oak groves, brilliant laurel and madrona, fields of wheat and bar- ley, ploughed fields, good fences, elegant farm-houses, and nu- merous gardens and orchards, go to make up the landscape. SCENERY. 73 The valley should be seen from the mountain-top, whence it appears spread out as level as a floor. The fields, differing in color according to the season and their condition of cultiva- tion, lie like a great checker-board, over which are scattered numerous farm-houses, and irregular streaks of timber mark- ing the position of the river and its tributaries. The oak-trees form a most important part of the scene. They are wide in proportion to their height, thick in the trunk, heavy in the main boughs, many of which have a horizontal or downward course. The top of the tree has the semicircular shape, and the smaller branches have the pendant grace seen in the Eastern states only in the elm. The large upper boughs of the Cali- fornian white-oak have at their extremities some branches or twigs that hang perpendicularly down from three to twenty feet, and many of the trees for this reason look in the summer as though they were covered with vines. Add to these pecu- liarities the abundant gray Spanish moss, hanging Uke long and venerable beards from all the twigs and boughs, and the dark druidical mistletoe, and we have one of the most important and characteristic features of the Californian land- scape. Suilol valley, a little dale about three miles in diameter, nearly circular in shape, and shut in on all sides by mountains, is destined to become famous at some future day for its beauty. Now it is in a state of nature, but art will give it new charms. The places in the state most visited on account of their nat- ural scenery are the Yosemite valley, the big-tree groves, and the Geysers. 54. Yosemite Valley. — Yosemite valley is a dell of match- less cliffs and cascades, with more scenes of grandeur and beauty than can be found within an equal space in any other part of the world. Shut in closely by walls of rock almost perpendicular, from two thousand to four thousand five hun- dred feet high, it has within a radius of five miles five cas- ca<]e:s, one of which is two thousand feet high, another nine hundred and forty, another seven hundred, another six lum- 4 ^ 74. RESOURCES OF CALIFORNIA. dred, and another three hundred and fifty, and their waters flow through a natural meadow ornamented by beautiful trees and brilliant verdure. The valley is a chasm in the Sierra Nevada, four thousand feet above the level of the sea, and distant about one hundred and twenty miles in a direct line from San Francisco, and in a nearly due eastward direction. It is watered by the main branch of the Merced River, which above and below makes its way through the mountains in deep and dark gorges, the bottom of which is rarely seen by the sunhght. The valley is ten miles long and nearly three wide in the middle, from which it decreases each way. It is bounded on all sides by Avails of yellowish granite, from two thousand to four thousand feet high, in some places perpendicular, and everywhere precipit- ous. It is only at the ends of the valley that it is possible for travellers to get in or out of it, and even there the entrance and exit are difficult for horses and impossible for wagons. The general course of the valley is east and west. The main entrance is at the western end, where a steep path leads down a descent of two thousand five hundred feet. The view from the ridge overlooking the valley is splendid. The chasm is seen winding away amidst the cliffs ; a cascade is in sight, and numerous mountain-peaks rise in various directions. At the bottom of the dell are seen the meandering river, the green grass, and lofty trees diminished to the appearance of shrubs. The waterfall seen on the right several miles distant, is a mere white streak on the face of the rock, and does not appear grand in the least, but it is nine hundred and forty feet high, and be- comes imposing as the traveller approaches it. The body of water is about seventy feet wide on the first of June. The fall is called the Cascade of the Rainbow, from the beautiful colors which always, in sunhght, adorn the mist floating about it. Nearly opposite this cascade, on the northern side of the valley, and about three-quarters of a mile distant, but apparently much nearer when the tourist looks up at it, is the Capitan (or Cnptain), a rock which projects nito the valley and rises up S C E X E R T . 75 perpendicularly from the level green-sward three thousand and ninety feet. Continuing our course up the valley, we come soon to another high peak on the same side of the valley, known as the Signal Rock, two thousand nine hundred and twenty-eight feet high. Four miles above the Rainbow cas- cade we come to the great falls of the Yosemite, where tho stream of that name, eighty feet wide, leaps down two thou- sand and sixty-three feet in three falls, of which the first is one thousand three hundred feet high, the next two hundred and fifty, and the third four hundred and fifty. About three hundred feet from the top of the upper fall there is a project- ing ledge on which the stream breaks when the water is low, but up to the middle of June, while the current is large and swift with melted snow, the great body of the water leaps clear of the ledge, and pitches sheer down into the hell of rocks below. The Yosemite fill, sometimes calh d by the Indian name of "Cholook," is, in so far as height is concerned, the greatest cataract in the world; but it does not impress the observer like Niagara. The body of water, never large, is almost lost in spray before reaching the bottom ; and in the late summer, the stream dries up entirely. Niagara is sublime, overwhelming the soul with the idea of power ; Yosemite is beautiful and romantic — that is all. The tremendous precipices here, as throughout the valley, are greater and more impres- sive than the cascades, which have not enough v/ater to con- found. Besides, the falls cannot be approached from those points whence they might be seen to the greatest advantage ; and looking from a distance, the Yosemite somewhat resem- bles a great sheet of white satin hanging over the cliff. But inferior as this one cascade is to Niagara, the valley, taking all its scenery together, is far superior in variety and romantic beauty, and equal in grandeur. A day or two at Niagara is enougli ; while a lover of nature may stay at Yosemite for months and continually find new delights in the study of the scenery. I have given the total height of the three falls of the Yosemite, all of which are very near together, at two thou- 76 EESOUCES OF CALIFORNIA. sand and sixty-three feet, which is the figure given by the offi- cial surveyor of that county ; but others have estimated the height at two thousand three hundred and two thousand five hundred feet. Across from the Yosemite Falls, on the southern side of the valley, is the Pyramid Rock, so named from the shape which it bears when seen from some points of view. It is three thousand two hundred feet high. Three miles further up and at the head of the valley is " Mirror or Tocoya Lake," a beau- tiful body of water covering about eight acres. The northern side of this lake washes the foot of the North Dome, a huge mountain of rock crowned with a dome-like knob, three thou- sand six hundred and thirty feet high ; and near the southern edge of the lake is the perpendicular flxce of the South Dome, a still higher mountain, which rises up four thousand four hun- dred and eighty-one feet, towering above all the peaks in the vicinity. This peak is a sublime sight, with its perpendicular wall, which, as you look up at it, seems as if it would keep going up forever. Winding back now along the southern side of the valley, we soon come to the southern fork of the Merced River, which rushes down through a gorge. We ascend this gorge on foot, climbing with great labor over rocks and through the brush- wood, and at the distance of a mile and a half come to the Vernal or Canopah Falls, where the stream, about one hun- dred feet wide, falls three hundred and fifty feet into a basin surmounted by large evergreen trees. This cascade possesses one great advantage over all the others of the Yosemite val- ley, and that is, it can be approached from above, where we look down upon it from the top of the granite cliff, leaning over a natural parapet of rock, as convenient as though made expressly for the accommodation of picturesque tourists. About half a mile above the Vernal Fall the river takes a another leap, called the Nevada or Awanee Falls, but it costs a mile and a half of roundabout clambering to get to it. The fall is seven hundred feet high, half of which the water shoots SCENERY. 77 plumb down through the air, and strikes the projecting rock, breaking into spray. About two miles west of Nevada Falls is the cascade of Tu- sayac, about six hundred feet high, but it is very difficult of acces4S. A few hundred yards above Lake Tocoya is Lake Tesahae, wiiicli has an area of about six acres, and is forty feet deep. No description can convey a clear idea of the great variety of scenery in the valley. There are a thousand nooks and cor- ners and woody dells, full of enchanting picturesqueness. The rocky cliffs take all manner of queer forms, resembling pyramids, castles, and domes, chimneys and spires. In one place there is a narrow cleft one hundred feet deep in one of the rocks, as though some giant had commenced to split off part of the mountain and had left his work unfinished. The river, as it meanders through the valley, is a great ad- dition to its beauty ; and its waters, as well as those of the lakes, are clear as crystal in tlie summer, though turbid in the spring- Mountain trout are found in all these streams. ' The climate of the valley is cool. The numerous cascades agitate the air, and near the fall there are often gusty winds. There is much difference between the vegetation and teni- peviiture of the two sides of the valley; the northern side, where the sunshine is felt throughout the day, being m^ich warmer than the shadows of the southern cliffs. Shrubs and flowers are in the full glory of foliage, and flower along the northern wall in May and June, while the same species are still bare or budding a mile or two to the southward ; but the more delicate annual shrubs are usually more healthy on the southern than on the northern side of the stream, because those in the warmer spots are stimulated to come out so early as to be badly nipped by the frosts, which prevail here all through the spring and into the summer. The valley is almost inaccessible, on account of snow, before the middle of May, and the best time for a visit is in June. In the late summer and fall the quantity of water in these streams decreases IB KESOUKCES OF CALIFORNIA. greatly, and the Yosemite cascade becomes a mere trickling brooklet. There are a couple of houses for the accommodation of trav- ellers, but the fashionable way with those who visit the valley is to go in parties on horseback, provided with pack animals, carrying tent, bedding, provisions, and cooking utensils along. Ladies dress in the Bloomer style. Wagons do not come ■within forty miles of the valley. There are some quail and hare, but no larger game. The dell was inhabited by a war- like tribe of red men eight years ago, but they undertook to fight with the whites and have all been cut off, and scarcely a sign of their existence remains, save here and there the dim vestige of a trail. The valley was first entered by white men in 1848, if rumor be true, and afterward in 1850 and 1852, but its wonders at- tracted no notice from the press, and were unknown to the public until 1854, and did not attract many visitors until 1856. § 55. 3fmnrnoth Tree Gr(Tves. — The next great natural wonder of California is the big-tree grove in Mariposa county. It is a grove of four hundred and twenty-seven mammoth trees, the largest of which are thirty feet in diame- ter and three hundred feet in height. This is the largest spe- cies of tree in the world, and this is the largest grove of them. The grove is about twenty miles from the Yosemite valley, and thirty miles southeast of the town of Mariposa, and about four thousand five hundred feet high on the western slope of the Sierra Nevada. When the traveller enters the grove he sees on all sides of him numerous giants of the forest, varying from twenty to thirty-four feet in diameter, and from two hun- dred and seventy-five to three hundred and twenty-five feet in heicjht. Sublime siorht ! Each tree fills him with wonder as he looks at it. A glance at one of these immense trunks conveys a new idea of the magnificence of nature ; " glorious as the universe on creation's morn" is this grove. The Titans and the gods fought with such tree-trunks as these for clubs, when the attempt was made to carry heaven by storm, as re- SCENERY. 79 corded in Grecian mythology. The trees are so high that you must look twice before you can see tlieir tops, and then you must keep on looking before you can comprehend their height. The best way to see them is to lie down and look up, and re- member that the spire of the New York Trinity Church, which is the highest artificial structure in the United States, tower- ing far above all the rest of the American metropolis, though two hundred and eighty-four feet high, would be entirely lost to distant view if set down among these trees. The grove covers a space half a mile wide and three-q-uar- ters of a mile long. Classifying its trees according to their size, we find that there is one tree thirty-four feet in diameter j two trees of thirty-three feet; thirteen between twenty-fiv* and thirty-three ; thirty-six between twenty and twenty-five; eighty-two between fifteen and twenty ; making a total of one hundred and thirty-four trees between fifteen and thirty-four feet in diameter ; and then there are two hundred and ninety- three between one and fifteen feet through. One very large tree has fallen, and a considerable portion of it has been burned ; but appearances indicate that it was ^ nearly forty feet in diameter, and four hundred feet high. yy^ The Mammoth Tree is a cone-bearing evergreen, belonging to the botanical genus named Gupressus (cypress) by Linnaeus. After the time of that naturalist, his genus of the Cupressus was divided ; so that the Mammoth Tree would have come under the head of the Taxodium^ which, about the year 1850, was again divided by Endlicher, the German botanist, and the redwood-tree was declared to belong to a new genus, called Sequoia. In 1853, the mammoth trees first came to the notice of the public. The botanists in San Francisco, engaged in the tur- moil of business, looked at the specimens, but had not time to examine them, and supposed them to be of the same species with the redwood, to which the mammoth tree certainly does bear a very close resemblance. Thinking the tree, however, to be very remarkable on account of its great size, they sent 80 EESOUKCES OF CALIFORNIA. some of its cones, leaves, and wood, to botanists in New Yori, but they were unfortunately lost on the way. A few months later, an English collector sent some specimens to Professor Lindley, who not only found the tree to be of a new species, but determined to make a new genus of it, and he affixed to it the name Wellingto?iia glgcmtea. When the news of the se- lection of tliis name arrived in California, a foolish and preten- tious fellow, who meddled with matters of science of which he knew nothing, wrote a ranting article against Lindley, for try- ing to confer the honor of the great tree of America upon a Briton like Wellington, and declaring that the only proper title for the tree would be Washingtonia gigantea. If there had been any bad taste in conferring the name of a Tory and a man of blood upon such a magnificent tree, still the rules of botanical nomenclature are well estabhshed, and the matter of the name is left entirely to the discretion of the man who first gives a technical description of the plant and determines its genus. American botanists, therefore, never recognized the name Washingt07iia^ because Lindley's name w^as of undoubt- ed priority ; and to acknowledge the priority, and yet recognize the Washingtonia, would be equivalent to proving their own stupidity. And yet English botanists have, in scientific rec- ords, accused American botanists and "Americans" of making an agitation to establish the name as Washingtonia. These facts are part of the history of botany, and facts of interest relating to the big trees. The general opinion among botanists is, that Lindley was wrong in declaring the mammoth tree to be of a new genus: it is a /Sequoia., related in the closest manner to the redwood. "When the redwood and the mammoth tree come to be held as of a distinct genera, then nearly every difference heretofore considered merely specific may be made the basis for establish- ing new genera. Dr. Seeman called the mammoth tree the /Sequoia gigantea^ and it bears that name with botanists gen- erally. The /Sequoias are found only in California; the Sequoia SCENERY 81 gigardea only on the western slope of the Sierra Nevada, be- tA\een latitudes 34° and 41°. The tree h.ns the great pecu- liarity' that it bears two kinds of leaves : those on the young trees, and on the lower branches of larger ones, are about five- eighths of an inch long and an eighth wide, and are set in pairs opposite each other, on little stems; the other kinds of leaves, growing on the branches which have borne flowers, are trian- gular, about an eighth of an inch long, and they lie close down to the stem. The cones are not much larger than a hen's Qgg^ whereas the cones of many smaller conifers of the coast are larger than pine-apples. The seeds of the Sequoia gigantea are not more than a quarter of an inch long, a sixth wide, and almost as thin as writing-paper. The bark is reddish-brown in color, of a coarse, dry, stringy, elastic substance, and very thick — on the largest trees not less than eighteen inches. The wood is soft, elastic, straight-grained, free-splitting, light when dry, and red in color. It bears a close resemblance to red cedar, but the grain is not quite so even. The wood is very durable^^ The mammoth tree grows in a deep, fertile soil, and is al- ways surrounded by a dense growth of other evergreens, such as various species of pine, fir, v«;pruce, and Californian cedar. The scenery in these forests is beautiful. The trees grow very close together ; and the trunks, usually from a foot to two feet in diameter, rise in perfect perpendicularity, and with little or no diminution of size, more than a hundred feet without a limb : and while all is perfect stillness and rest and shadow on the ground, the traveller, looking to where the sunbeams are perceptible here and there on the thick foliage, can see the dexible tops swinging from side to side in the roaring moun- tain-breeze. The soil, being never visited by the sun, is always moist, and produces a luxuriant and beautiful little undergrowth of mosses, flowers, and berries. When in such forests, I have at times compared myself to a merman, who, while at the bot- tom of the ocean, amid a large growth of queer sea-weed, and surrounded by beautiful shells and the treasures of a thou- sand wrecks, should look from his abode of peace, and see 4* ^ 82 KESOUECES OF CALIFORNIA. the surface of the water, far above him, raging in a terrific storm. Many yomig trees of the Sequoia gigantea^ produced from the seed, are growing in gardens in Cuhfornia, in the Eastern states, and in Europe. The mammoth tree is found only in a few small groves, of which six or seven are known, though probably there are many in unexplored parts of the Sierra iSTevada. Three of these groves are in Mariposa county, one in Calaveras, one in Tuolumne, and one in Tulare. The three Mariposa groves are within two miles of each other. The second one in size contains eighty-six trees ; the third thirty-five. The Tuolumne grove contains ten trees, one or two of which are said to be thirty-five feet in diameter. ^.The Calaveras mammoth grove was the first discovered, and attracts the o:reatest number of visitors. There are in this grove ten trees thiity feet in diameter, and eighty -two between fifteen and thirty, making ninety-two over fifteen feet through. One of the trees, which is down, must have been four hundred and fifty feet high and forty feet in diameter. The " Horse- back ride," one of the notabilities of the place, is a hollow trunk, which a man can ride upright through on horseback, sevent;<^-five feet. In lft04, one of the largest trees, ninety-two feet in circum- feren'ie and three hundred feet high, was cut down. Five men worked twenty-two days in cutting through it with large au- gers. On the stump, which has been smoothed off", there have been dancing-parties and theatrical pei-formances ; and for a time a newspaper, called the £ig Tree Bulletin^ was printed there. At the same time that this tree was cut down, another was stripped of its bark for a distance of one hundred and sixteen feet from the ground. This tree continued green and flourish- ing two and a half years after being thus denuded, and did not begin to show signs of dying until a very hard frost came in the winter of 1856-57. Although seven years have passed SCENERY. 83 since its bark was stripped off, some of its branches are yet green. A section of bark and part of the wood of tlic felled tree are now in the Enghsh Crystal Palace. The rings of this tree were counted ; and its age was variously estimated, according to the difierent methods of counting, at from nineteen hundred to three thousand years. Probably its age was about two thousand years. It sprouted while Rome was in her glory. It is older than any kingdom, language, or creed, of Europe or America. It was a large tree before the foundation of the Christian Church, and was fifteen hundred years old before the period of modern civilization began. Twenty centuries look down upon the tourist from the tops of the larger trees; and some of the little ones will still flourish for a thousand years from now, when all our present kingdoms and republics shall have disappeared, and our political and social systems shall have been swept away as full of evil, and replaced by other and better systems, under which men will live in civUized society without each being forced to rob his brother by means more or less legal and respectable. In many of the trees in all the groves, hollows are burned at the foot, and some of them have been burned so as to stand on three legs. One of these, in the Calaveras grove, called " Uncle Tom's Cabin," has an open space under it of mora than a dozen feet square. The largest trees seem to end ab- ruptly at the top, having been broken off by the snow, which often falls to a great depth so high up on the Sierra Nevada. The trees, in some places, grow very near together ; in others, they are comparatively far apart ; and occasionally two or three will be seen which are united at the ground, although they may have been twenty or thirty feet apart when they sprouted. It is said that the big-tree grove of Tulare county is eight miles long, and contains larger trees than either Calaveras or •Mariposa, the largest measuring one hundred and twenty-three feet in circumference twelve feet above the ground. We have, however, no detailed description of this grove. 84 ^^ -BESOUECES OF CALIFORNIA. § 56. Geysers. — The Geysers, in the northern part of Sono- nm county, are among the wonders of the state. They are in a deep and steep ravine, amid a district filled with the marks of violent volcanic action. Down the western slope of the mountains which separate Clear Lake from the basin of Rus- sian River, runs a stream called the Pluton River; and near this are the Geysers, a multitude of springs, boiling with heat, and emitting large quantities of steam, with a hissing, roaring, and sputtering noise. ISTear them are many tepid and cold springs, which add to the wonderful character of the place. Hot and cold springs, quiet and boiling springs, are found within a few feet of each other. And then the waters differ as much in taste, odor, and color, as in temperature and action. One is almost as fetid at times as rotten eggs ; another has black water, resembling ink ; a third is called the " Eye-water Spring," and its waters are reputed to be excellent for curing sore eyes and cutaneous diseases ; and the waters of others are strongly purgative. The ground in the ravine is in places deeply covered with the minerals deposited by the springs : among these, sulphur, sulphate of magnesia (Epsom salts), sul- phate of aluminum (alum), and various salts of iron, predomi- nate. The chief feature of the Geysers is called "The Steampipe," an orifice about eight inches in diameter, in the hill-side, from vrhich rises a large volume of sieam to a height varying from fifty to two hundred feet. The steam roars continuously, sometimes bursting out in pufis louder than that made by the general-escape pipe. It deposits flowers of sulphur on the objects which come within its range. " The Devil's Punch-Bowl," called also " The Witches' Caul- dron," is in a large hole, six feet across, in the hill-side. The liquid in the bowl is black and thick, and is always in commo- tion with the heat, and the vapor from it deposits black flow- ers of sulphur on the rocks around. The sides of the canon are bare, and smoking with heat. The Geysers are a favorite place of resort for pleasure-seekers SCENERY. 85 in the state. They are seventeen hundred feet above the levd of the sea. >v § 57. 3fud- Volcanoes. — In the Colorado Desert, about lati- tude 33° 25', and longitude 115° 45', are some remarkable mud-volcanoes. They are in that part of the desert below the level of the sea; and if the water of the ocean were turned in upon that low land, they would be lost to sight. As it is now, they are very rarely visited, because they are in a region so desolate, that an excursion to them is accompanied by serious hardships. The volcanoes cover a space a quarter of a mile long and an eighth of a mile wide ; this area is of soft mud, through which hot water and steam are constantly escaping. The noise can be heard at a distance of ten miles, and the steam is visible at a greater distance. The quantity of water thrown up is small ; that of the steam great. The vapor rises steadily in some places, with a hissing noise ; in other places it bursts out with the noise and action of an explosion, throw- ing the mud a hundred feet into the air, with a loud report. There are places where the mud is in constant movement? and rises in great bubbles, and bursts as if boiling with intense heat ; while in other places regular cones, apparently hardened into permanency, and with shapes varying from low hillocks to sharp points, have been formed. There are boiling springs which throw up their water twenty or thirty feet ; and there are large basins, one hundred feet across, and five or six feet below the geiieral surface, in which a bluish paste is continu- ally boiling. Some of the springs are surrounded by incrusta- tions and arborescent concretions of carbonate of lime; others are encircled by deposits of sulphur. The air blown from the salses is fetid with sulphur. It is very dangerous to approach the springs and cauldrons, because the whole earth is soft in the vicinity of them, and frequently the crust is broken and thrown up with great force, to establish new spiings, steam- vents, and mud-cauldrons ; and the boiling slime or water thrown up on these occasions would suffice to kill a man in a few seconds. ^ 86 EESOTJRCES OF CALIFORNIA. § 58. Santa Cruz Ruins. — Fifteen miles northeastward from the town of Santa Cruz are "The Ruins," as they are called — forty and odd perpendicular cylinders of sandstone, from a foot to two feet in diameter, with holes from six to fourteen inches wide running through them. These cylinders were discovered in 1855, in a bed of sand, on the side of a sandstone mountain, and were at first supposed to be the remains of some work of human hands: whence their name of. "The Ruins." Much curiosity was excited by their discovery, and a number of men were employed to dig away the sand, so as to expose the foun- dation on which the cylinders stood. The excavation was car- ried down in one place to the depth of forty feet, and the base of the column was found to rest on the bed-rock sandstone. The surfice of the rock was sloping and rough, and there was nothing to indicate the work of man. It is now supposed that the cylinders were deposited by mineral springs, although it is believed that no similar columns have been formed elsewhere, the elevations made by mineral springs being, with this excep- tion alone, shaped like hillocks or cones — never like cylinders. The theory of deposition by springs may be the best mode of explaining their existence, but it is not satisfactory : the cyl- inders rise perpendicularly, or nearly so, and are very little thicker at the base than at the top ; some of them preserve the same thickness from bottom to top. The material of the shafts differs from that of the bed-rock by being coarser and darker. And besides, the texture appears in places to have a spiral form, as though it had been made of a thick paste, rolled up spirally into a cylinder, and then hardened into a solid ; leav- ing, however, a plain trace of the manner in which it was made. And some pieces, which have been broken off, suggest such a mode of formation. § 59. Mirage. — Among the most remarkable scenes wit- nessed in California are the illusions of the mirage in the des- erts of the Colorado and the Great Basin. "All the phenomena of mirage," says Professor W. P. Blake, " are exhibited on a grand scale upon the Colorado Desert. Mountain-ranges, so SCENEKY. 87 far distant as to be below tlie horizon, are made to rise into view in distorted and changing outlines. Inverted images of smaller objects, and apparent lakes of clear water, are often seen, and invite the traveller to turn aside for refreshment. The first exhibition of mirage that was seen [by Blake's party] was from the margin of the plain at Carriso Creek, looking toward the Gila, about ninety miles distant. It was early in the morning, and the eastern sky had that golden hue which precedes the rising sun. Tall blue columns, and the spires of churches, and overhanging precipices, seemed to stand upon the verge of the plain. Their outlines were changing gradu- ally, and, as the sun rose higher, they were slowly dissipated. After reaching Fort Yuma, and witnessing the strangely pre- cipitous and pinnacled outline of the mountains beyond, it was at once apparent that the mirage consisted of their distorted images. When we were upon the northern part of the desert, the peak of Signal Mountain was often distorted and raised above the horizon. The points of distant ranges also seemed at times to be elevated above the surface, precisely as the headlands of a coast sometimes appear to rise above the water at sea. " Many of the phenomena called mirage are not due to re- fraction, but are believed to be the result of reflection from the sand, or smooth surface of clay, or the polished pebbles. The smooth clay forms an excellent reflector for all the rays which are incident at a slight angle, and is most frequently the cause of the appearance of water. The beautiful surface of the pebbly plain may be regarded as a combination of myr- iads of reflectors ; for each pebble is so highly polislied, that it reflects light almost like a mirror. The reflection from such a brilliant surface, when seen at a favorable angle, looks like a sheet of water, the similarity being heightened by the motion of the stratum of heated air in contact with the surface." The phenomena of mirage are frequently witnessed in the Sacramento Basin, and also in the coast valleys, on warm, dry days. 88 EESOUKCES OF CALIFORNIA. § 60. Caves. — There are a number of caves in California. Of these the most noted are the Ahibaster Cave, seven miles from Auburn, in Placer county ; the Bower Cave, twelve miles from Coulterville, in Mariposa county ; the Cave of Skulls, in Calaveras county ; and the Santa Cruz Cave, two miles from the town of Santa Cruz. The Alabaster Cave has two cham- bers : one about one hundred feet long by twenty-five wide ; the other two hundred feet long by one hundred wide. It contains a large number of brilliant stalactites and stalagmites. The Bower Cave has a chamber one hundred feet long by ninety wide; it is reached by an entrance seventy feet long, and in one place only four feet wide. The Santa Cruz Cave has no beauty to render it attractive. The Cave of Skulls is remarkable for having contained, when first discovered, a num- ber of human skulls and bones, all covered with layers of car- bonate or sulphate of lime, from the thickness of a leaf to an inch. These bones are now in the cabinet of the Smithsonian Institute. At Cave City, and seven miles from Murphy's, in Calaveras county, is a cave in which a Know-Nothing lodge was accustomed to meet in 1855. In the bluff bank of the Middle Fork of the Cosum'nes River, eighty feet above the stream, is a cavern, called Limestone Cave, w^ith many intri- cate passages and some fine stalactites. § 61. 'Wate7'falls. — Besides the cascades of the Yosemite valley, there are a number of others in the state. There is a cataract, about five hundred feet high, on Fall River, which empties into the Middle Fork of Feather River ; one of three hundred and eighty feet, where the South Fork of the Ameri can River slides down over a convex rock, looking Hke a streak ' of snow when seen from a distance ; one of sixty feet, in the San Antonio River, in Calaveras county ; another of seventy- five, on the same stream, which falls fourteen hundred feet within a mile ; and one of three hundred feet, called the " Riffle- box Falls," in Deer Creek, Nevada county. California has five natural bridges. The largest of these is on a small creek emptying into the Hay Fork of the Trinit} SCENERY. 89 Kiver, where a ledge of rock three hundred feet wide crosses tlie valley. Under this rock runs the creek, through an arcli twenty feet high by eighty feet across. The rock above the arch is one hundred and fifty feet deep. On Lost River, in Siskiyou county, there are two natural bridges, about thirty feet apart. The rock is a conglomerate sandstone, and each is from ten to fifteen feet wide, and the distance across the stream is about eighty feet. One of these bridges is used regularly by travellers. On Coyote Creek, in Tuolumne county, teii miles northward from Sonora, are two natural bridges, half a mile apart. The upper bridge is two hundred and eighty -live feet long with the course of the water, and thirty-six feet high, with the rock thirty feet deep over the water. The lower bridge is similar in size and height to the other. § 62. Solfataras. — In the northeastern part of Plumas coun- ty are many hot springs — perhaps numbering one thousand — covering an area of ten acres. They roar and hiss so as to be heard at a distance of a mile, and their steam can be seen from a greater distance. The whole place smells strongly of sul- phur, which mineral, as well as alum and various earthy salts, abound in the soil about the springs. In four or five places in California the earth is constantly hot, and sulphureous gases and vapors are always escaping. There is such a solfatara about fifteen miles eastward from Santa Barbara; another near Owen's Lake; another near the Geysers, in Sonoma ; and another near the hot springs in Plu- mas county. It was rumored in 1858 that there was an active volcano in Plumas county, near Lassen's Peak, but there is no satisfactory proof of its existence, though there is a portion of country in that vicinity of which very little is known. § 63. Mount Shasta. — One of the best opportunities for ro- mantic adventure in the state is in the ascent of Mount Shasta. Several parties have gone to its summit — no trifling underta- king. The ascent is very difficult ; the sides of the peak are steep and rugged. The distance from the southern foot of the mountain to the summit is estimated at fifteen miles. Four 90 RESOURCES OF CALIFORNIA. miles from the summit there is a bench of trap-rock : seven miles farther is a second bench, of red cement or l:iva; thiee miles farther is a third bench, of black lava and obsidian. Near the second bench there are several lakes in cavities wnicn were once probably craters. One of them certainly was once the vent of volcanic action. On the extreme summit of tlie mountain are a number of basaltic columns, looking like chim- neys. The scenery is very grand ; for, as the peak is fourteen thousand four hundred feet high, and towers far above all the mountains around it, the view has no limit in any direction save a very remote horizon. The Klamath, Trinity, Scott, Rogue, Pit, and Sacramento valleys are all visible, besides Lassen's Peak, the Downieville Buttes, the Marysville Buttes, the Three Sisters in Oregon, and so on. About a hundred yards w^est of the summit there are a dozen steaming-hot sul- phur springs, and the earth about them is so hot as to be un- pleasant. The air is so rare at the summit of Mount Shasta, that some persons ascending it have been troubled while there with dizziness, headache, spitting of blood, and difficulty of breathing. BOTANY. 91 CHAPTER y. BOTANY. § 64. Peculiar Fauna and Flora, — California lias a botany- arid zoology of her own. Her indigenous plants and animals are peculiar to her soil. Her plants, her quadrupeds, her birds, and her lishes, are diiierent from those of other countries. The Californian vulture is, next to the condor of South America, the largest bird that flies ; and he might easily migrate to other parts of the continent, but he makes his home only in tliis state, and is certainly never seen east of the Rocky Mountains. The grizzly bear might travel almost as well, but he is found only in California and Oregon. The Californian deer is differ- ent from that of Virginia in horns, teeth, feet, color, and size. The bird known as the roadrunner or paisano might fly to all parts of the continent, but is found only west of the Sierra Nevada. There is a blue-jay here, but it differs from the bird known to the New-Englanders as the blue-jay. The robin of New England difl'ers from the robin of Old England, and the Californian robin differs from both. The sturgeon of the San Francisco market are not the same with those eaten in New York ; and one species found in California is not found in a state so near as Oregon. Our trees are like, and yet are un- like, those of the Atlantic states and Europe. We have oak juid pine, spruce, sycamore, and horse-chestnut trees, and yet any observant man sees at a glance that they differ in many impoitant particulars from the trees known by those names elsewhere. California, with a little of the country adjacent, is a distinct botanical district. Her vegetation was first pro- 92 KESOUECES OP CALIFOENIA. duced on her own soil, and has not been derived from or com- municated to any other district by the course of nature. § 65. Distribution of Plants. — Most of the Sacramento and San Joaquin valleys, the Colorado Desert, the eastern slopes of the Coast Mountains, and the Coast Range south of latitude 35°, are treeless ; the Sierra Nevada and the western slopes of the Coast Range north of 35°, have fine forests ; and in the foot-hills of the Sierra Nevada, and in the coast valleys, there are beautiful open groves of oak-trees. The timber of the Sierra is mainly spruce, pine, and fir ; that of the coast, north of 37°, redwood; and spruce and pine south of that latitude. § 66. Superiority of Co7iifers. — The botany of California is remarkable for containing a number of the largest and most beautiful coniferous trees in the world, growing to a height of three hundred feet and a thickness of eight and ten feet in the trunk, and some of them still larger. Among these gigantic olories of the veo-etable kimrdom are the mammoth tree, the redwood, the sugar-pine, the red fir, the yellow fir, and the arbor-vitoe, or IViuja gigantea. Other large conifers contrib- ute to the magnificence of our forests. We have the laurel, the madrofia, the evergreen-oak, and the nut-pine (Pinus sa- bifdcma)^ evergreen trees with a growth resembling that of deciduous trees. Our deciduous trees are few, and of little value to the mechanic. The mammoth tree [Sequoia gigantea) wa5 described in the preceding chapter. § 67. Redwood. — The redwood {Sequoia sempervirens) is the second in size and the first in commercial value of all the trees in California, though not much superior to the sugar-pine in either respect. It grows only within thirty miles of the ocean from Monterey to Crescent City, and is never found out of the state. It bears a remarkable resemblance in color and texture of wood and bark, and color, form and distribution of foliage to the mammoth tree, to which it is not much inferior in size. A redwood-tree called " Fremont's tree," in Santa Cruz county, is two hundred and seventy-five feet high, and nineteen BOTANY. 93 feet in diameter six feet above the ground ; and others equally large are found in the northwestern part of the state. Trees two hundred and fifty feet high and eight feet through are not rare. The wood is very straight-grained, free-splitting, durable, soft, and light. So freely does it split, that boards twenty feet long, eight inches wide, and an inch thick, are sometimes made from it with the frow. No w^ood in the world splits so beautifully and regularly. There is no better wood for the general use of the farmer, and it is the chief building ma- terial of the coast. No timber is more durable either above or below ground. The color is a rich dark-red, which, when var- nished, makes a fine appearance in furniture. The tree grows in dense forests, which contain an immense amount of timber. Thus, on the plain southeast of Crescent City, there are hun- dreds of acres of land of which every fifteen feet square, on an average, supports a tree three feet through and two hundred and tw^enty-five feet high — a statement that may appear in- credible to those who have seen only the forests east of the Mississippi River. These trees will often furnish twenty saw- logs, each ten feet long, and every acre wall supply material to make one million feet of sawn lumber, which, at the low rate of fifteen dollars per one thousand feet, is worth fifteen thou- sand dollars. The redwood stump, after the tree has been cut down, throws out a number of shoots, one or two of which choke down the weaker ones and become large trees. A red- wood forest is almost inexterminable. § 68. Pines. — The sugar-pine (Plnus lamhertiana) is the most magnificent tree of all the pine kind, and indeed it has no superior in the vegetable creation, save the mammoth and the redwood, the confessed monarchs of the plant kingdom. It is closely related to the white pine {Pinus strohus) of the East- ern states; "though," as Dr. Newberry says, "like all the conifers on the Pacific coast, it exhibits a symmetry and perfec- tion of figure, a healthfulness and vigor of growth not attained by the trees of any other part of the Avorld," The mature tree sometimes reaches a heii-ht of three hundred feet and a diam- 94 RESOURCES OF CALIFORNIA. eter of twenty, but it rarely exceeds two hundred and ten. The young trees of the sugar-pine give early promise of thb majesty to which they subsequently attain. They are unmis- takably young giants; even when having a trunk a foot in diameter, their remote and regnlarly-whorled branches, like the stem covered w^ith a smooth, grayish-green bark, showing tliat, although so large, the plant is still " in the milk," and has only begun its life of many centuries. The sugar-pine conspicuously exhibits one of the most geneijal and striking characteristics of the conifers — the great development of the trunk at the expense of the branches. Nearly the vx'hole growth is thrown into the trunk, which generally stands with- out a flaw or flexure, a perpendicular cone, all its transverse sections accurately circular, sparsely set with branches, which, m their insignificance, seem like the festoons of ivy wreathing about the columns of some ancient ruin. The leaves are three inches long, dark bluish-green in color, and they grow in groups of five. The foliage is not dense. The cones are large, sometimes eighteen inches long by four thick. The wood is similar to that of the white pine — white, soft, homogeneous, straight-grained, clear, and free-splitting. It furnishes the best lumber in the state for the "inside work" of houses, and is the chief building material used in the Sierra Nevada, Avhere it grows. The tree derives its name from a sw^eet resin which exudes from tlie duramen or hard wood of the tree. This resin is sugar-like in appearance, granulation, and taste, and could not be distinguished from the manna of the drug-stores except by a slight terebinthine flavor. The pine sugar is ca- thartic. It is found in small quantities only, though it is said one hundred and fifty pounds of it were collected by a man who devoted himself for a few weeks to the business of gath ering it. The Western yellow pine [Plnus jponderosd) is a noble tree, next in size among the pines of California to the sugar-pine. It so.iietimes reaches a diameter of seven feet. Its leaves grow in threes at the ends of the branches, giving the foli BOTANY. 95 age a peculiarly tufted appeai-auce. The color of the leaves is a dark yellowisii-green. The bark is of a light yellowish-brown or cork color, and is divided into large, smooth plates from four to eight inches wide and from twelve to twenty inches long, whereby the tree may be recognized at a distance. The tree is found near the snow-line in the Sierra Nevada, and east of the summit, and northward to Washington Territory. The nut-pine {Phius sabiniajia) is remarkable as a cornfer for its spreading top, and for its large cones full of edible seeds. It branches out somewhat after the manner of a ma- ple ; rarely more than sixty feet high, thoagli often with a trunk four feet through — a thickness of trunk that with most other conifers would give more than double the height. About half way from the ground to the top, the trunk divides into a number of branches, which grow upward. The nut- pine is found in the lower part of the Sierra Nevada, and in the coast mountains near the head of the Sacramento valley. The seeds are larger than the common white bean, and are very palatable, with a slight terebinthine taste. The leaves are from four to ten inches long, and grow in threes. The foliage of the tree when seen from a distance, resembles that of the willow, both in color and distribution. In places where the nut-{)ine is found, the woodpeckers select them as store- houses for their winter food, cutting holes in their bark and putting an acorn in each. The Indians formerly relied upon the nuts for a considerable portion of their food. They climbed the tree by catching hold of the rough, strong bark with their hands, then putting their feet against the tree, without touch- ing it with their body or knees, they walked up till they reached the limbs. The twisted pine {Pinus contorta) is found in the northern part of the state. The leaves are yellowish green in color, about two inches long; and they grow in pairs. The tree does not exceed sixty feet in height. Coulter's pine {Pinus coidterii) grows in the Santa Lucia mountains. It reaches a height of one hundred feet, and has 96 RESOURCES OF CALIFORNIA. a trunk three feet through. Its branches are large and spread- ing, the leaves 2. foot long and pale sea-green in color; the cones seventeen inches long, seven inches through, and like a sugar-loaf in shppe. § 69. Firs. — The red fir, or Douglas spruce {Abies douglasii)^ is a tree of very large size, growing to be three hundred feet high and ten feet thick in the trunk. It is, as Dr. Newberry says, " one of the grandest of the group of giants which com- bine to form the forests of the West." The wood is strong, but coarse and uneven in grain ; the layers of each years growth being soft on one side and very hard on the other. The timber is much used for rough work in houses, and for ship-building. The tree grows in dense foresies on the Sierra Nevada and Cascade Mountains, from 35° to 49°, and near the coast north of 39°. The yellow-fir or Williamson's spruce [Abies williamsonii) bears a close resemblance to the red fir, and the two trees are usually found in company with each other. The black fir {Abies menziesii) is smaller and of little value. The Abies bracheata (Santa Lucia fir) grows in the Santa Lucia mountains. The height is about one hundred feet, the shape a perfect cone, the lowest branches resting on the ground. The tree produces a resin used by the Catholic priests for in- cense. The Western balsam-fir {Picea grandis)^ or white fir, attains a height of one hundred and fifty feet, and a diameter of seven feet in the trunk. The bark on the trunks of the young trees contains numerous cysts full of the resinous fluid called the balsam of fir. § 70. Cedars. — The Western juniper, or cedar {Juniperus occidentalis), bears a strong resemblance to the juniper {tZu- niperus virginianus) of the Eastern states. Its wood, however, is white in color. It grows to be about thirty feet high. The wood of a juniper-tree found near the quicksilver mines of New Idria is so hard and fine in texture, that it would probably be valuable to engravers. BOTANY. 97 The Californian white cedar {Lihocedwus decnrrens) grows one hundred feet high, and seven feet thick in the trunk. It is found from Mount Shasta to the Tejon Pass. The trunk is usually angular. Many of the trees are affected with a dry-rot which destroys their value as timber. The fragrant-cedar (Ciq^ressus fragrcms) is found along the northern coast of the state. It is a large tree, and produces a white, clear lumber, valuable for furniture and the inside work of houses. The wood has a strong, lasting, and not unpleas- ant odor, half way between turpentine and ottar of roses. Lawson's cedar {Cupressus lawsoniana) is a tree of little value. The arbor-vitai, also called cedar (Thuja giganted), is a most symmetrical and graceful conifer, growing to be nearly three hundred feet high. § 71. Yew and N'utmeg.—Thii Western yew is an upright tree, from fifty to seventy-five high, with thin and light foli- age, the leaves being about an inch long. Its growth is straighter, its branches fewer, and its foliage thinner, more feathery, and fighter in color, than the European yew. It grows on the Sierra Nevada from 34° northward to British Columbia. The coast cypress ( Cupressus macro-carpus) is found only on Cedar Point, at Monterey, and there are not more than one hundred trees of it there. The foHage is very dense. The Cafifornian n aiiie. {Tor re'i a calif arnica) is a graceful and beautiful evergreen found in the Coast Mountains near the bay of San Francisco. It grows from fifty to seventy-five feet high, and resembles the Western yew in foliage and general form". The fruit is hke a nutmeg in size and shape, but it has a disagreeable terebinthine taste, and is never used as a condi- ment. § 72. Laurel— "Th^ Californian laurel, or bay ( Oreodaphne calif ornica), is one of the most common and beautiful trees of the coast valleys. It is an evergreen, which grows to a height of fifty feet, with a trunk sometimes thirty inches in diameter. 98 EESOUKCESOFCALIFOKNIA. The leaves are dark green, lustrous, four inches long, one inch wide, sharp at both ends, with smooth edges. The foliage is dense. The wood is grayish in color, very hard, durable, and difficult to spHt. Both leaves and wood have an aromatic odor, which is stronger in the former ; and becomes still stronger when the leaves are bruised. The odor resembles that of bay-rum. It gives the headache to some sensitive persons. § 73. Madrona. — ^The madrona (Arbutus menziesu) is one of the most striking trees of the Californian forest. It is an evergreen, with an open growth, somewhat like that of a maple, bright-green and lustrous leaves, and a bright-red bark. Its height is sometimes fifty feet ; its diameter in the trunk two feet. The leaves are oval in shape, three inches long, pea-green underneath, and dark and shining above. The bark is smooth, and it peels off at regular seasons ; the new bark is a pea-green, which changes to a bright red. The wood is very hard, and is used to some extent in the arts, especially for ma- king the wooden stirrups commonly used in the state. The tree bears a bright-red berry in clusters, of which the birds are fond. § 74. Mcmzanita. — The manzanita [Arctostaphylos glauca), another prominent feature in the Californian forest, is a dense, clump-like shrub, which grows as high as twelve feet, and nearly as broad as it is high. The trunk divides near the ground into several or many branches, and these terminate in a great multitude of twigs, so that the shrub is a dense mass of branches and branchlets, all of which are very crooked. The wood is dense, hard, and dark-red in color. The bark is red and smooth, occasionally peeling off and exposing a new Ught-grcen bark, which soon turns red. The leaves are regu- kirly oval in form, about an inch and a half long, thick and shining, and pea-green in color ; they set vertically upon their stems. The manzanita bears a pinkish-white blossom in clus- ters, and these are replaced by round red berries about half an inch in diameter; they have a pleasant, acidulous taste, and BOTANY, 99 are often eaten by the Indians and grizzly bears, but there is too little meat on them to pay white men for the trouble of gathering them. The shrub grows in the coast valleys, and in the Sierra Nevada, up near to the limit of perpetual snow. The name means " little apple," manzana being the Spanish for apple. § V5. Gecmothiis. — The ceanothus, sometimes called the Cali- fornian lilac, of which there are many species, is a beautiful evergreen shrub, growing about ten feet high, with clusters of hlac-like flowers, of various shades of blue, violet, and red, according to the species. The tree produces a multitude of little twigs, and a dense foliage, and may be trimmed into almost any shape. § 76. Oaks. — The Californian white oak ( Quercus hi7idsii)^ or long-acorned oak, is a very large tree, and the characteristic oak of California. It resembles the white oak of the Atlantic slope in the color of its bark and the shape of its leaves ; but its growth is very difierent. It seldom reaches a greater height than sixty feet, and is often wider than high. Some- times it measures one hundred and. twenty-five feet from side to side. The trunk, which occasionally grows to be eight feet through, throws out large horizontal boughs within ten feet of the ground, and above that point the trunk is soon lost among the large branches. The tree furnishes no straight timber, and the wood is so soft and brittle as to be of no use in the arts ; whereas the white oak of the Mississippi valley is a most valuable tree, with a trunk so tall and straight, tlmt sills and beams of it sixty feet long are common, and with a wood so tough, that it supplies all the axles and plough-beams of the country. The Californian white oak is not even tit for fence-rails. The tree, however, is very beautiful and majestic, and the open groves of it in the valleys and foot-hills form, as Dr. Newberry says, "the most important element in those scenes of quiet beauty which so often excite the admiration of the traveller in California." The tree bears much resemblance in form and size to the oak of England, the groves of it appear- 100 EESOTTRCES OP CALIFORNIA. ing like the English parks. At the ends of the large boughs are branches which hang down hke vines — giving the tree, when seen from a distance, something of the appearance of an elm. The acorns are large, sometimes two and a half inches long. They once formed the chief article of food of the Cali- fornian Indians. The evergreen oak ( Quercus agrifolia) is a low, spreading tree, much like an apple-tree in size and shape. The foliage, however, is darker and denser. The acorns are small, thin, and sharp-pointed. The wood is hard, crooked in grain, and valuable for knees in ship-building. The Californian chestnut oak ( Quercus densiflora) is a low, handsome evergreen tree, wdth a leaf very much like that of the chestnut. The bark is very rich in tannin, and is exten- sively used for the tanning of hides. The tree is rare north of latitude 39°, and is most abundant in the mountains about Santa Cruz. The Western chinquapin ( Gastanea chrysophylla)^ or golden- leaved chestnut, is an evergreen shrub that grows in the Sierra Nevada. At the height of three feet it bears an edible and palatable fruit, something like the beechnut in shape, but larger. The flowers and ripe fruit are often found on the same bush. The leaves are dark-green above, and covered Avith a yellowish powder beneath. The Western chinquapin grows to be a tree thirty feet high in some parts of Oregon. The fulvous oak ( Quercus fulvescens) is a deciduous tree, that grows about thirty feet high, with leaves somewhat like those of the Western chinquapin. The acorn, when young, is concealed in the cup, the two together resembling a little wheel ; but the acorn, when mature, is an inch and a half long, and projects considerably beyond the cup. The wood is tough- er than that of most of the oaks of California. Kellogg's oak ( Quercus kelloggii) is a large deciduous tree, found only in California. Its leaves are deeply sinuate, with three principal lobes on each side, terminating in several acute points. It bears fruit only in alternate years, or at least mos*- BOTANY. 101 abundantly every other year. An idea prevails that the acorns give to swine a disease of the kidneys. The huckleberry -leafed oak ( Quercus vacci?ii folia) is a shrub, from four to six feet high, which grows on the mountains in the northern part of the state. Its leaves, in size and form, resemble the huckleberry ; the acorn is of the size and shape of a small hazel-nut. § VY. Buckeye. — The Californian horse-chestnut, or buck- eye {^sculus californica)^ is a shrub, or low, spreading tree, abundant in the Sacramento, San Joaquin, and coast valleys. It likes to grow about rocky ledges, in ravines, and on the banks of streams. Sometimes it throws up a dozen stems, which grow to a thickness of three or four inches each; but usually it has one trunk, six or eight inches through. The tree rarely exceeds fifteen feet in height, and it has a hemi- spherical shape, very dense foliage, rising from the ground in a globular form. It continues to put forth large clusters of fragrant blossoms from early spring till late summer. The leaves are among the first to open of the deciduous trees of the state. Five leaves grow together on one stem. The fruit has a close resemblance to that of the buckeye-tree of the Mis- sissippi valley, but is larger and more abundant. It is a staple article of food with those few Californian Indians who stiU depend upon w^ild fruits and game for their subsistence. § 78. Sycamore. — The Mexican sycamore [Platanus r^ct- mosa) exhibits a striking resemblance to the Western s) ca- more of the Atlantic slope. It has the same straggling, in eg- ular growth; the same smooth, white, scaly bark; the same large, yellowish leaf: but instead of having only one ball on a stem, like the Atlantic sycamore, it has several, the stem run- ning through one or two, and terminating in the last one. § 79. Pitahaya. — The pitahaya ( Cereus giganteus)^ a gigan- tic cactus, is one of the most prominent features of the botany of the deserts in the southern part of California. It grows to a height of fifty feet, with a trunk thirty inches in diameter. Sometimes the trunk has no boughs, but usually it throw^s out 102 EESOIJRCES OF CALIFOENIA. from two to six, which are about half the thickness of the trunk ; they run out horizontally for a foot or two, and then turn upward and rise parallel with the trunk. There are no twigs or leaves, but flowers and fruit grow on the tops of the trunk and branches. The whole plant resembles a huge can- delabrum. The flowers are three inches long, as wide, with stiff, curling,' and cream-colored petals. The fruit is as large as a hen's egg^ and the meat is a red pulp, full of little seeds. The taste is insipid ; but when the fruit is dried, according to the Indian custom, it acquires a flavor somewhat like that of afig. , § 80. Yucca. — The yucca, or bayonet-tree, is a kind of palm, — an endogenous tree that lives in the southern deserts. It sometimes grows to be thirty-five feet in height, with a trunk two feet through ; but usually it is about ten feet high, with a trunk eight inches in diameter. It has no twigs or branches, but sometimes it divides into two trunks. The foliage, con- sisting of leaves eighteen inches long, and shaped like the blade of a bayonet, hangs down from the tops of the trunks. § 81. llezquit. — The mezquit {Algarohia glandidosa) is a low tree of the Colorado Desert. It sometimes reaches a height of twenty feet, with a trunk fifteen inches in diameter. The lower branches are very near the ground, and the whole tree has a very regular, semispherical form. The leaves are like those of the black locust, and the foliage thin. The tree bears numerous pods, from three to five inches long, full of sweet, nourishing beans, about the size of the common white bean. The mezquit-bean is often eaten by men, and horses and mules are very fond of it. The curly mezquit {Stromhocarpus puhescens) is a similar shrub, and bears a crooked bean, called the " screw-bean." It also grows only on the desert. § 82. Miscellaneous Trees and Shrubs. — A few walnut-trees crow alono- the Sacramciito Iliver, and it is said that some chestnuts have been found in Mendocino county, but they are unknown in the greater part of the state. We have no indi- BOTANY. 103 genous beech, elm, hickory, locust, acacia, or sassafras. Our wild cherry and wild plum are bushes, but their fruits resem- ble the wild plums and cherries of the East. We have willows and Cottonwood, which differ little in appearance from those of the Mississippi valley. There are wild grapes, blackberries, gooseberries, huckleberries, raspberries, salmon-berries, and strawberries. A truffle, or a root resembling it, is found in the valleys of the coast and the Sierra N^evada. The grizzly hear considers it a delicacy, and frequently digs it up. A shrub called the "joint-fir" (a species oi Ephedra)^ sometimes used for making tea, is found in Calaveras and Tuolumne coun- ties. In the valleys of the Coast Mountains is found the yerba huena (Spanish for "good herb"), a creeping vine, bearing some resemblance in its leaf and vine to the wild strawberry. It has a strong perfume, half-way between peppermint and camphor. The yerba de la vibora (Spanish for " rattlesnake- herb," known to botanists as the Dauciis 2:>usillus) is a carrot- like vegetable, the leaves of which are said to be a specific for the bite of the rattlesnake. § 83. Poison OaJc. — The poison oak, or poison ivy {Rhus toxicodendron)^ grows abundantly in the Sacramento Basin, and along the coast. It thrives best on a moist soil, and in the shade. In a thicket with other bushes it sends up many thin stalks eight or ten feet high, with large, luxuriant leaves at the top ; in the shade, the leaves are green. In the open, dry ground, exposed to the sun, and without support from oth- er bushes, the poison oak is a low, poverty-stricken little shrub, with a few red leaves. If it can attach itself to an oak-tree, it becomes a parasitic vine, and attains a thickness, though very rarely, of four inches in the trunk, and climbs to a height of forty feet. The touch of the leaf is poisonous, and causes a very irritating eruption of the skin. It rapidly communicates by the touch from one part of the body to another, causing severe inflammations and swellings. The most delicate parts of the body are most affected by the poison. The eyes are sometimes closed up entirely by the swelling round them j and 104 RESOUECES OF CALIFORNIA. many cases are recorded of faces so swollen, that they could not be recognized by intimate friends. Some persons are not aftected by the touch of the Rhus ; but instances have occurred wherein j^ersons supposing themselves, after long experience, to be free from danger, have at last been poisoned : and when the poison has once taken hold, the system is always very easily affected from that time forward. Even passing to the leeward of the bush on a windy day, or going through the smoke of a fire in ivhich it is burning, will bring the poison to the surface again. § 84= Amole. — The amole {Chlorogalum lyomeridicmuin)^ or soap-plant, lias an onion-like, bulbous root, which, "when rubbed in water, makes a lather like soap, and is good for removing dirt. It was extensively used for washing, by the Indians and Spanish Cahfornians, previous to the American conquest. The amole has a stalk four or five feet high, from which branches about eighteen inches long spring out. The branches are cov- ered with buds, which open in the night, beginning at the root of the boughs, about four inches of a branch opening at a time. The next night, the buds of another four inches open, and so on. § 85. Nutritious Herbage. — Of indigenous nutritious grasses there are a number in the state. The wild oat, though not a grass, may be mentioned under this head. It resembles the cul- tivated oat so nearly, that there has been some doubt wiiether they are not identical, but the opinion among botanists is that they are distinct species. The wnld oat, in the year 1835, was found only south of the bay of San Francisco ; but about that time, when the Tvhite men crossed frequently from the southern to the northern side of the bay, the oat was sowm in a natural way by horses and cattle, and it spread rapidly over the Sacramento valley and the coast region. It grew very luxuriantly, and in some places surpassed in the height, size, and abundance of stalks, any field of cultivated oats which I have ever seen. It is said that in some localities the oat-stalks were so high, that men sitting erect on horseback could not BOTANY. 105 see each other at a distance of ten feet. The soil and climate were evidently very favorable to it. During the last six or eight years, the wild oats have been eaten down so closely by cattle, that in many places they have been killed out. They are propagated from year to year, not by the roots, but by the seeds, many of which fall into cracks in the earth, where they lie in safety until the rains come, when the ground closes up and the grain sprouts. The earth cracks in the summer, in many parts of the state ; and in places where the wild oats grow, the position of the cracks of one year may be traced the next season by the position of the stalks of the grain. The wild oat grows on hill and plain, and furnishes a large part of the wild pasture of the state. It is wholesome, nutri- tious, and palatable for cattle. Much of it is cut for hay. The amount of grain which it furnishes is small in proportion to the quantity of straw, and it is never threshed. After the wild oats, in importance to the herdsman, comes the "burr-clover," so named from a spherical burr, about a quarter of an inch in diameter, which it bears in clusters of three. This burr-clover is found in all the settled parts of the state. Cattle do not like it when green ; but after it dries, the burrs fall upon the ground, and are picked up by the cat- tle, while the stranger is astonished at seeing them eating and keeping fat on what appears to him to be bare earth. On ex- amining the surface of the ground, he will find that it is cov- ered with the dry stalks and burrs of the burr-clover. The bloom consists of three very small yellow flowers. It is said that the stalks of this clover take root whenever the joints touch the ground. The alfilerilla [Er odium cicutarium) is another indigenous nutritious herb of much importance to the herdsman. It is succulent, sweet, hardy, bearing clusters of spikes or pins an inch and a half long. These spikes have given it the name of pin-grass ; and the resemblance of its leaves to the geranium has suggested the name of " wild geranium," by which title it is also known to some persons. It has a large root, which it 5* 106 RESOUECES OP CALIFORNIA. sends deep into the ground, thus enabling it to resist the drought, while above the surface it puts forth a dense mass of stalks and leaves, spreading out sometimes several feet in every direction. Cattle prefer it to every other indigenous herb of the state. The seeds seem to abound throughout the soil, for wherever the earth is ploughed up for the first time, there the alfilerilla appears, though it may never have been seen there before. It is common in gardens, cultivated fields, and fallow lands. The white Californian clover has a large yell o wish- w^hite bloom, from an inch to an inch and a half in diameter, a beau- tiful plant, well suited as an ornament for yards and gardens. It grows very large, and two feet high in moist, favorable sit- uations ; while in dry places it w^ill also mature its seed with- out rising more than two or three inches above the ground. It is very sweet, and it is often eaten by the Indians, w^io like it both raw and boiled. Cattle are also extremely fond of it. Another species of clover has a round bloom about a third of an inch in diameter, composed of violet-tinged flowers. Another clover has a bloom from a sixth to a quarter of an inch in diameter, the flowers of which are subdued green, tipp'^d with pink at the end. The Melilotes officinalis^ another herb, commonly called a closer, though not strictly entitled to that name, likes a very moist soil, and then grows luxuriantly, crowding out nearly every thing else. Its bloom consists of a drooping head about an inch long and a sixth of an inch thick, hung with little yel- low flowers. Cattle are not fond of this herlJ in any shape, but they like it better in hay than when green. Of nutritious grasses there are a number, but they do not form a sod. The drought of summer and fall seems to kill the roots. Of wild flowers there are a great variety and abundance in California, and they have their difierent seasons for blooming ; and in caiions where the soil is always moist, flowers may be seen in every month of the year. In the spring-time the hill- BOTANY. 107 sides are frequently covered with them, and their red, blue, or yellow petals hide every thing else. Each month has its flow- ers : in March the grass of a valley may be hidden under red, in April under blue, and in May under yellow blossoms. There is such a variety that within an hour I have counted twenty species on a spot not more than twenty feet square. This was on dry, sandy soil, in Sonoma valley, in the month of May. None of the flowers are large, brilliant in color, or rich in sweet, strong perfume. The tule is a reed which covers all the large tracts of swamp lands in the state. It has no leaf, but a plain, round stalk, va- rying from half an inch to an inch and a half at the butt, and tapering gradually to a point. It is usually not more than eight or ten feet high, but at the Tulare Lake it grows to fifteen or twenty feet. The grass and herbage begin to grow and clothe the land- scape in green after the first heavy rains of the rainy season. These rains may come in December, January, or February; and until they do come, the earth, in the districts not covered, with timber, is brown. The grass continues green until June, when it begins to dry up and turn yellow and brown, which colors then predominate in the landscape until the rains come again. The death of the grass, except at high elevations, is caused not by the cold but by the drought ; and in those months when the prairies of Indiana and Illinois are covered with snow, the valleys of California are dressed in the brilHant green of young grass. The mistletoe grows abundantly on the oak-trees of Califor- nia. The Spanish moss, which hangs in long lace-like gray beards from the branches, also serves to give beauty to the groves in the valleys. Note. — Most of mj information about the botany of the state has been derived from the reports of Dr. J. S. Newberry, in the United States Pacific Railroad Survey, and from the conversation of Dr. A,. Kellogg, Dr. IL Behr, and Mr. H. G. Bloomer, of San Francisco. 108 KESOUECES OF CALIFORNIA, CHAPTER YL ZOOLOGY. § 86. General List. — Among the indigenous animals of Oal- ifoTnia are the grizzly bear; the black bear; the panther, the wild-cat; the gray wolf; the coyote; three foxes; the badger; the raccoon ; the opossum ; the mountain-cat ; the weasel ; two skunks ; one porcupine ; three squirrels ; two spermophiles ; two ground-squirrels ; three rats ; three jumping-rats ; one jumping-mouse ; nine mice ; one mole ; the elk ; one deer ; one antelope ; the mountain-sheep ; three hares ; two rabbits ; the seal ; the sea-otter ; the sea-lion ; the beaver ; two vul- tures ; the golden eagle ; the bald eagle ; the fishhawk ; eighteen other hawks ; nine owls ; the road-runner ; twelve woodpeckers ; four humming-birds ; eleven flycatchers ; one hundred and nine singers ; one pigeon ; two doves ; three grouse ; three quails ; one sandhill crane ; forty-one waders ; sixty-six swimmers, including two swans and five geese ; about two dozen snakes, including the rattlesnake ; half a dozen sal- mon ; two codfish ; and one mackerel. §87. ^ears. — The grizzly bear [Ursus horrihilis) is the largest and most formidable of the quadrupeds of California. He grows to be four feet high and seven feet long, with a Aveight, when very large and fat, of two thousand pounds, be- ing the largest of the carnivorous animals, and much heavier than the lion or tiger ever get to be. The grizzly bear, how- over, as ordinarily seen, does not exceed eight hundred oi nine hundred pounds in weight. In color the body is a light grayish-brown, dark brown about the ears and along the ridge of the back, and nearly black on the legs. The hair is long, ZOOLOGY. 109 coarse, and wiry, and stiff on the top of the nect and between the shoidders. The "grizzly," as he is usually called, is more common in California than any other kind of bear, and was at one time exceedingly numerous for so large an animal ; but he offered so much meat for the hunters, and did so much damage to the farmers, that he has been industriously hunted, and his numbers have been greatly reduced. He ranges throughout the state, but prefers to make his home in the chaparral or bushes, whereas the black bear likes the heavy timber. The grizzly is very tenacious of life, and he is sel- dom immediately killed by a single bullet. His thick, wiry hair, tough skin, heavy coats of fat when in good condition, and large bones, go far to protect his vital organs ; but he often seems to preserve all his strength and activity for an hour or more after having been shot through the lungs and liver with large rifle-balls. He is one of the most dangerous animals to attack. There is much probability that when shot he will not be killed outright. When merely wounded he is ferocious ; his weight and strength are so great that he bears down all opposition before him; and he is very quick, his speed in running being nearly equal to that of the horse. In attacking a man, he usually rises on his hind-legs, strikes his enemy with one of his powerful fore-paws, and then commences to bite him. If the man lies still, with his' flice down, the bear will usually content himself with biting him for a while about the aims and legs, and will then go off a few steps and watch him. If the man lies still, the bear will beheve him dead, and will soon get tired and go away. But let the man move, and the bear is upon him again ; let him fight, and he will be in im- minent danger of being torn to pieces. About half a dozen men, on an average, are killed yearly in California by grizzly bears, and as many more are cruelly mutilated. Fortunately, the grizzly bear is not disposed to attack man, and never makes the first assault unless driven by hunger or maternal anxiety. The dam will attack any man who comes near her cubs, and on this account it is dangerous to go in the 110 KESOUKCES OF CALIFORNIA. early summer afoot through chaparral where bears make their home. Usually a grizzly will get out of the way when he sees or hears a man, and sometimes, but rarely, will run when wounded. It is said that grizzlies in seasons of scarcity, used to break into the huts of the Indians and eat them. No in- stance of this kind, however, has been reported for some years past. The greater portion of the food of the grizzly is vegetable, such as grass, clover, berries, acorns, and roots. The manza- nita, service, salmon, and whortleberries, are all favorites with him. The roots which he eats are of many different species, and it was from him that we learned the existence of a Cali- fornian truffle, very similar to the European tuber of the same name. The grizzly is very fond of fresh pork, at least after he knows its taste, and if swine come within his reach, he soon learns the taste. The farmers in those districts where the bears are abundant, shut up their hogs every night in corrois or pens, surrounded by very strong and high fences, which the bears frequently tear down. After having killed a hog, if any part of the carcass is left, the grizzly will return the next night and feast upon the remains, and go until it becomes putrid. He prefers, however, the fresh pork if it can be had. Not un- frequently the grizzly discovers the carcasses of deer, elk, and antelope, killed by hunters, who have gone off for horses to carry their game home. In such case, the hunter usually finds little left for him when he gets back. They do not like climb- ing, and rarely attempt to ascend trees. The grizzly, though he often moves about and feeds in the day, prefers the night, and almost invariably selects it as the time for approaching nouses, as he often does, in search of food. The cub is one of the most playful, good-humored, and amusing of animals. He will tumble somersets, sit up on his haunches and box, and in some of his pranks will show a humor ai\d intelligence scarcely inferior to that of very young children. The grizzly may easily be tamed, and it becomes very fond of its master. Adams, the Californian mountaineer and bear-hunter, trained several griz- ZOOLOGY. Ill ?:lies so that they accompanied him in his hunting excursions, defended him against wild animals, and carried burdens for him. The meat of the young grizzly resembles pork in tex- ture and taste, exceeding it in juiciness and greasiness ; but the meat of the old he-bear is extremely strong, and to delicate stomachs it is nauseating. The black bear ( Ursus cmiericanus) is found in the timbered portions of California, but is not abundant. It is more often seen near the coast north of Bodega than in any other portion of the state. Dr. IS[ewberry, speaking of the food of the black bear on this coast, says : " The subsistence of the black bears in the northern portion of California is evidently, for the most part, vegetable. The manzanita, wild plum, and wild cherry, which fruit profusely, and are very low, assist in making up his bill of fixre. Karely, too, we saw trees of yellow-pine bear- ing marks of bears' teeth, where they had torn off the outer bark to get at the succulent inner layer, which is capable of sustaining life, and to which the Indians very generally have recourse when pressed with hunger." It is believed that nei- ther the grizzly nor the black bear hybernates in California. § 88. Panther and Wild- Cat. — The panther of California, supposed by Dr. Newberry to be the Felis concolor — the same with the panther found on the Atlantic slope of the continent — has a body larger than that of the common sheep, and a tail more than half the length of the body. Its color is dirty- white on the belly, and elsewhere a brownish-yellow, mottled with dark tips on all the hairs. The panther is a cowardly animal, and, except when driven by some extraordinary motive, never attacks man. A friend of mine, who was out hunting, dressed in a buff coat, was creeping through some brush to get near a deer, when he felt a heavy animal strike his back. He sprang up very suddenly, and saw a panther, which had jumped down upon him from a tree, probably mistaking him for a calf or a deer. The brute seemed very much astonished and frightened at seeing a man there, and immediately fled at full speed. The panther is nocturnal in his habits, and always j^refers the night 112 KESOUECES OF CALIFORNIA. as a time for attacking colts, which are a favorite prey with him. He is found in all parts of the state where there is tim- ber, but he never stojDS long in any place, unless he can find bushes to hide in. The American wild- cat [Lynx rufus) is common in Califor- nia, particularly in the vicinity of the bays of San Francisco and San Pablo, where he often catches fish and water-fowl as well as land-animals. His color is a light brown, with dim, dark spots on the sides, and longitudinal lines along the middle of the back. § 89. Wolves and Foxes. — The gray wolf ( Ccinis occidenta- lism is found in all the inhabited j)arts of California, but is not abundant. The coyote is very common in the state, and occupies the same place here with that occupied in the Mississippi valley by the prairie-wolf. Dr. Newberry thinks the two belong to l^he same species ( Ganis latrans), but I am inclined to believe that they are specifically different. The color of the coyote has more of a reddish tinge, he howls more, does not bark so much, and is more cunning. His food consists chiefly of rab- bits, grouse, small birds, mice, lizards, and frogs ; and in time of scarcity he will eat carrion, grasshoppers, and bugs. He is very fond of poultry, pigs, and lambs, and will destroy almost as many of them as would a fox. He is one of the worst ene- mies and most troublesome pests of the farmer. His method of catching chickens is to hide near the hen-roost about day- light, and, as the hens come down, he pounces upon them from his hiding-place ; and his motions are often so quick, that the victim has not even time to squall before she dies. In the spring and autumn, when wild geese and ducks are abundant, many coyotes make their homes in the tules, where they catch the birds which have been wounded by the hunters. The coyote loves nothing better than a young pig. When he sees an old sow with her young ones, he will hide, and wait a long time, in hopes that a little one will come within his reach ; but if there be no hiding-place, he goes up boldly. The ZOOLOGY. 113 SOW will at once face the assailant, and start to attack him. He allows her to come up within a few feet of him, and then moves off slowly ; and she, like a fool, thinking she Avill catch him, continues the chase. While running, he keeps his head turned to one side, partly to watch her, and partly to watch the pigs ; and when he has seduced her far enough away, he suddenly makes a dash at the pigs, and, getting one of them, runs off with it, leaving the agonized and furious sow far. be- hind. If the coyote does not succeed in getting a pig at the first attempt — that is, if he does not lead the sow far enough away — he tries it again and again, till he succeeds, the sow being so stupid as to follow him, after having repeated oppor- tunities to see his purpose. The coyotes frequently go in packs, and sometimes will un- dertake to attack a cow. On such occasions, they have a con- certed plan of operations : they surround their intended victim, and v>^hile those in front rush at her as a feint, those behind attempt to cut her hamstrings. As their teeth are very sharp, they often succeed. The cow's hamstrings once cut, she falls, and is completely at their mercy ; and they quickly pick her bones. The coyote is a great thief, and will steal the pillow from under a sleeping man's head ; for it happens in California that bags of provisions are often used as pillows. Wlien the coyote is hungry, he will gnaw any thing that is greasy, and for that reason he frequently cuts off the hemp and raw-hide ropes with which horses are tied out at night ; but he never bites into hair-ropes, which for that reason were formerly used ex- clusively for staking out horses. The coyote is nocturnal in his habits, and is very fond ^ howling or yelping. He begins with a shrill, quick bark, ana follows up with a succession of yelps, ending in a long-drawn, quavering, melancholy howl. When one begins, all others within hearing take up the cry. Ten years ago, the traveller in the Sacramento valley rarely passed a night without hearing their music. They are not so nimierous now, but still they 114 RESOURCES OF CALIFORNIA. are frequently seen in the most densely-settled parts of tlie country. Tho red fox ( Vulpes fulviis macrourus) is found north of latitude 37° ; the gray fox ( Vulpes virginianus) in all the tim- bered parts of the state. The coast fox ( Vulpes littoralls) is found only on the island of San Miguel, off the coast of Santa Barbara. In its color it bears a great resemblance to the gray fox, but it is not more than half as large, is less cunning, and is slower in its motions. Its tail is only one-third the length of its body. The specimens observed were very bold and stupid, allowing themselves to be caught, over and over again, in the same manner. The desert fox ( Vulpes macrourus), which is found in the central deserts of the continent, crosses the Sierra Nevada, and is often killed in Calaveras and Tuolumne counties. § 90. Badger, etc. — The American badger (Taxidea ameri- cand) is abundant in the plateau of the Sierra Nevada, and is occasionally found in other parts of the state. It is very shy, and is rarely seen by the traveller. The black-footed raccoon [Procyon hernandezii) is found in the timbered portions of the Pacific slope of our continent from Santa Barbara to British Columbia. It is longer than the At- lantic raccoon [Procyo7i lotor), but resembles it very closely in its mental character and capacity, habits and appearance. The raccoon is fond of grapes, and when he enters a vineyard selects those of the finest flavor. An opossum {Didelphys californica) is found hi the wooded portions of the state, but is not abundant. The yellow-haired porcupine [Erethizon epixantlms), a na- tive of California, is the largest of its genus. The spmes are a couple of inches long, yellowish in color, with brown tips. On the lower part of the sides the spines are replaced by long, stiff bristles. The mountain-cat, or striped bassaris {Bassaris astuta), is abundant along the western base of the Sierra Nevada, be- tween latitudes 36° and 39°. The body is about the size of ZOOLOGY. 115 that of the domestic cat, but the nose is very long and sharp, and the tail very long and large. The color of the animal is dark gray, with rings of black on the tail. The miners cull it the " mountain-cat," and frequently tame it. It is a favorite pet with them, becomes very playful and familiar, and is far more afi'ectionate than the common cat, which it might replace, for it is very good at catching mice. The pine-marten (Mustela americana) is found in California, but is rare. The yellow-cheeked weasel {Putorius xanthogenys) is found along the coast, in the vicinity of the bay of San Francisco. The common mink [Putorius vison) has a skin as valuable as that of the beaver ; the fur is of a dark, brownish, chestnut color, with a white spot on the end of the chin. California has two skunks (JiepA^Y^« occidentalis and Me- phitis bicolor), very common animals. The Mephitis hicolor^ or little striped skunk, is chiefly found south of latitude 39° ; the other in the northern and central parts of the state. The colors of both are black and white. § 91. Tlie Squirrel Pltmily. — The Californian gray squirrel (Sciurus jossoi'), the most beautiful and one of the largest ot the squirrel genus, inhabits all the pine-forests of the state. Its color on the back is a finely-grizzled bluish gray, and white beneath. At the base of the ear is a little woolly tuft, of a chestnut color. The sides of the feet are covered with hair in the winter, but are bare in the summer ; the body is more slender and delicate in shape than that of the Atlantic gray squirrel. It sometimes grows to be twelve inches long in the head and body, and fifteen inches long in the tail, making the entire length twenty-seven inches. Dr. Newberry says: ''The Cali- fornian gray squirrel is eminently a tree-squirrel, scarcely de- scending to the ground but for food and water, and it subsists ahnost exclusively on the seeds of the largest and loftiest pine known [Pinus kmibertiana), the ' sugar-pine' of the Westeiii coast. The cones of this magnificent tree are from twelve to sixteen inches in length, and contain each one hundred or more 116 KESOURCES OF CALIFORNIA. seeds of the size and shape of the small white bean of com- merce. These cones would be unmanageable by the squirrel in the tree, and he has the habit, so common in the family, of dropping them to the ground, where he can dissect them at leisure. This he usually does early in the morning, climbing to the extremities of the topmost branches, where the cones hang, and cuttiug off a sufficient number to supply his wants for the day. He then descends, and, commencing at the base of the cone, tears off the scales in rapid succession, and skil- fully possesses himself of the seeds which they conceal. He is compelled, however, to supply other wants than his own, for the smaller pine-squirrel {Sciurus douglasii) and the ground- squirrel [Tamias townsendii) appropriate a large share of his booty. When oak-trees are near, and acorns are ripe, he has recourse to them for subsistence ; as often as opportunity offers, robbing the woodpeckers of their stores, in which also he has the active co-operation of his more diminutive congeners. From the fact that he feeds upon the ground, it has been sup- posed that he was less active and less fitted for climbing than most tree-squirrels. This, I think, is not true. He is exceed- ingly quick and graceful in his movements ; and if less fre- quently seen to spring from tree to tree than the black and gray squirrels of the eastern states, it is because he inhabits coniferous trees, which are remarkable for the insignificance of their branches compared with the size of the trunk, the limbs never stretching out and interlocking, as those of the oak and maple and other trees, in which our common species live." The Californian pine-squirrel [Sciurus douglasii) inhabits the pine and redwood forests of the state. He is gray above and red beneath, with a black stripe separating the two colors. He lives in a burrow or hollow log, but climbs well, and ob- tains his food chiefly from the pine-cones, which he cuts off in numbers at a time, and tears to pieces at his leisure, after they have fallen to the ground. He lays up a store of the seed in his burrow, for his winter supply. He is quick in his motions, graceful in his attitudes, and shy in his habits. ZOOLOGY. 117 The Missouri striped ground-squirrel has five dark-brown stripes on the back, separated by four gray stripes ; the sides are rec^dish-brown, the belly grayish-white, and the tail rusty- black above and rusty-brown beneath. The animal is four or five inches long. It is found in the northern parts of the state. It eats acorns and the seeds of the pine, manzanita, and ceano- thus, in the thickets of which last-named bush it prefers to hide its stores. The Spermophile has two species in California, which resem- ble each other so closely, that they are usually supposed to bo the same ; they are popularly known as the Californian ground- squirrels, the little pests which are so destructive to the grain- crops. Their bodies are ten or eleven inches long in the largest specimens ; the tail is eight inches long, and bushy ; the ears large ; the cheeks pouched, and herein consists the chief difier- ence between them and squirrels ; the color above black, yel- lowish-brown, and brown, in indistinct mottlings, hoary-yel- lowish on the sides of the head and neck, and pale yellowish- brown on the under side of the body and legs. They dwell in burrows, and usually live in communities in the open, fertile valleys, preferring to make tlieir buri'ows under the shade of an oak-ti'ee. Sometimes, however, single spermophiles will be found living in a solitary manner, remote from tlieir fellows. Their burrows, like those of the prairie-dog, are often used by the rattlesnake and the little owl. Dr. Newberry says : " They are very timid, starting at every noise, and on every intrusion into their privacy dropping from the trees, or hurrying in from their wanderings, and scudding to their holes with all possible celerity ; arriving at the entrance, however, they stop to recon- noitre, standing erect, as squirrels rarely and spermophiles habitually do, and lookmg about to satisfy themselves of the nature and designs of the intruder. Should this second view justify their flight, or a motion or step forward still further alarm them, with a peculiar movement, like that of a diving duck, they plunge into their burrows, not to venture out till all cause of fear is past. Should you in the mean time have 118 EESOUECES OF CALIFORNIA. seated yourself with your back against a tree, and have re- mained for a time as immovable as the trunk against which you lean, you will soon see sundry little heads protruding from the burrows, with as many pairs of eyes and ears skilled to detect the least sign of danger from then* equally-feared ene- mies, the coyote, the Calil'ornian vulture, the red-shouldered and red-tailed hawk, and man himself If, however, your si- lence and quietness persuade them that you are none of these, they will swarm forth from their holes, and at first timidly, but, gaining confidence, more fearlessly, engage in all the sports and antics for which the sciuridce are noted, and in which none excel the species under consideration. It is a l^retty sight, and one to which I have often treated myself, to sit down quietly under these old oaks, and watch the squirrels running about over the grass and trees, gambolling and play- ing together. As far as the eye could reach through the vista» the sprightly movements of these innocent animals could be discerned." The two species are called Beechey's spermophile (S2^ermO' philus heecheyi) and Douglas's spermophile {Spermo2yhilus douglasii). The size, habits, and general appearance of the two species are the same, but they differ in the color of a stripe along the spine from the base of the head to the middle of the back: in Beechey's spermophile it is yellowish-hoary, in Doug- las's it is dark-brown. The former species is found very abun- dantly south of the straits of Carquinez; the latter north of it, and fewer in number. Beechey's spermophiles are among the most formidable ene- mies of the farmer in those districts where they make their homes. They increase very rapidly in the vicinity of farms, and do great damage in grain-fields and gardens ; they eat grain and garden vegetables in all stages of their growth; they peel young fruit-trees and vines ; they are, in short, dan- gerous to nearly every thing that is cultivated. They are very industrious, and lay up large stores for the winter, spending several hours every pleasant summer's day in gathering food. ZOOLOGY. 119 They go considerable distances to fields; and the traveller, whose a]>proach scares them, sees them in hundreds rmming across tlie road before him, with their tails erect, hurrying from the field to hide themselves in their burrows. Many a large wheat-held, which would have yielded forty bushels to the acre if there had been no spermophiles to trouble it, is so despoiled by them, that the crop will not pay for harvesting. They are particularly abundant in the Santa Clara, Amador, and Pajaro valleys ; and their number is an important consid- eration in the estimate of the price of land. They will not live in moist land, nor very near the ocean, where the fogs prevail. They are poisoned with strychnine and phosphorus, drowned by irrigation, and shut out by tight board-fences. In wet winters many of them are drowned ; after a dry winter they are'' always numerous. Away from cultivated fields they depend for food chiefly upon grass-seeds, grass-roots, and acorns. The Californian gopher {Thomomys hulhivorus) is, next to Beechey's spermophile, the most abundant and most trouble- some rodent of the state. \^hen full grown, it has a body six or eight inches long, Avith a tail of two inches. The back and sides are of a chestnut-brown color, paler on the under parts of the body and legs ; the tail and feet are grayish-white ; the ears are very short. In the cheeks are large pouches, covered with fur inside, white to their margin, which is dark-brown. The gopher inhabits the fertile valleys of the coast from lati- tude 34° to 39°. He spends nearly all his time under ground, and does most of his mischief there, gnawing off" the roots of fruit-trees and garden vegetables, eating newly-sown grain and seeds, and nibbling at flowers and sweet bulbs. He is not a climber, nor is he very agile : if he gets into a trench eight inches wide and a foot deep, with perpendicular sides, he will run a long distance in it rather than clamber out; and one of the best methods of catching him is to make such a trench round a field, and pjace square tin boxes, fifteen inches dtep, eight inches square, and open at the top, in the bottom of the 120 PwESOUKCES OF CALIFORNIA. trench, at regular intervals of about fifty yards. The gopher frequently travels at night, and when he conies to this trench he falls in. He then runs along in it, looking for a convenient place to get out, and, coming to a tin box, lalls into that. He can neither jump out nor gnaw through ; so he remains a pris- oner till he starves to death, or the farmer comes along and kills him. The Colorado gopher [Thomomys fulmis) is found in that portion of the state south of latitude 34°, but is not abundant. It is smaller than the Californian gopher, and has more of a reddish tinge in its colors. Its habits and appearance other- wise are very similar to those of its northern congener. The broad-headed gopher [Thomomys laticeps)^ found in the vicinity of Humboldt Bay, is about five inches long. Its color on the back, sides, and belly, is yellowish-brown, with a reddish tinge between the fore legs. § 92. The Rat Family. — California has a number of indi- genous jumping-rats, jumping-mice, and other rats and mice, too many and not sufiiciently singular, or interesting to the general reader, to deserve a complete description here. I shall content myself, therefore, with giving a simple list of them, with the districts they inhabit, their entire length from the point of the nose to the end of the tail, and the main color of the back : Philip's jerboa, or jumping-rat [Dipodomys philipi) ; Sac- ramento Basin and the southern valleys ; twelve inches ; yel- lowish-brown. The dun jumping-rat {Dipodomys ay His) ; coast valleys south of Saa Francisco ; twelve inches ; lead-color. The Colorado j umping-rat [Perognathus 2)erdcillatus) ; Col- orado Desert ; nine inches ; tawny. The King's River jumping-rat [Peroynathus pa7^vus) ; King's River valley ; four inches. Hudson's jumping-mouse {Jacidiis Jiudsonii) ; valley of Ca- noe Creek; eight inches; yellowish-brown. Black rat {Mas rattus) ; coast from Humboldt Bay to San ZOOLOGY. 121 Diego ; fourteen inches. There is much doubt whether it is indigenous. The long-tailed mouse [Reithrodon longiccmda) ; coast near S.ui Francisco ; five inches ; dark-bi-own. Gambel's mouse i^He^peromys gamhelli) ; from Tomales B y to Kern River; five inches; glossy-brown. Boyle's mouse {Hesperomys hoylii) ; valley of the American River; eight inches ; glossy-brown. Californian mouse {Hesperomys caUfornicus) ; Santa Clara valley ; six inches ; sooty-brown. Desert-mouse {^Hesperomys eremieus) ; Colorado Desert ; five inches ; grayish-yellow. The bush rat {JS^eotoina mexicana) ; near San Diego and in the Colorado desert ; thirteen inches ; yellowish brown. The JSfeotoma fuscip)es^ a rat ; coast valleys, from 38° to 40° ; fifteen inches ; reddish above. The Arvicola montana^ a mouse ; near Petaluma, Monte- rey, and Lost River ; six inches ; yellowish brown. The long-fiiced mouse (Arvicola lougirostris) ; Pit River valley ; six inches ; yellowish brown. The Californian ground-mouse {Arvicola edax) ; coast val- leys south of San Francisco; six inches; yellowish brown. The Arvicola californica^ a mouse much like the species last named. The Oregon mouse {Arvicola oregowi) ; near Tanales Bay; four inches ; yellowish brown. The Oregon mole {Sccdops tounsendii) is found near the bay of San Francisco, and perhaps in other parts of the state. It is six or seven inches long, nearly black in color, with faint- purplish or sooty-black reflections in the hair. § 93. The Deer Family. — The American elk {Cervus cana- densis) is found in California as well as in many other parts of the continent. The animal is nearly as large as a horse, and has some resemblance to it in general shape, though smaller, and slimmer in the head, neck, and legs. Its length Irom the nose to the tail is seven feet ; its height five feet; its 6 122 EESOUKCES OF CALIFORNIA. greatest weight one thousand pounds. The color is a chest- nut brown, dark on the head, neck, and legs, lighter and yel- lowish on the back and sides. The horns are very large, some- times more than four feet long, three feet across from tip to tip, measuring three inches in diameter above the burr, and weighing, with the skull, exclusive of the lower jaw, forty pounds. The horns of the old bucks have from seven to nine, perhaps more, prongs, all growing forward, the main stem running upward and backward. The elk were very abundant in California previous to 1849, and they were frequently seen in, large herds ; but within the last ten years they have become rare, and before the close of another decade they will be ex- tinct in our state. A few are found in the San Joaquin valley, but the best place for hunting them is in Mendocino county. Several hundred carcasses find their way every year to the San Francisco market. The young fat elk furnishes a very juicy and sweet venison. The white-tailed Virginian deer, once common in the states east of the Mississippi, is not found in California, but in its place we have the black-tailed deer {Cei'vus columhianus)^ which is a little larger and has brighter colors, but does not furnish as good venison, the meat lacking the juiciness and savory taste of the venison in the Mississippi valley. The av- erage weight of the buck is about one hundred and twenty- pounds, and of the doe one hundred pounds, but bucks have been found to weigh two hundred and seventy-five pounds. The summer-coat of the black-tailed deer is composed of rather long and coarse hair, of a tawny brown, approaching chestnut on the back. In September this hair begins to come ofi", expo- sing what the hunters call the " blue coat," which is at first fine and silky, and of a bluish-gray color, afterward becoming chestnut brown, inclining to gray on the sides, and to black along the back. Occasionally deer purely white are found. The horn, when long, is about two feet long, and forks near mid-length, and each prong forks again, making four points, to which a little spur, issuing from near the base of the horn, may ZOOLOGY. 123 be added, making five in all. This is the general form of the horn ; sometimes, however, old Lucks are found with but two points. The deer likes the hills and the timber ; the prong- horned antelope {Antilocapra anierlcana) loves the valley and the open land. Before the Americans took California, the Sac- ramento and San Joaquin valleys abounded with herds of an- telope ; but now they are rare in the northern part of the state*, and not abundant in the southern part. The traveller in the Tulare valley and in the Great Basin near the Coast Moun- tains, sees herds of them every day. Thousands are killed yearly for the market. In size the antelope is not quite so large as the Californian deer, which it resembles closely in form and general appearance. They are distinguished at a distance by their motion : the antelope canters, while the deer runs ; the antelope go in herds, and move in a line following the lead of an old buck, like sheep, to which they are related, while deer more frequently are alone, and if in a herd they are more inde- pendent, and move each in the way that suits him best. In color, the back, upper part of the sides and outside of the thighs and forelegs are yellowish brown ; the under parts, lower part of the sides, and the buttocks as seen from behind, are white. The hair is very coarse, thick, spongy, tubular, slightly crimped, or waved, and like short lengths of coarse threads cut off bluntly. The horns are very irregular in size and form, but usually they are about eight inches long, rise almost perpen- dicularl}^, have a short, blunt prong in front, several inches from the base, and make a short backward crook at the top. The female has horns as well as the male. The hoof is heart- shaped, and its print upon the ground may be readily distin- from the long, narrow track of the deer. The antelope is about two feet and a half high, and four feet long from the nose to the end of the tail. The mountain sheep ( Ovis montana) is found on the Sierra Nevada, from the Tejon Pass to the Oregon line, but it is a rare and very shy animal, and is seldom killed. Its length is about five feet, and its Tveijrht sometimes three hundred and 124 RESOURCES OF CALIFORNIA. fifty pounds, considerably greater than that of the deer or do- mesticated sheep. The color is white beneath, grayish brown elsewhere. The horns of the ram are very large, sometimes five inches through at the base and three feet long. The horns, after starting upward, turn backward, then downward, and so round with a circular or spiral shape, the tip inclining outward. Mountaineers assert that these horns are used by the sheep in getting down from the high cliffs which he is fond of frequenting. Instead of clambering down toilsomely over the rugged and broken rocks, he makes an easy job of it by leaping headlong, confidently down, over precipices fifty, yes, one hundred feet high, and alights head first on his horns, which are strong enough to be unbroken by the shock, and elastic enough to throw him ten or fifteen feet into the air — and the next time he alights on his feet all right. § 94. The Hare Family. — The Californian hare, or "jackass rabbit," as it is commonly called [Lepus callfornicus)^ is one of the largest of its class, growing sometimes to be two feet long from the nose to the end of the tail. Its ears are very large, and have suggested the vulgar name. It was once abundant in all the valleys from the Klamath to the Colorado ; it is more rare now. The color beneath is a pale cinnamon ; above it is mixed black and light cinnamon, the longest hairs being of a light smoky-ash color for about half the length, then dark sooty-brown, then pale cinnamon-red, and finally black at the tip. The prairie hare {Lepus campestris) also, one of the largest hares, inhabits the plateau of the Sierra Nevada, Pit River valley, and the country about the Klamath lakes. It is all w^hite in winter ; in summer yellowish gray, with brownish tinges above and white beneath. The length, from the tip of the nose to the root of the tail, is from seventeen to twenty- three inches ; and the tail and ear each measure about four inches. Audubon's hare [Lepus audabonil) inhabits the coast val- leys from Petaluma to San Diego. It is fifteen inches long, ZOOLOGY. 126 with a tail measuring to the end of the hairs on it three inches. The color is mixed yellowish-brown and black above, white beneath, thighs and rump grayish. Trowbridge's hare {Lepus trowhridgii) is found along the coast southward from 39°. The length is from eleven to fifteen inches ; the tail, with hair and all, less than an inch. The back is yellowish brown mixed with dark brown, paler on the sides, and ash-colored beneath. The sage rabbit {Lepus artemisia) is found in all the open parts of California north of the Straits of Carquinez. It is from eleven to sixteen inches in length ; in color, brown above and white beneath, with a yellowish tinge, the under part of the neck a yellowish brown. The fur on ah parts of the body is lead-colored at the base. § 95. Aquatic Mammals. — The American beavers {Castor canadensis) were once very abundant in all the large streams of California, and it was chiefly for their sake that the first Ameri- can trappers entered the country some thirty-five or forty years ago. They are still found in nearly all parts of the state, and even numerous, it may be said, in some of the sloughs near the junction of the Sacramento and San Joaquin Rivers. They rarely build dams in California, but live in burrows in the banks. When they dive they slap the water with their tails, making a noise that can be heard at a considerable distance in a still night. Their skins, which once commanded very high prices, have lost much of their value since the adoption of silk for making hats. The common mink {Putorlus vison) is found in California, but is not abundant. The general color of the animal is dark brownish-chestnut, with a white spot on the end of the chin. The skin of the minl^^is as valuable as that of the beaver. The Californian otter {Lutra callfornica) is found all along this coast, and was formerly abundant on all the large streams. It is carnivorous, living entirely on fish and shell-fish. It pre- fers large streams and lakes for its home, while the plant-eating beaver prefers small streams. The Californian otter is some- 126 EESOUECES OF CALIFOENIA. times five feet long from the point of the nose to the tip of the tail. When in the water, its hair is at times beautifuUy iridescent. The sea-otter (EnJiydra marinci) is larger than the Califor nian otter, and is also carnivorous. It generally makes its home near islands, and roams about in the water within ten or twenty miles of land. The sea-otter was at one time nq,xy abundant along the coast of California, and it was one of the attractions which induced the Russian Fur Company to estab- lish a post at Fort Ross, in latitude 38° 30', Avhere a number of Aleutian Indians were employed from 1812 to 1840 in the otter fishery. They would start out in their little single ca- noes, made water-proof with a covering of fish-bladders, so that there was no danger of their sinking if the sea should sweep over them, and thus they would go out fifty miles to sea and travel up and down the coast, usually coming Iiome well laden with sea-otter skins worth sixty or eighty dollars each. The sea-otter is still abundant on the southern coast, and there are men in Santa Barbara county who make it a business to hunt them. " The otter," says Mr. W. A. Wallace, " is very harmless, and always seeks to escape from human observation. When attacked they make no resistance, but endeavor to escape by sinking in the sea. If closely pursued and there is no escape, they scold and grin like an angry cat. If they escape the ene- my, as soon as they are safe they turn and deride him with various diverting tricks, such as standing on end in the water, jumping over the waves, holding the paws over the eyes, as if to shade them from the sun while looking at the enemy — then lying flat upon the back and stroking the belly. In their escape they carry their sucklings in their mouths, and drive before them those not fully grown. They were formerly taken, by the Russians and Indians, by means of nets, clubs, and spears. The young are said to be delicate eating, the flesli resembUng lamb. The flesh of the old ones is insipid and tough. ZOOLOGY. 127 " The otter is never seen upon land. He is purely an aquatic animal. AVhen he swims he turns upon his back and propels himself with great rapidity. The fore-paws are rounded like a cat's, but the claws of the older ones are generally worn off. The hind-legs, or propellers, are broad and flat, like paddles, and are used very dexterously. The seal much resembles the otter, seen at a distance, but he swims upon his belly, and the hunter seldom mistakes the one for the other. The otter sleeps in the water, lying upon his back, and anchors himself from the motions of winds and waves by drawing a string of kelp across his breast, just below his fore-legs. "When discov- ered in this position, they are often approached very near by the hunters. They are very buoyant in the water, but when the chase has been long continued, and the blood of the otter becomes heated by the exercise, on being shot the body sinks rapidly to the bottom, and never rises. More than half the otters shot are lost in this way. " Once a day the otter comes near the shore for food. He eats every thing that grows in salt water, and is particularly fond of abelones {haliotiis), mussels, and sea-eggs. At high water the abelone loosens its shell from the rock, to receive the nourishment which the overfloAving waters bring to it, and it is then easily taken from the rock and removed from its shell. The otter is well acquainted with all the peculiarities of this fish, and this opportunity to capture it for food." The common seal, a species of phoca, is abundant along the coast. The sea-lions, of the Otaria genus, frequent the coast from May to November, making their homes during the winter in some other cUme, but where is not known. They delight to collect on clear summer days on rocks near the water's edge, and bask in the sun. They may often be seen on the rocks near the Golden Gate, and heard too, for they keep up a kind of barking or growling in chorus, which grows louder as they see any one approaching. They do not wait, however, to let a man come near, but pitch off into the sei before he is within 128 RESOURCES OF CALIFORNIA. two hundred yards of them. Their color varies from light yellowish-brown to dark brown. § 96. Vultures. — The Californian Y\\\i\\v^ {Cathartes calif or- ma77t/5), sometimes im])r()perly called "condor," the largest bird on the continent, and next to tl.e condor the largest flying bird in the world, inhabits all parts of the state, though it is not abun- dant in any place. It is as prominent and peculiar a feature of the birds of California as the grizzly bear among the quadru- peds. It is very shy, and is rafely killed. The total length of the Californian vulture is about four feet, and its width from tip to tip of the outstretched wings, ten feet or more. Its color is brownish black, with a white stripe across the wings. The head and neck are bare, and red and yellow in color. The bill is yellowish white, and the iris carmine. Dr. Newberry says : *' A portion of every day's experience in our march through the Sacramento valley, w^as a pleasure in Avatching the graceful evolutions of this splendid bird. Its flight is easy and eflbrt- less, almost beyond that of any other bird. As I sometimes recall the characteristic scenery of California, those intermina- ble stretches of waving grain, with here and there, between the rounded hills, orchard-like clumps of oak, a scene so solitary and yet so home-like, over these oat-covered plains and slopes, golden yellow in the sunshine, always floats the shadow of the vulture." Dr. Ileermann, of the United States Pacific Railroad Sur- vey, wrote thus: "Whilst unsuccessfully hunting in the Tejon valley, we have often passed several hours without a single one of this species being in sight, but on bringing down any large game, ere the body had grown cold these birds might be seen rising above the horizon and slowly sweeping toward us, intent upon their share of the prey. Nor in the absence of the hunter will his game be exempt from their rav- enous appetite, though it be carefully hidden and covered by shrubbery and heavy branches ; as I have known these marau- ders to drag forth from its concealment and devour a deer within an hour. Any article of clothing thrown over a carcass ZOOLOGY. 129 will shield it from a vulture, though not from the grizzly boar, who little respects such flimsy protection. My coat, used on one occasion to cover a deer, was found on our return torn by bruin to shreds, and the game destroyed. The Californian vulture joins to his rapacity an immense muscular power, as a sample of which it will suffice to state that I have known four of them, jointly, to drag off, over a space of two hundred yards, the body of a young grizzly bear weighing upward of one hundred pounds." The turkey-buzzard, or turkey-vulture [Gathartes aura), specifically the same with the bird known by that name in the Atlantic states, is found in all parts of California. From the tip of the bill to the end of the tail it is about thirty inches long, and six feet from tip to tip of the outstretched wings. The head and neck are bare, covered with a bright-red wrin- kled skin. The plumage commences below that, with a circu- lar ruff of projecting feathers. The color of the plumage is black, with a purplish lustre, many of the feathers havhig a pale border. The bill is yellowish in color. § 97. The baffle Mmiily. — The golden eagle [Aquila can- adensis) inhabits California, and indeed all parts of North America. Its length is thirty or forty inches ; its color on the head and neck is yellowish brown, white at the base of the of the tail, and brown, varying to purplish brown, and black elsewhere. The bald eagle [Ilalicetus leucocephalos) was abundant in California ten years ago, and is still often seen along the Sac- ramento, San Joaquin, and Klamath Rivers. It frequents rap- ids for the purpose of catching fish, which seem to furnish the larger part of its food. It is from thirty to forty inches long, white on the head and at the base of the tail, and brown- ish black on the breast, wings, and back. The fish-hawk {Pandio7i carolinensis) is found along all our large rivers. It is from twenty to twenty-five inches long. The head and under pai-ts are white, with pale yellowish-brown spots on the breast. The back, wings, and tail are dark brown. 6* 130 EESOUECES OF CALIFOENIA. The goshawk (Astur atriccqnllus) is of the same size with the lish-hawk, and in color is dark — a bhi'.sh-slate above, and mottled- white and light ashy-brown beneath. There are seventeen other hawks in the state, most of them small and i-are. § 98. Oiols. — California has nine species of owds, namely : the barn, great-horned, screech, long-eared, short-eared, great gray, saw- whet, burrowing, and pigmy owls. All of them are found extensively on the continent, beyond the limits of our state, and all save the last two are common east of the Mis- sissippi. The burrowing owl [Athene cunicularia) is ten inches long, ashy-brown above and whitish-brown beneath, variegated by spots and bands of white and dark-brown. Dr. Newberry says : " The burrowing owl is found in many parts of Califor- nia, where it shares the burrows of Beechey's and Douglas's spermophiles. We usually saw them standing at the entrance of their burrows. They often allowed us to approach within shot, and, before taking flight, twisting their heads about, bowed with many ludicrous gestures, thus apparently aiding their imperfect sight, and getting a better view of the intruder. When shot at and not killed, or when otherw^ise alarmed, they fly with an irregular, jerking motion, dropping down much like a w^oodcock at some other hole." The pigmy owl ( Glaucidhim gnorna) is seven inches long, and inhabits the w^ooded districts. It flies about actively in the daytime, and appears to subsist chiefly on sparrows, which it catches in daylight. The general color is brownish-olive above and brownish- white beneath. § 99. Hoad-runner. — The paisano, or road-runner ( Geococcyx calif ornianus)^ is one of the most remarkable birds of the state. It hves almost entirely upon the ground, very rarely flies, and frequents the highways, along which it will run from any one approaching. Its speed is nearly equal to that of a common horse, and it often furnishes an exciting chase to the solitary rider. It is abundant in the valleys and low hills, and makes ZOOLOGY. 131 its home among the bushes. The bird is akin to the cuckoo, ^ and its generic name signifies " ground-cuckoo." Its length is from twenty to twentythree inches, of which twelve are taken up by the tail. The general color is olive-green above and white beneath; the central tail-feathers are olive-brown, the others dark-green — all edged and (except the central two) tipped w^ith white. Dr. Heerman says : " I have not witnessed the follownig feat, but am assured by many old Californians that this bird, on perceiving the rattlesnake coiled up asleep, basking in the sun, will collect the cactus and hedge him around wnth a circle, out of wdiich the reptile, unable to es- cape, and enraged by the prickly points opposing him on every side, strikes himself, and dies from the eifects of his self-inocu- lated venom." § 100. Woodpeckers. — There are eleven species of wood- pecker in the state ; of which two, the Californian [3Iela7ier2)es formicivorus) and Lewis's (Ifelanerpes torquatus), are worthy of special mention. The Californian woodpecker is called by the Spanish Cali- fornians the carpintero, or carpenter, because he is in the habit of boring holes with his beak in the bark of the nut-pine, red- wood, Californian white oak, and Western yellow pine, and then storing acorns in them for his winter use. The holes are just large and deep enough to hold each an acorn, wdiich is hammered in so that there is no danger of its falling out. The acorns on the northern side of the trees, where they are joro- tected from the rains, wdiich come from the southward, often keep good for years. The bark of the nut-pine is preferred, probably being softer and more regular in grain than other bark. The holes are bored to within two or three feet of the ground, and to a height of fifty feet — sometimes, but rarely, in the limbs as well as the trunk. From thirty to fifty holes are often found in a square foot. In seasons when or places where acorns are rare, the woodpecker wiU put away hazel-nuts in the same manner. The squirrels often plunder the stores, and then the birds attack the thieves, darting down upon them and peck- 132 KESOUKCES OF CA.LIFORNIA. ing them with their Ijeaks. When the squirrel sees the prop- erty-owner coming, he hurries to a hole, or gets under a hmb, where the woodpecker cannot conveniently strike him. Some- times Indians and even white men are glad to avail themselves of the woodpecker's stores as a protection against starvation. The length of the bird is nine inches ; the anterior part of the body above and the tail are black ; the belly, rump, a patch on the forehead, and a collar on the neck, white; and the crown, and a short occipital crest, red. Dr. Newberry says : "This beautiful bird, the rival and representative of the red- headed woodpecker [of the Atlantic slope of the continent], is an inseparable element of the scenery of the Sacramento val- ley. While we were encamped under the wide-spreading oaks of that region, I had a very good opportunity to study their habits, as they would come into the trees in the shade of which I was lying. They are not shy, and frequently came round in considerable numbers. Their manners are the very counter- part of the Eastern ' red-head,' and their rattling cry is not unlike his. Like the ' red-head,' I have seen two or three of them amuse themselves by playing 'hide and seek' around some trunk or branch ; and like the ' red-head,' too, they de- light to sit on the end of a dry limb, and fly ofi" in circles for the insects which come near them." Lewis's woodpecker is in color dark glossy green above and gray beneath, with dark-crimson patches on the sides of the head and belly. The feathers on the under part are bristle-like. It prefers an elevated home, and is found ten and twelve thou- sand feet above the sea. § 101. Humming- Birds. — There are four humming-birds in CaUfornia, all different from those found in the Atlantic states. The white-throated swift, a bird resembling the swallow, but smaller, is common in the Colorado Basin. We have a whip- poor-will different fi-om the one known in the Eastern states. Two night-hawks are found in our state, one of them appear- ing on this slope of the continent only in the vicinity of tlie Colorado, and on the other slope not extending far beyond the ZOOLOGY. 133 Rio Grande. The belted king-fisher {Cenjle aleyoii) is at home in California as well as in all other parts of tlie conti nent. § 102. Fly-catcher. — The family of fiy-catehers [Colopteri- dw), which connects the non-melodious with the true singing birds, is represented in California by eleven species, most of which are not seen in the Atlantic states. They are small birds, from five to nine inches in length, and their colors are usually dull. Most of them have their upper mandible bent down abruptly at the tip ; and they always have twelve feath- ers in the tail. One of the most common and the best-known of the fly-catchers is the bird called the " pewee." § 103. Singers. — The zoological sub-order called Oscmes, or singers, has one hundred and nine species in our state, inclu- ding two mocking-birds, three thrushes, two blue-birds, three robins, three larks, five blackbirds, eleven finches, six wrens, six swallows, six warblers, one martin, one bunting, six tit- mouses, one snow-bird, two grosbeaks, one cow-bird, one ori- ole, one crow, three ravens, three jays, one w\ater-ouzel, two magpii;3s, and so on. Some of these birds are not called "sing- ers" in common language, but they all belong to the Oscines sub-order, which is marked by a peculiar muscular apparatus for singing, composed of five pairs of muscles in the thi'oat. Though there are many species of Oscines in the state, yet the birds are not so numerous, so melodious, nor are they heard so often, as the feathered songsters in the Eastern states. The traveller may proceed for days in the Sacramento Basin, during the summer season, without hearing more than a few chirps. Our singing-birds have been multiplying very rapidly of late, because of the settlement and cultivation of the land, whereby their supply of wdiolesome and palatable food is much increased, and their enemies the hawks are driven away. Most of our swallows, one mocking-bird, one black-bird, and one raven, found in California, are also seen east of the Mississippi ; but all our jays, robins, blue birds, and magpies, and our oriole, are, of species not found in the Atlantic states. The majority 134 EESOUECES OF CALIFOKNIA. of the Oscines indigenous on this coast are unknown in the older states. Our mocking-birds are never domesticated, and are not to be compared to the mocking-bird of Virginia. § 104. Scratchers. — The ornithological order oi Rasores, or scratchers, is represented in California by eleven species, name- ly : one pigeon, two doves, three grouse, two quails, one par- tridge, and one sand-hill crane. The pigeon, partridge, grouse, quails, and one of the doves, are specifically difierent from the birds known by the same name east of the Mississippi. The wild-turkey is not found in our state. The most abundant and prominent of our scratchers, the Californian quail [Lophortyx californicus), is found in all the valleys of CaUfornia and Oregon. Its breast and upper parts are lead-colored, with an olive-brown gloss on the back and wings ; the chin and throat are black, with a white line run- ning backward from the eye ; the forehead is brownish-yellow ; the belly is pale-buff, wdth an orange-brown round spot in the middle, changing to white at the sides ; the feathers on the back and sides have a central streak of white, and those on the top and sides of the neck have black edgings. The head bears a crest numbering from three to six feathers, usually five, about an inch and a half long. The shafts are bare, very slender, and, though all are m a straight fine on the longitu- dinal medial line of the head, they are so near together as to look Hke but one shaft, more especially as the fine, fur-like bushes at their tops all combine to form a compact little plume. These feathers are usually erect, the plume leaning forward when the bird is trying to look its best in the presence of com- pany ; but when running about in the grass, and not thinking of its appearance, the crest is lowered, falling forward over the bill. The Californian quail has two notes — the song and the call. The song of the Atlantic quail is in two notes — the well-known whistle, sounding like " Bob- White." The song of the Cali- fornian quail has but one note, beginning like the " Bob" and ending like the " White" of its Eastern relative. The calls ol ZOOLOGY. 135 tlie Atlantic and Pacific quails are nearly alike, and may be represented by the syllables " hi-re-he." — " As a garae-bird," says Dr. Newberry, " the Californian quail is inferior to the Eastern one, though perhaps of equal excellence for the table. It does not lie as Avell to the dog, and does not afibrd a good sport. It also takes a tree more readily than the Atlantic quail. Like its Eastern relative, the cock-bird is very fond of sitting on some stump or log projecting above the grass and weeds which conceal his mate and nest or brood, and espe- cially in the early morning, uttering his peculiar cry." The plumed quail {Oreortyx pictus)^ likewise called the " mountain quail," while the Lophortyx callforniciis is often styled, the " valley quail," is peculiar to this coast, and is one of the most beautiful features of its ornithology. It is a partridge ten inches long, very plump in shape, handsome in color, ma- jestic in its bearing, and graceful in motion. Its head is sur- mounted by a crest of two straight feathers, three and a half inches long, which hang backward, one immediately over the other. The breast and neck are lead-colored, the upper parts generally olive-brown ; the throat, and head beneath the eyes, orange-chestnut ; the abdomen white. There are numerous variegations of white, black, and minor shades, on the plumage, all contributing to heighten its beauty. The mountain partridge lives in the hills and mountains, from the Teion Pass to the Columbia River. Its sono^ sus;- gests the sound represented by the word " whoit," whistled fuller and louder than the song of the Californian quail. It roosts upon the ground ; and if bushes be near, in which to hide, it will rather run than fly from its enemies. It seldom flies more than two hundred yards at a time. The cock is equally attentive with the hen to the young brood, which usu- ally varies from eight to twelve in number. The families seem to be much attached to each other, and if they are scattered, they are very uneasy until all are collected again. In such cases, the hunter can entice them to come to him by imitating the call of either old or young. They are easily domesticated 136 KESOUKCES OF CALIFORNIA. — more readily than their brethren of the valley. The moun- tain i^artridge hates the quail, and when brought into its pres- ence always attacks it; the smaller bird makes no resistance, Gambel's quail {Lorphortyx gambelli) is a bird diiFering from the Californian quail only in having duller colors, and is per- haps specifically the same, the difference in color being a mere accident of climate. Occasionally, white quails, very similar in form and size to the Lophortyx calif ornicus^ are found near Humboldt Bay. The sage-cock, or cock of the plains ( Centrocercus iirophasi- aniis), the largest of the American grouse, often weighing five or six pounds, inhabits the dry plains in the vicinity of Pit River. It is sometimes twenty-nine inches long, and forty-two inches across from tip to tip of outstretched wings. Its color above is variegated with black, brown, brownish-yelloAv, and whitish-yellow ; its breast is white, its belly black. The male has bare, flame-colored patches of skin on the neck, which are ordinarily hidden by the feathers, but which are plainly visible when he struts about before the hen, with his neck puffed out like a pouter pigeon's. The sharp-tailed grouse {Pedioccetes pliasianellus) is also found in the northeastern corner of the state. It is eighteen inches long, light brownish-yellow above, varied with black, and white beneath, the feathers on the breast and sides having brown marks shaped like a Y. The tail is long and sharp, the central feathers and the others growing gradually shorter as they approach the sides ; there are eighteen feathers in the tail. The dusky grouse (Tetrao ohscurus) inhabits the coniferous forests of the Sierra Nevada, in the northeastern part of the state. The cock, according to common report, is the hand- somest of all the American grouse. It is twenty inches long, dark-brown above, mottled with lead-color, and lead-color be- neath. There are twenty feathers in the tail, which is broadly tip))ed with a light slate-color. The band-tailed pigeon ( Columba fasciata)^ the only wild ZOOLOGY. 137 pigeon found on the Pacific coast, bears a strong resemblance in form, size, and color, to its congener in the Atlantic states, and has similar habits, but is not numerous. Small flocks mi- grate through the state every spring and autumn, and some of them spend the summer here. The white-winged dove [Mclophelia leiicoptera) has been seen in the southern part of the state, but is very rare. It has white spots on its wings, whence its common and technical names are derived. The common dove [Zenaidura carol'mensls) of the Atlantic slope is found on the Pacific slope as well. The sand-hill crane ( Grus canadensis) are found from the meridian of Cincinnati to the Pacific, and are not rare in Cali- fornia. They spend the winters in our valleys, and in the spring migrate to the Klamath Lakes and farther north, where they spend their summers and breed. Subsisting upon vege- table food exclusively, they are themselves good to eat, and are frequently seen in the San Francisco market. § 105. Waders. — The order of waders (^Grallatores) is rep- resented in California by forty-one species of birds, namely : one crane, two herons, two bitterns, one fly-up-the-creek, one ibis, six plovers, one oyster-catcher, two turnstones, one avoi- set, three phalaropes, one stilt, one willet, one godwit, one curlew, five snipes, five sand-pipers, one sanderling, three rails, and one coot. The oyster -catcher, one turnstone, one plover, and one heron, are the only species in the list not found east of the Mississippi, and none of them have such value or pecu- liarities as would give interest to a particular description of them. § 106. Swimmers. — California has sixty-six species of the order of swimmers [Natatorcs) : of these there are two swans, six geese, twenty-two ducks, four albatross, two petrels, seven gulls, four terns, three pelicans, three cormorants, four guille- mots, one loon, and various miscellaneous species. One swan, all the albatrosses, five gulls, the two petrels, the loon, and one guillemot, are found only on this coast. 138 RESOURCES OF CALIFORNIA. The trumpeter-swan {Cygnus hiiacmator) is a very large bird, measuring five feet from the point of the bill to the end of the tail, and six feet across from tip to tip of the outstretched wings. The plumage is snowy-white in color, its legs and bill black. The name of " trumpeter" is given to it because of its clarion-like scream, which is heard as it flies. It frequents the lakes in the northern and northeastern parts of the state, and is sometimes seen in the rivers. It is a shy bird, and is rarely killed. The American swan, founds also on the Atlantic slope of the continent, is similar in appearance and size to the trumpeter, but lacks its loud voice, and is otherwise distinguishable from it chiefly by having an orange-colored spot on its bill in front of the eye, whereas the bill of the Cygnus buccinator is en- tirely black. Wild geese are very abundant in California during the sj)ring and fall, when they pass through on their migrations. Among them are the Canada goose {Bernicla canadensis)^ the snow-goose {Anser Jiyperboreus)^ the white-footed goose, or " speckled belly" {Anser ergthrojms), Hutchins's goose (7?e?-- nicla Imtchinsii), and the black brandt {JBcryiicla nigricans). Hutchins's goose is more abundant than any of the others. Some of them, Avhile in the state, get all their food in the tules ; others in the spring resort to the fields of young grain, where they pasture. Dr. Newberry says : " I was much interested in noticing the perfect harmony of intercourse which seemed to ex- ist among the smaller species. They intermingled freely while feeding, and when alarmed arose without separation; and I have seen a triangle flying steadily high over my head, com- posed of individuals of three species, each plainly distinguish- able by its plumage, but each holding its place in the geomet- rical figure, as though it was composed of entirely homogene- ous material ; perhaps unequal members of the darker species, with three, four, or more pure snow-white geese flying togeth- er somewhere in the converging lines." AmoniT the ducks of California are the mallard and canvas- ZOOLOGY. ' 139 back. The meat of tlie latter has not so fine a flavor as in the Eastern states, probably because it does not here find the wild celery upon which it feeds along the streams of the middle states. Many of the geese and ducks pass the winter in California, where they find an abundance of food in the gram-fields and tules. The murre, or foolish guillemot ( Zfria ringvin), is similar to the gulls, seventeen inches long, dark-brown above and white beneath, with transverse stripes of ashy-brown on its sides. Its throat is brown in summer and white in winter. It frequents the islands along the coast, and lays its eggs there on the bare ground or rocks. These eggs are wonderfully irregular in form, size, and color, but are generally about three and a half inches long, sea-green in color, with dark-brown spots of angu- lar shapes on them, Quantities of these eggs are obtained ev- ery year at the Farallones, and are sold in the San Francisco market at about half the price of hen's eggs per dozen, or, if taken by weight, at one-fourth. Their taste, however, is rank, and they are not used by those who can aftbrd to buy the hen's eggs. Dr. Heermann says: "At one o'clock every day during the Qgg season, Sundays and Thursdays excepted (this is to give the birds some little respite), the egg-hunters meet on the south side of the island. The roll is called, to see that all are present, that each one may have an equal chance in gathering the spoil. The signal is given, every man starting off at a full run for the most productive eggiug-grounds. The gulls {Larus occidentalism Western gull), understanding, apparently, what is about to occur, are on the alert, hovering overhead, and await- ing only the advance of the party. The men rush eagerly into the rookeries ; the aff"righted murres have scarcely risen from their nests, before the gull, with remarkable instinct, not to say almost reason, flying but a few paces ahead of the hunter, alights on the ground, tapping such eggs as the short time will allow, before the egger comes up with him. The broken 140 RESOURCES OF CALIFORNIA. eggs are passed by the men, who remove only those which are sound. The gull, then returning to the field of its exploits, procures a plentiful supply of its favorite food." § 107. Fishes. — The fishes of the coast and rivers of Califor- nia are all different from those of the Atlantic side of the conti- nent, with the exception, perhaps, of one species of the halibut. The cod and shad, two of the most important fishes of the sea of the Eastern shore, and the lobster among crustaceans, are here wanting, as also the cat-fish kind in the rivers. Otherwise our waters are probably as rich in game for the fisherman as those of any country. § 108. Salmon. — The most important fish of California is the quinnat salmon [Sahno quinnat)^ a species found from Point Conception to the Columbia River. Its color above is oliva- ceous browm, changing to salmon-color beneath. The largest one ever caught Aveighed sixty-two pounds ; the common size is from ten to thirty pounds. The salmon are born in the rivers, but go down to the sea, where they spend part of every year. They commence to enter the bay of San Francisco in Novem- ber, and continue to come in for three or four months. They ascend the Sacramento and San Joaquin Rivers and some of their smaller tributaries, deposit their spawn, and in .June go out to sea again. They come in lean and go out lean, but in the late winter and early spring they are fat. There are two com- mon popular errors, that the salmon do not eat after leaving the sea, and that they never get back alive. The former error is owing to the fact that no large articles of food are found in its stomach, and the latter to the fact that when going out all are lean, and that many are found dead along the banks of salmon-streams. But the salmon find their chief food in mi- nute animalculas, and not in fish, for catching which they seem to be so well fitted, with their large mouths and sharp teeth. It is well known that the salmon bite like trout, and furnish excellent sport in clear water to the skilful fisherman with the fly. They dislike the mud with which the streams emptying into San Francisco Bay are filled by the miners, and therefore ZOOLOGY. 141 do not go far from the sea or ascend the small tributaries ; but elsewhere they ascend every little brook, up to points where there is scarcely enough water for them to swim ; and in these expeditions they are so much exhausted and bruised that they soon die ; but the number thus killed is as nothing compared w^ith those which go out to sea again. The female salmon having found a suitable place, uses her nose to dig a trench in the sand about six feet long, a foot wide, and three inches deep, and having deposited her spawn in it, throws a little sand over it wath her tail, and departs, leaving her eggs to be hatched and the offspring to be fed as best they can. In the month of May the young salmon are found on their way to the sea, from three to six inches long. It is supposed that the salmon always return to the river in which they were born ; so that the salmon born in the Klamath River never enter San Francisco Bay, nor do those born in the Sacramento and San Joaquin Rivers ever enter Humboldt Bay. Although the sea- son in which salmon are abundant in the rivers extends from November to June, yet some of them are found in the streams of California at all seasons, and they can be had fresh in the San Francisco market every day in the year. The quinnat is the chief salmon of all the streams and bays of California, but Gairdner's salmon {Fario gairdneri) is found in the Klamath River, and the stellatus salmon in Humboldt Bay and its tributaries. Gairdner's salmon has a silvery-gray back, silvery sides, and a yellowish-white belly. The body has numerous indistinct, blackish spots. The stellatus salmon is light-olive in the back, yellowish- white on the belly, and rarely exceeds two or three pounds in w^eight. § 109. Halibut. — There are two species of halibut on the coast of California, the Californian {IIlj)2^oglossus califoriiicus) and the common {Hlppoglossus vulgaris). There is some doubt whether the latter species is properly named ; if it be, then w^e have one species of fish found on the Atlantic coast. The CaUfornian halibut is a slender fish, weighing at the largest twenty-five pounds, in color grayish-brown above and 142 EESOIJKCES OF CALIFOKNIA. white below. The halibut prefer a colder climate, and are not sufficiently abundant in this latitude to sustain a special fish- ery ; but a few are in our market throughout the year. They live in deep water, and in places where the bottom is rocky. They eat little fish and shell-fish, and bite readily at the hook. Their meat is very delicate. § 110. Turhot. — The turbot { Pleuronychthys rugosus) is the only large fiat-fish, except the halibut, found along our shore. It sometimes grows to weigh twenty pounds, but the common size is from three to ten pounds. The turbot inhabits deep waters and rocky bottoms, eats fish, and bites readily at the hook. It is one of the best fish in our market. § 111. Sole. — We have four species of small flat-fish, com- monly called soles [Psettlchthys sordid us, PseUichthys tnela- nostictus, Parophrys vetidus, and Platessa bilineata). They are so much alike, that they are not distinguished from one another by fishermen generally. The Platessa bilineata is the largest, sometimes weighing two i^ounds; the others rarely exceed one pound. They frequent the shallow waters of the bay of San Francisco, and are caught abundantly in nets at all seasons of the year. The flat-fishes do not bury themselves in the mud here through the winter, as they do in the North At- lantic. The soles feed on Crustacea, little fishes, and marine animalculae. § 112. Mackerel. — The mackerel {Scomber dlego) is found north of Point Conception. It is good, but not more than half as large as the Atlantic mackerel. The Cahfornian mack- erel rarely exceeds ten inches in length. It lies near the sur- face of the water at sea, and is not fond of entering bays or going very near the shore. Like its Eastern congener, it bites readily at any white rag or shining w^hite substance jerked through the w^ater. § 113. Pock-Fish. — The rock-fish furnish the main supply of fish in the San Francisco market. All belong to the genus Sebastes, of which there are eight species, the most important being the red (rosaceus), black {melano2^s), and wharf rock- ZOOLOGY. 143 fish {auriculatiis). The red rock-fish grows to weigh twenty pounds ; the other species rarely exceed four or five. The w^iarf rock-fish is the only one caught in the bay ; the others live out at sea, in deep water and on rocky bottoms : they eat crabs and shell-fish, and bite freely at hooks. They are always m market, and their meat is excellent at all seasons. § 114. Sturgeon. — We have three species of sturgeon, of which the only important one is the Californian sturgeon [Aci- penser brachyrinthus)^ which sometimes grows to be seven feet long and to weigh two hundred pounds. The sturgeon is a sea-fish, Avhich enters fresh water to spawn, but it is caught in the bay of San Francisco and tributaries at all sea- sons of the year ; whereas in the Eastern states there are sea- sons for sturgeon in the market, as there are for beans and peas. The sturgeon eats the slimy matter, both animal and vege- table, at the bottom of the sea. It never bites, its mouth being circular in form, and fitted only for sucking. It has a habit of shooting up from the bottom and springing out of ^^'ater, and then falfing flat upon its belly, Tnaking a loud splash — very difierent from the porpoise, wdiich also darts out of the water, but always strikes head first, making little noise. Some ichthyologists suppose that the object of the sturgeon in thus falling on the water is to free itself from parasites ; others that it is merely a kind of play. The spawning-season is not known precisely, but it is probably from December to May. The meat of the sturgeon is coarse, and in the market is worth only about one-fourth or one-sixth of that of the better table fishes ; but the sturgeon-fishery is profitable, because of the abundance and large size of the fish. § 115. Jew-Fish. — The Jew-fish [Stereolejns gigas), one of the largest scale-fishes — weighing sometimes five hundred pounds — is abundant south of Point Conception, and rarely straggles as far north as San Fj-ancisco Bay. Only two have been caught near the Golden Gate, and one of them filled the city with wonder. It is a bottom-fish, living in deep and shoal 144 EESOURCES OF CALIFORNIA. water, and frequenting lagoons and kelp. It often comes to the surface, and, xiccording to report, goes to sleep there. It bites readily at the hook, and may be taken with harpoons. The meat is very good. §116, Sun-Fish — The sun-fish { Orthagorisciis analis) is found occasionally south of Point Conception, where it is seen floating on the surface, in accordance with the habits of the genus everywhere. It weighs from one to a hundred pounds. Its form suggests the idea that the body has been cut off near the broadest part, and the tail sewed on. § 117. Green-Fish. — The green-fish (^Opplomona panther i- na)^ generally called cod in the San Francisco market, but having no relationsliip to the true cod, is abundant along the coast. It grows to be about two feet in length. The meat is coarse, and green in color ; and the fish has little commercial value. § 118. Sea-Bass. — The sea-bass [Johiiius nohilis) is a plain, oval fish, bluish-gray in color above, silvery below, weighing from fifteen to forty pounds. It is closely related to the weak- fish of the New York market. The meat is white and deli- cate, and always commands a high price in the market. It is a surface-fish, and sometimes enters the bays, but is not abun- dant anywhere. It is caught from March to November. § 119. Sheepshead. — The Californian sheepshead {Lahrus pulcher) is a black fish, with a broad, bright-red band sur- rounding the body, and weighs from one to twelve pounds. It has white, broad, projecting teeth, like those of a sheep. It has no relationship to the Atlantic sheepshead, but is a conge- ner of the black-fish of the New York market. The meat has a very fine flavor when fresh, but loses its delicacy after being dead a day or two. It is found south of Point Conception, on rocky and kelpy bottoms, from April to October. Its food is chiefly shell-fish. § 120. Smelts. — We have four species of fish called smelts (^Atherinop)sis callforniensis., Atherinopsis affiiiis^ Osmerus preciosus, and Osmerus similis). The Atheri?iopses are not ZOOLOGY. 145 true smelts, but belong to the same genus with the sandcr- lings of the Atlantic, Avhich last are thrown away, or used only as bait ; whereas our Atherinopses are valuable fishes. The Athermojysis callforniensis forms the great bulk of the smelts in our market. It is the largest of the Pacific smelts, some- times reaching a length of fifteen inches, and a pound in weight. The Osmerus species are small. All of them have bright silver bands along their sides. The smelts are more abundant here than on the Eastern coast, and are the best of our small fishes. They are caught at all seasons of the year ; in the bays with nets — never at sea, or witli hooks. § 121. A72chovies. — ^There are two snachoYies ^{J^ngrauUs mordax and JEnc/rcmlis 7iamis) on the coast of California. They are so nearly alike, that they are undistinguishable ex- cept by ichthyologists. Both are small, from four to six inches long, very delicate in flav^or, but very bony. They are fully equal to the European anchovy for the table. They feed on minute animalculae, go in shoals, and are caught with nets in the bays at all seasons of the year. § 122. Sardine and Her ring. — The sardine [Meletta ceru- lea) is abundant from Humboldt Bay to San Diego. It grows to a length of eight or nine inches, and is therefore much larger than the Mediterranean sardine, to which it is fully equal in flavor. It is found along the coast from April to October, and is caught in the bays with nets. The herring {Clupea mirahilis) is not so abundant as the Atlantic species, nor so large, but is equal in flavor. It comes in the spring, and goes in the autumn. § 123. Viviparous Fishes. — The viviparous or embiotocoid fishes of this coast are a peculi:ir feature of its ichthyology. They constitute, perlinps, the most remirkable natural group of fishes in the world, and their discovery caused a m.ii ked sensation nmong zoologists. Other vivij)arons fishes had been previously known, but their young are brought forth in a very inunature condition ; whereas the little embiotocoid fishes are born with a fulness of development similar to that of warm- 146 RESOURCES or CALIFORNIA. blooded animals, and the moment after they leave the mother they are seen swirammg and taking care of themselves. There are seventeen or eighteen species belonging to the several genera, among which the embiotoca and holconotis are promi- nent. All are marine fishes save one, which is found in fresh water. They weigh from half a pound to three pouuds, and most of them are grayish brown above and silvery beneath. They are abundant in the market at all seasons of the year, and are called " perch" by the fishermen, though they have no relationship to the true percli. The meat is not good. The young are born from April to August. § 124. Fresh- Water Fishes. — Among the fresh-water fishes the most important is the brook-trout (Salar iridea)^ which is found in all the mountain-streams of the state, and oflers fine sport for fly-fishing. It not unfrequently grows to weigh two pounds, and, if report is to be believed, sometimes reaches ten and twelve pounds. In appearance and flavor it is similar to the trout of other countries. A fish called the salmon-trout \Ptychocheilus grandis)^ but not related to the salmon, the trout, or the salmon-trout, is found in all the large rivers and lakes of California. It grows to weigh thirty pounds. Its teeth are not in the mouth, but in the throat, where it crushes such shell-fish as it feeds upon. It bites voraciously, and is caught with the hook and with nets. The meat is poor, bony, and insipid. It is brought to the market in winter. The small ones are called pikes. A chub {Tygoma crasslcauda), and two suckers {Catosto- mus lahiatus and Catostomus occidentalis)^ never weighing more than three pounds, are also found in our rivers. They are not valuable. § 125. Shell- Fish and Crustaceans. — We have five species of shell-fish valuable for the table : one oyster, two muscles, one cockle, and a soft-shelled clam. The oysters are small, not finely-flavored, nor abundant. We have no lobster, but a prawn [Pallnuris)^ yerj similar to the lobster in size, color, flavor, habits, and general appearance, except that it lacks the ZOOLOGY. 147 large claws. Crabs are abundant. The abelone or aulone (Ilaliotis) is found as far north as Point Reyes, and abounds south of Point Conception. It is a mollusk with one shell, from five to seven inches across ; the shells are beautifully- iridescent, and are much used in the arts for buttons, knife- handles, inlaying, &g. Many vessels are engaged in fishing for them. The abelones stick to the rocks and to each other, collecting in some places in masses two feet thick ; the fi&Ler- men break them ofi* from the rocks with a spade. When the abelones do not suspect danger, they loosen their hold and raise their shells from the rock, and then the fisherm.xu may easily thrust his spade down along the surface of tho stone ; but if he alarms the abelone beforehand, he finds the shells fastened down to the rock with great power, and all the strength of a man is scarcely sufficient to pry one of them off. The meat of the abelone is eaten by the Chinese, who dry them ; the dried meat resembles horn in its color and hard- ness, and in shape looks as though it might be the hoof of a colt. The shrimp ( Crangon franciscorum) is found in the bays of California, and was very abundant a few years ago, but lately is getting scarce, at least in San Francisco Bay. § 126. Reptiles. — The snakes of California are not large, numerous, nor remarkable. Only one of them, the rattlesnake, is poisonous. The scorpion is found in the warmer portions of the state, but is not abundant. Tarantulas are common in Calaveras, Mariposa, Fresno, and Tulare counties. They belong to the same genus with the spiders, but the body growls to be three inches long and an inch wide, and the entire length from end to end of out- stretched legs is five inches. The body and legs are covered with silky, brown hair. The tarantula eats little insects of various kinds, but, unlike most other spiders, has no net. It lives in a hole in the ground not much larger tlian itself when pressed into the smallest compass, and the hole is covered by 148 RESOURCES or CALIFORNIA. a little door on a hinge, whicti closes by its own weight or by a spring. In the top of the door are several little holes, into which the tarantula can insert its claws when it wishes to en- ter ; and so quick are its motions when terrified, that it often disappears suddenly under the eyes of men pursuing it, and they have great difficulty in finding its hiding-place-. The door fits tightly, and is larger on the outside, so that it never sticks fast. The bite of the tarantula is poisonous, but not fatal — or at least has never, so far as I know, proved fatal in California. It rarely bites men, and generally flees when it discovers their approach. The tarantulas have dangerous enemies in several species of wasps, the females of which kill them by thrusting eggs into their bodies. When the larvae of the wasp are hatched, they make food of the carcass. So soon as the taran- tula dies, the wasp drags it to her hole, usually the deserted burrow of a spermophile, where she may collect twenty or thirty dead tarantulas in one season. There are three differ- ent species of these wasps ; one kind is blue, another yellow. Sometimes the wasp darts down repeatedly upon the taran- tula, and does not touch him except with her egg-planter, de- positing an egg at every thrust. On other occasions the two grapple, and the wasp continues to insert her eggs until the tarantula dies. The editor of a newspaper of Mariposa thus describes the killing of a tarantula : " Some of our readers may have heard of the tenacity with which the venomous tarantula is pursued by an inveterate enemy, in the form of a huge wasp — invariably resulting in the defeat and death of the former. ^ye were an eye-witness to one of these conflicts last week, while on a ramble among the adjacent hills. This is the sea- son when the poisonous tarantula leaves his well-fashioned abode to perambulate the dusty roads and smooth paths so often trod by the industrious miners, and about their haunts a dozen or so may be seen any day, of this hideous enlargement of the spider-race, within a circuit of a few yards, leisurely wending their way along the roads and by-ways. Often have ZOOLOGY. 149 we marked, with attentive curiosity, his awkward gait while lifting his long, unwieldy legs above the short blades of grass, and wondered for what uses and purposes this ugly little mon- ster was placed upon this beautiful globe. While attentively watching the motions of one of these insects during our walk, we were much surprised to see the object of our attractioit suddenly stop short in his wanderings and raise itself up to its full height, as though watching the coming of some unwelcome visitor. We at first supposed that it had just espied us, and was expecting danger at our hands ; but upon our retreating a few steps, he quickly crouched behind a tuft of dried grass, and remaining very quiet, seemed to make himself as small as pos- sible. A slight buzzing was heard in the air, and in a moment a wasp passed near, hovering on the wing over his trembling victim, the much-dreaded tarantula. Like some bird of prey, the wasp remained thus poised a moment, and then, quick as thought, darted down upon the enemy, and stung him many times with great rapidity. The tarantula, smarting under the pain, began a retreat, with all the speed of which he was ca- pable ; but the wasp hung over him with wonderful tenacity, and again and again struck him with his venomous sting. Gradually the flight of the tarantula became slower and more irregular, and at length, under the repeated thrusts of his con- queror, he died, biting the grass with his terrible fangs." Locusts and grasshoppers are abundant in the valleys ; mus- quitoes in the tules, and along the streams in the Sacramento Basin ; and fleas everywhere. § 127. Honey -Dew Aphis. — Among the noteworthy insects of the state is one which secretes a sweet liquid called " honey- dew," and deposits it on trees. It is transparent, thick like honey, and sweet, sometimes with a bitter after-taste, but more frequently having a flavor like parched corn. The leaves and twigs are covered with it, the deposit usually being nearly even, occasionally in spots or drops. The honey-dew is more frequently found on oak-trees than on any other tree or bush ; and oftener in dry seasons, and remote from the coast, than in 150 EESOUECES OF CALIFORNIA. wet weather or within the reach of the sea-fogs. A kind of molasses may be made by breaking oft' the twigs covered with the secretion, and boihng them in water. Honey-dew is found in most countries where tlie soil is bar- ren or the climate dry, and may be the same with the manna of the Hebrews. It is known, too, that various insects secrete sweet liquids ; and some of the Aphis genus are kept as milch- cows by the ants, which stroke them dowm or tickle them witli their antennae, when they want some of the sweet milk, and the captive Aphis obligingly squeezes out the secretion through her sides, which is industriously gathered by the milk-ants. ]sroTE. — Nearly all the information about tlie quadrupeds and birds of Cali- fornia, heretofore printed, may be found in the papers of Dr. J. S. Newberry and Professor S. F. Baird, in the United States Pacific Railroad Survey Re- ports. Most of my information about the fishes and fisheries, and much even of the language, is derived from the conversation of Dr. W. 0. Ayres, of San Francisco ; and I hope that, as he is the most competent man, he will some day treat the subject in a special work. AOEIOULTUEB. 151 CHAPTER YII. AGRICULTURE. § 1-^8. General BemarJcs. — Of the 160,000 square miles in the area of California, about 60,000 may be tillable; of which 16,000 are in the coast valleys, 30,000 in the low lands of the Sacramento Basin, 12,000 in the Sierra Nevada, and 2,000 in the Klamath Basin : while the 25,000 square miles of the Great Basin, the 15,000 of the Colorado Desei't within the limits o± this sUate, 30,000 of the Sierra Nevada, 26,000 of the Coast Mountains, and 6,000 of the Klamath Basin, may be put down as unfit for the plough. The 60,000 square miles of tillable land contain nearly 40,000,000 acres, but only 1,000,000 are cultivated in the state : of the remaining 39,000,000, one-fourth have a soil very thin, or not fertile because of the presence of alkaline substances ; one-half are too remote from market, even where the soil is good ; and a considerable portion is tied up in lawsuits, so that the ownership is doubtful, and the claim- ants dare not improve it for fear of losing the improvements. Only a small portion of the state is, therefore, fit for the plough. Not more than one acre in ten could now be tilled profitably, and I suppose that not more than one acre in four will be tilled during this century. As compared with the great agricultural states of the Mis- sissippi valley, in so far as relates to the proportion of rich land fit for the plough, California is at a great disadvantage, and is probably inferior in this respect to every state on the Atlantic slope of the continent. In Illinois and Indiana, nearly every foot of land has a rich soil and a level position. Again, Cali- ]52 FvESOUKCES OF CALIFORNIA. ■* fornia is at a great disadvantage as compared with her sister- states east of the Rocky Mountains, in the proportion of land fitted for growing a variety of crops. In the northern part of the Mississippi Viilley, nearly every acre will produce all the main articles of cultivation — fruits, maize, potatoes, and gar- den vegetables, as well as wheat and oats. In this state, how- ever, of the 40,000,000 tillable acres, at least 30,000,000 a^-e so dry, that they cannot, because of the want of moisture, and the impossibility of irrigation, be made to produce any crop save small graiu ; and of the remaining 10,000,000 ncres, three- fourths will not yield fruits, maize, potatoes, pumpkin**, or gar- den vegetables, without irrigation. These are undoubtedly vei-y serious drawbacks to the agri- culture of the state, but we have great advantages in many other points. The climate in the valleys, for instance, is so warm and the sky so clear through the winter, that vegetable life upon moist ground is almost as active in January as in July ; and our trees and shrubs have nearly twice as much time to grow and mature as in the free states of the East, where frost reigns from October to May. It is a well-known fact that California has produced larger specimens of garden vegetables, more thrifty growth and rapid development of fruit-trees, and larger crops of small grain to the acre, than any state in the Union, and many persons have supposed our soil to be richer. This supposition is erroneous, as I am satis- fied ; the superiority of the Californian productions is owing to the more favorable climate. I am not aware that any com- parison of our soils has been made by chemical analysis with those of Illinois, Missouri, Indiana, and Ohio ; but the proba- bility is, that the latter are more fertile. The loam is deeper ; ' the vegetation has been greater, and it has enriched the soil by the accumulation of its decomposed remains through thou- sands of years ; whereas in the valleys of California, the vege- tation is comparatively scanty, and the air is too dry to permit a decomposition of wood or grass to enrich the soil. The bot- tom-lands of the Sacramento and San Joaquin are far inferior AGRICULTURE, 153 in depth, blackness, and fertility of loam, to the valleys of the Miami, Wabash, and Illinois Rivers. § 129. Agricultural Districts. — Let us now consider the dif- ferent districts in the state suitable for agriculture. These dis- tricts, as I have said before, compose only a small part of Califor- nia, and have strongly-marked boundaries. They are nearly all valley-land, shut in by mountains. The Great Utah Basin has very little tillable land in the state ; there are small patches of fertile soil, but too slight to deserve special mention. The Colorado Basin is in about the same condition. It is possible that a considerable tract of land will be rendered fit for tillage by turning the Colorado into the low part of the desert ; but this is a remote contingency, and we have no accurate infor- mation about the character of the soil which it is proposed to irrigate in this manner. In a few little valleys, however, just at the eastern foot of the Coast Range, the soil is fertile, and the climate so warm, that fruits ripen six weeks earlier than on the western side. The largest tracts of tillable land in the Klamath Basin are the Scott and Shasta valleys, each about thirty miles long and four wide. They are elevated from three to four thousand feet above the sea ; the winters are severe, and frosts common in spring and autumn, and not rare in summer. Most of the soil is a gravelly clay, with a rich, sandy loam, along the im- mediate borders of the streams. Wheat, oats, apples, and. potatoes, do well ; but maize, peaches, melons, tomatoes, and sweet-potatoes, require a warmer climate. There is some level land in the eastern part of the Klamath Basin, near the Kla- math Lakes, but the soil is barren, and the vegetation like that of a desert. Del Norte county, which may be said to belong to the Klamath Basin, has 44,117 acres of land, of which 15,240 are covered with redwood, '7,277 with spruce, 19,204 are prairie, 2,400 are sand-ridges, and 4,712 are in la- goons. Most of the redwood land is level and fertile, but the timber is dense almost beyond example, and could not be cleared profitably, because all the redwood stumps throw out 154 EESOURCES OF CALIFORNIA. Sprouts, which grow up to trees. Much of the prairie-land is tei'tile and suitable for cultivation, but it is remote from the market. Klamath and Trinity counties are almost destitute of valley -land. Both, however, have numerous small spots of rich soil in their mountains, and both have a mining popula- tion who must be fed, and have the means and disposition to pay well for the necessaries and delicacies of life. The farms must be small, but the farmers are protected by the rugged mountains from the competition of those in the large valleys. Hay-Fork valley, one of the best little tracts of tillable land in Trinity county, is three thousand six hundred feet above the sea-level. The largest tract of level land in the plateau of the Sierra Nevada is the valley of Suisun River and Honey Lake, about sixty miles long and ten wide. The elevation is about four thousand five hundred feet above the sea; much of the soil is sandy and alkaline, with no indigenous vegetation save the worthless wild sage. Portions of the soil, however, are fertile, and there are a number of farms under cultivation. Honey Lake valley has the advantage of proximity to Washoe, and good roads for comnmnication. There are 115,000 acres in the valley, of which 20,000 are swampy, at least in wet sea- sons. Eagle Lake valley is about one-third the size of Honey Lake valley, and of similar soil. All along the western slope of the Sierra Nevada there are little spots of fertile soil, well suited for cultivation ; but with the exception of a few, they are too small to deserve special mention. The soil is usually a red clay or a black loam. The largest tillable spots on the ^vestern descent of the Sierra Ne- vada are in Plumas county. Sierra valley is forty-five miles long by six wide, and is drahied by a tributary of Feather River. Much of the land is barren sand ; much is tule-swamp, and only a small portion is fit for tillage. No water flows from the valley after July. The Big Meadows contain 100,000 acres ; Beckworth's valley, 90,000 ; Lidian valley, 20,000 ; Mountain Meadows, Red Clover valley, and Mohawk valley, AGKICULTURE. 155 10,000 acres each ; and Americau valley, 5,000. In all of them the soil is very sanely, but not barren. Tliey are from three to five thousand feet above the sea ; all shut in by high moun- tains; and all containing a considerable portion of swampy land. The low land of the Sacramento Basm comprises 20,000 square miles — about 3,000,000 acres. The Sacramento valley has several benches. The lowest bench is about twenty feet above the low-water mark of the river, and has a soil of sandy loam, richer immediately along the stream tlian farther off. The next bench, very irregular in height and width, has a soil of red, gravelly clay, which extends back to the mountains. In some places this clay becomes very soft in wet seasons — so soft, that weak cattle may mire down in it and be miable to extricate themselves. I knew a case where a team Of weak oxen, exhausted by hard driving and scanty food, sank down in a wet gravel-ridge, so that only their heads und a little of their necks and shoulders appeared above-ground ; and passing the place some months later, when the ground had become as hard as clay and gravel ever are, I saw the six bare skulls of the oxen resting with their chins on the earth where they had sunk down, and behind them were the projecting spines of the back-bone, with the yokes still on the necks of each pair of oxen. This gravel is seldom cultivated at present, but in many places it will produce good crops of barley. It forms at least one-half of the Sacramento valley. Very little of it can be irri- gated ; and the general belief is, that no corn, potatoes, garden vegetables, fruit, or grapes, can be grown on it without irriga- tion. The sandy loam produces large crops of wheat, barley, and oats, without irrigation. Fruit-trees and grape-vines thrive without it after they grow to be three or four years old, but in most places require it till they have taken a good start. Garden vegetables cannot be grown without irrigation, unless planted very early, and of such kinds SkS ripen before July. In the level valley there are no springs, nor are there any artesian wells ; so the only method of getting water is by pumping it 156 KESOURCES OF CALIFORNIA. up from common wells, for which purpose windmills are ex- tensively used, and thus most of the water used for irrigation is obtained. A large part of the valley, especially of that near the rivers, is subject to overflow ; and about once in five years a flood comes, sweeping away houses, fences, and cattle, de- stroying gardens, and covering the earth with a thick clay, which, instead of enriching the soil, is far poorer than the an- cient deposits of sandy loam, made before the miners had com- menced to tear down the mountains for their golden treasures. In these times of flood, so much of the valley is covered with water, that it looks like a great lake, and the pilots of the river steamers know the channel only by the rows of trees along the banks, for the banks themselves are completely hidden from sight. The flood rarely comes earlier than January or later than March. The bottom-lands along the Feather River are considered richer than those near the banks of the Sacramento. Tribu- tary to Sacramento valley on the western side is Cache Creek valley, about twenty miles long by five wide ; and connected with it is Clear Lake valley, a basin nearly circular in shape, and twenty miles across, surrounded by mountains. The lake is about one thousand feet above the sea. South of Cache Creek, and also tributary to the Sacramento valley, is Putah Creek, which drains Berreyesa valley, twenty miles long by two wide. These little valleys have very rich land ; and being shut in by near mountains, the soil is much moister than out in the open plain. The nearer to the coast and the farther north, the greater the moisture as a general rule ; and it may almost be said that the value of the land depends upon the moisture. In the northwestern corner of the Sacramento Basin, along the banks of Cottonwood Creek, there are some beautiful, moist, and fertile little vales. The Sacramento valley has very few trees, save along the banks of the streams and stream- beds, where oaks, sycamores, laurels, willows, buckeyes, birch, and wild grape, are the principal growth, marking in summer AGRICULTtTKE. 157 the places where the Avater runs in winter. The only trees growing a\vay from the watercourses are oaks, whicli are usually found in groves, and almost invariably Avithout under- growth. In the Sacramento valley there are about two hundred square miles, or one hundred and twenty-eight thousand acres, of tule-land, most of it above high tide, and covered by water only in times of flood. Very little of it has been drained or cultivated, and therefore we do not know its vaUie. All the tule-land is covered five or six feet deep with water in times of flood. The northern part of the San Joaquin valley is much like the southern part of the Sacramento valley. When the San Joaquin River approaches within fifty miles of Suisun Bay, it divides into three channels, which are separated from one an- other by islands of low tule-land. In times of high flood, the river spreads out and covers a space fifteen or twenty miles Avide. There is less gravel and clay but more sand in the San Joaquin valley than in the Sacramento valley ; the soil is drier, and contains more of alkaline substances, and the vegetation is more scanty. From Pacheco's Pass across to Firebaugh's Ferry, a distance of about fifty miles, there is not a tree, and in the autumn the country looks like a desert. At Fresno City the soil is nearly a pure sand, and the river at Ioav Avater is not more than six or eight feet below the surface of the plain. From the bend of the San Joaquin River, southAvard, a district sixty miles Avide by one hundred and fifty long, most of the soil is a barren sand, in many places covered Avith au alkaline efilorescence. The country about Kern River is very desolate, and be- tween that river and the Tejon Pass is a desert plain, covered Avith a scanty and useless vegetation. East of Tulare Lake, however, there is some rich soil, particularly in the " Four- Creek country," Avhere the Cahuilla River, issuing from the mountains, divides into half a dozen streams, Avhich spread out over a space twelve miles Avide, and then unite again, filling a 158 RESOTJKCES OF CALIFORNIA. large tract of fertile land with abundant moisture. Tulare Lake is fifty-seven feet above Fresno City, and might be drained, and its land converted into cultivated fields, but Avhether with a profit is a question now unanswerable. This country is so remote from the main centres of population, that probably the chief occupation for residents here must be the breeding of sheep and cattle. Turning our attention now to the valleys in the Coast Moun- tains, we find that in all the low land between latitudes 39° 30' and 40° 40', the soil is a rich and moist loam, very favorable for pasture and for maize, but not so well suited for small grain. In some valleys the season is six weeks later than it is across the mountain in the Sacramento valley. Russian River valley produces more maize than all the remainder of the state. Lying between the bend of Russian River and the head of Petal uma valley is Santa Rosa plain, which has a soil of rich sandy loam, excellent for grain, and probably favorable for the grape. Near the mouth of Russian River is the plain of Bodega, the best place in the state for potatoes. The soil is a light, sandy loam, which is kept moist by the sea-fogs. Peta- luma valley is the chief dairy district of the state. The soil is a rich, moist loam. Sonoma valley has a soil of red gravelly clay near the mountains, and a warm, sandy loam near the . creek. This is the chief grajDc district in the northern half of the state. Much of the soil is too thin to produce good crops of wheat. The grape is grown without irrigation, the distance from the ocean (about twenty-five miles) not being so great as entirely to cut oif the fogs. The bed-rock is in some places trap, in others sandstone, and in others magnesian limestone. The latter is supposed to be particularly favorable to the growth of the grape. Next to Sonoma valley is Napa, which has a deep, clayey soil, the strongest in the state, and therefore the best for wheat. In proportion to its size, it produces more wheat than any other part of the state. The upper part of the valley has a great deal of gravel, and may be good for grapes. A larger AGEICULTUKE. 159 proportion of the land is cultivated in IsTapa valley than in any- other part of the state, and the cultivation is more thorough. Suisun valley has a rich, sandy loam, good both for barley and wheat. Vaca valley, a small vale near Suisun, has a very warm, fertile soil, and is shut in by the hills from the wind. It will be an excellent place for fruit, and every thing will ripen early there. South of the straits of Carquinez is Diablo valley, which has an excellent soil for wheat and barley. So also has San Ramon valley, but the fruit has been badly nipped by frost during the last three or four years. Amador valley has a soil of rich sand at the sides and strong loam in the centre, all of it moist and fertile. Livermore valley, which may be consid- ered as the eastern half of Amador, is a bed of gravel, of little value for tillage. Suiiol valley has a rich, sandy loam. The Alameda plain, on the eastern side of San Francisco Bay, from San Pablo to San Jose, is one of the richest agricultural dis- tricts in the state ; the soil is fertile — in some places clay, in others sand. The soil on the western side of the bay is similar in character, but there is not so much of it. The lower part of Santa Clara valley has a fertile, black, sandless loam, changing to sand and then to gravel, which last is abundant toward the head of the valley, where very little of the land is tilled. The principal fruit district in the state is in the vicinity of San Jose. The plain east of Monterey Bay, in Santa Cruz county, has a fertile soil, and a climate peculiarly favorable to beans ; excel- lent crops of wheat and barley are also grown here. The soil of Pajaro valley is one of the richest and strongest in the state, and its crops of wheat and potatoes are unsurpassed. The Sa- linas has a rich, sandy loam in the lower part of its valley and near the river, but the sides and head of the vale contain much gravel ; the climate and soil are very dry, and only a small por- tion of the land is cultivated. The Cuyama, Santa Inez, and Santa Clara River valleys, are sandy and dry, and have but little tillage ; the last-named valley has a soil that is in places almost pare sand, too thin to secure a covering of grass in a 160 RESOURCES OF CALIFORNIA. wet winter. Most of the level land in Los Angeles, San Ber- nardino, and San Diego counties, is sandy and dry, and very little of it is cuUivated. Irrigation is necessary for fruit, vines, and vegetables. Wheat and barley do not produce well. Los Angeles is the principal grape district in the state ; the largest vineyards are planted in the bottom-lands of the Los Angeles, San Gabriel, and Santa Ana Rivers, where the soil is almost pure sand : and yet vineyards which have been in bearing twenty-live years, and have never been manured, are now as productive as ever. Allow a stream of water to run twenty- four hours through a field, and at the end of that time the bot- tom of the ditch will contain nothing but white sand, all the earthy particles in the soil having been dissolved and carried away. At the Monte the San Gabriel River sinks, and, after flowing two or three miles under-ground, reappears. The place where it sinks is very moist, covered with abundant vegetation, and, after Russian River valley, is the best district in the state for maize. § 130. Agricultural Frodiice.—CaWiornm has 1,000,000 acres of land in cultivation, about six-tenths of which are used for growing grains and roots emi)loyed as food for men and do- mestic animals. Of these grains and roots in 1860 (the agri- cultural statistics for which year were more fully reported than those of 1861) the following amounts were grown, namely: 6,700,000 bushels of barley; 5,000,000 of wheat; 1,500,000 of oats; 1,500,000 of potatoes; 500,000 of maize; 65,000 of beans; 55,000 of peas; 55,000 of sweet potatoes; 50,000 of buckwheat, and 40,000 of rye, making an aggregate of 14,- 470,000 bushels — an average of twenty-four bushels to the acre, and, estimating the population of the state at 400,000, an average of thirty-eight bushels to the person. I purposely omit the consideration of all articles not enumerated in the list, either because we have no statistics, or because the inser- tion would serve rather to confuse than to instruct. We grow very few roots of the turnip kind as food for cattle. Examining, then, the amounts of the crops above mentionf^. If larger cuttings cannot be had, small ones, half an inch thick and two feet long, are taken, and only an inch or two is left above-ground. If the cuttings are of the largest size, the fence is good in the second year; if small, four or five years may be required to make a tight fence. Twigs and poles are woven horizontally through the hedge. In the course of eight or ten years, the willows grow to be trees, with trunks five or six inches in diameter, and with dense tops from fifteen to thirty feet high. They thus not only shut out trespassing animals, but furnish a large amount of firewood, an item of no small importance in the woodless plains of the south, and throw a pleasant shade over the roads which they line. The willow- fence requires frequent irrigation, for its growth will usually depend upon the amount of water supplied to it. The cactus was used extensively for fences at the old mis- sions, and some fields are still enclosed with it. The plant is merely thrown upon the ground, where it takes root, no matter AGKICULTURE. 1G7 how dry or barren the soil, and grows up in a dense mass of thick leaves, six feet high and from five to ten feet wide. It is covered with thorns, and is feared by all large animals, but spermophiles and gophers are fond of burrowing imder it, for it protects them against their enemies, and its leaves fur- nish them with food. Several machines have been made to cut ditches through the tules, and throw the dirt up as an embankment on one side, but none of them have been very successful ; and the spade is stil] considered the best instrument for making fences in the tules. § 135. Barley. — ^The soil and climate of California appear to be particularly favorable to the growth of barley, which forms a larger proportion of agricultural produce here than in any other part of the world. It is a hardy grain, preferring a sandy or gravelly soil, and dry weather. Three kinds are grown in California — the common, the ^Nepaul, and the chevalier. Only a few acres of the Nepaul have been raised, as an experiment ; the chevalier is cultivated to a small extent, and chiefly for pearl-barley, of which a little is made in the country. The yield of the chevalier is from ten to twenty per cent, less than that of the common barley. The sowing commences with the first heavy rain, which comes in some years as early as the first of November, and continues to the first of April. The ground used for small grain bakes hard during the heat and drought of summer and autumn ; and ploughing is not possible until the rain comes, and rain enough to wet the earth thoroughly, at least six inches deep. The ploughs are then set to work immediately, running from four to eight inches deep. One ploughing is usually considered sufficient. The grain is sown according to convenience, soon after the ploughhig, or after the lapse of weeks, and is immediately harrowed in. The amount of seetl sown to the acre varies from a bushel and a half to two bush- els. The sowing is usually done broadcast, but some fiirmers prefer the drill. Early sowing gives the best yield, if the winter 108 EESOITECES OF CALIFOE XIA. rains be light ; but when the rains are abundant, the late-sown fields are the best. There is always danger that small grain in California, if sown early, will get more rain than it wants. The same barley is sown early and late ; our farmers do not know any thing of " winter barley" as distinct from " spring barley" — a division fomiliar in the Atlantic states. The harvest precedes that of wheat ; commencing in the Sac- ramento Basin early in June, and in the coast valleys late in the same month. The grain is all cut with reaping-machines, and is never housed, but is threshed on the field, with or with- out stacking. Sometimes it is bound ; frequently it is gath- ered in a tight wagon-bed, and hauled into a pile in the centre of the field, where it remains until the threshing-machine can come. The rarity of rain from June to October renders this course pretty safe; though it has happened, on one or two occasions during the last ten years, that grain in the field has been injured by September rains. The same land is cultivated year after year in barley ; and there has been very little, if any, decrease in crops during the last ten years. When men are hired to plough and sow by the job, they charge three dollars per acre ; reaping and binding cost two dollars per acre ; threshing costs from one-twelfth to one-tenth of the grain, and sacks holding one hundred pounds cost fif- teen cents apiece. The common yield is from thirty to thirty- five bushels per acre, and fifty per cent, more than the average barley-crop in the Eastern states. In 1856, according to the reports of the county assessors, the average yield of barley in Alameda county was 45 bushels ; in Sonoma, 39 ; in Marin, 39 in Sacramento, 26 ; in Amador, 34 ; in Santa Cruz, 30. In 1857 according to the same authorities, the average yield in Alame da was 40 bushels; Sonoma, 25; Marin, 39; Sacramento, 24 Amador, 25 ; and Santa Cruz, 30. In 1859, Alameda reported an average of 29 bushels ; Contra Costa, 30 ; Napa, 25 ; San Joaquin, 17; Sonoma, 40; Santa Cruz, 30; Yolo, 10; Sacra- mento, 25. In 1860, the assessors' reports show an average of 30 bushels for Alameda, 40 for Butte, 40 for Amador, 35 AGRICULTURE. 169 for Calaveras, 40 for Fresno, 45 for Marin, 40 for Los Angeles, 20 for Mendocino, 31 for Merced, 33 for Monterey, 28 for Ne- vada, 17 for Sacramento, 20 for San Joaqnin, 21 for Santa Clara, 30 for Santa Cruz, 16 for Shasta, 60 for Sonoma, 60 for Yolo, and 40 for Yuba. Many of these figures are merely guessed at by the asses- sors, who, however, are compelled to travel all over their re- spective counties, and converse with all the farmers. Their conjectures, therefore, are worthy of respectful consideration. But an average of sixty bushels per acre for a whole county looks almost too large to be believed unless supported by some special authentication more than we have. Nevertheless, crops of sixty bushels to the acre are not rare. In 1853, a field of one hundred acres in the valley of the Pajaro produced ninety thousand bushels, and one acre of it yielded one hundred and forty-nine bushels ! It was grown by J. B. Hill ; was men- tioned as undoubtedly true by the assessor of Monterey coun- ty in his official report ; and a prize was granted by an agri- cultural society for the crop. The field which took the prize of the State Agricultural Society, in 1859, yielded sixty-seven bushels to the acre. The field was a large one, and ten acres (a fair sample of the wliole) were measured. The crop which takes that prize is not necessarily the largest crop in the state, but only the largest among those ofi*ered for competition. No doubt, many laiger crops were harvested in 1857. In 1859, ninety bushels of Nepaul barley were grown to the acre by Mr. Burrell, in Santa Cruz county, but in a small field. There is probably no part of the world where volunteer crops do so well as in California, and barley seems to produce better on the volunteer system than any other grain. Volun- teer crops are those grown from the seed which falls out in harvesting; there is, therefore, no sowing or planting. Some- times the land is ploughed and harrowed ; sometimes it is left untouched. Large amounts of volunteer barley are grown every year, and sometimes the yield is excellent. One case is reported of a field in Yolo county which produced five siicces- 8 170 KESOUECES OF CALIFORNIA. sive volunteer crops of barley, the last and least crop araount- ing to thirty bushels per acre ! In 1860, the largest barley counties of the state were — Yolo, which produced 1,541,640 bushels; San Joaquin, 912,500 ; Al- ameda, 630,750 ; Contra Costa, 350,000 ; Sacramento, 300,683 ; Santa Clara, 300,000 ; Yuba, 243,761 ; Butte, 241, 340 ; Santa Cruz, 212,000; and Nevada, 207,000. § 136. IVyieat. — Many kinds of wheat are cultivated here, of which the main are Chile, Australian, Odessa or Old Cali- fornian, Ked Mediterranean, Sonora, Oregon White, Bald, and Egyptian. The general division of wheat into " winter" and *' spring," common in the wheat-growing districts of the East- ern states, is unknown. All our wheat may be set down as spring wheat. When winter wheat is brought here from abroad, it does not thrive the first year ; but in the second year, having been converted into spring wheat and acclimated, it yields well. The Chile gives general satisfaction, and is more cultivated than any of the others. The Australian has a tendency to smut, but this is corrected with blue vitriol. These two form three-fourths of the crop ; the other fourth is made up chiefly of Mediterranean and Sonora. The Egyptian yields largely, but has little gluten, and is fit only for coarse bread or maccaroui. All the acclimated wheat of the state is w^hite ; though imported red seed shows its color the first year, but in the second year it loses its redness. The qualities in which the best wheat excels are glutinous- ness or strength, flintiness or dryness, whiteness of color, thin- ness of skin, cleanness, plumpness and size of berry, and Av eight. The value of wheat depends, to a great extent, upon its strength. In this point lies its chief diflerence from potatoes, which always do and must occupy an inferior place upon our tables. Much gluten in flour renders the dough tough, makes handsome bread, with the air-bubbles in it small and uniform in size, and retains moisture, so that the bread will weigh much in proportion to the flour used ; while if the amount of AGRICULTURE. 171 gluten be small, the grain of the bread will be uneven, the dough will give way in places, allowing the formation of large cavities, and less moisture will be retained. The Avheat of dif- ferent countries varies greatly in glutinousness, and California occupies a very high position. Our wheat is far more glutin- ous than that of any other North American state, and, although I have no precise information, I am inclined to believe that we have a like superiority in this respect over European countries. The consequence is, that our wheat is now in demand in IsTew York to mix with their weak grain, so that a tolerably strong- flour may be made. But the wheat of California is not all equally glutinous ; some of it is much weaker than other. The most glutinous is that grown in Santa Clara valley ; the southeastern part of San Ma- teo county ; the southern part of Alameda county ; and Diablo, San Ramon, and Suisun valleys. That of Santa Rosa, Pajaro, Salinas, Petaluma, and Sonoma, is considerably inferior in glu- tinousness, but is better than that of the Sacramento, San Joa- quin, and Napa valleys, the vicinity of Half-Moon Bay, and Alameda opposite the Golden Gate. The strongly glutinous is about one-third of the crop of the state. It is not known wdiy the wheat in one district is more glutinous than in another. None of that grown very near the coast is strongly glutinous ; so the moisture seems to be injurious. Napa wheat is inferior in glutinousness to that of Sonoma, though farther from the coast, and more free from ocean-fogs, but the soil of Napa is much moister. In Oregon and Washington, where the climate is very moist, the wheat is as weak as at Half-Moon Bay. In the Mississippi valley, where a great amount of rain falls, the wheat is also weak ; and just in the Gallego and Haxall district, if report be true, the rain-fall is less than in any wheat-district east of the Alleghanies. And yet in the Sacramento and San Joaquin valleys, which are among the driest parts of California, the wheat is very weak. This is accounted for — by those adopting the theory that glutinousness depends entirely upon the ch- 172 RESOURCES OF CALIFOENIA. mate — hj saying that those valleys are visited, while the grain is in the milk, by weather so hot that the berries are burned, and are prevented from attaining their perfect development. It would be well if this matter were thoroughly studied, for it is one of much importance to the merchant and ship-owner, as well as to the farmer, the baker, and the consumer. The wheat grown on the clayey loam about Alviso is not so glutinous as that produced on the sandy loam about Santa Clara and the gravelly clay in other parts of the valley. It is worthy of remark that the soil of the Putah and Cache valleys, tributary to the Sacramento, differs in no noteworthy particu- lar from the soil in Suisun, Diablo, and San Ramon, which lat- ter yield strong while the former produce weak wheat. It has been observed that during the last three years the wheat of a large farm in San Mateo county, said to be the best cultivated in the state, has been gradually decreasing in strength. It is not known whether the change is caused by a difference in the seasons, or by a progressive exhaustion of the soil. So far as observations have been made in California, the amount of glu- ten is not affected by early or late sowing, thorough or careless cultivation, largeness or smallness of the yield, or cleanness of the crop. In fiintiness or dryness, Californian wheat has no superior, and no equal save in the Chilean. It may be stored in bulk, or it may be thrown into the hold of a ship within two weeks after harvest, and then sent twice through the tropics, and there is no danger that it will heat or sweat. The same may be said of its flour. No wheat or flour from the Atlantic states is near it in this respect. In August, 1860, J. B. Fris- bie loaded a vessel at Vallejo with wheat taken from the har- vest-field — it had never been inside of a house, but had lain upon the ground for several weeks after threshing — and that cargo of wheat, when discharged at Liverpool, was as sweet and clear from mustiness, mould, sprouting, or fermentation, as it was when harvested. The Atlantic flour, when kiln-dried and pressed, does not keep like ours as it comes from the mill, AGKICULTUEE. 173 after having gone there fresh from the threshing-machine and the harvest-field. The flour made from flinty wheat is peculiarly suited for shipment to tropical countries, where the moister flour soon ferments and sours. These are excellent markets, for they are certain, they pay well, and there is little competition. Most of the flour now exported to the West Indian islands and the Malaysian archipelago is of the Gallego and Haxall brands, which, because of their dryness and strength, are worth from twenty to fifty per cent, more in the market than other flour. California may not be able to supply the West Indian islands, but she certainly has peculiar advantages for supplying the tropical islands and shores of the Pacific. The flintiness of our wheat is undoubtedly owing to the dryness of the climate, and it is about the same in all the wheat-growing districts of the state. There is no noteworthy difierence in this respect between that of the Sacramento valley and that grown on the immediate coast. It is all so dry as to keep well in any cli- mate. Millers in New York and Liverpool make some objec- tion to our wheat, that it is too hard for their millstones ; but this is their misfortune, not our fault. The difiiculty is reme- died by moistening the wheat before grinding. Most of the wheat of this state is white, but it is not equal in whiteness to that of the Genesee valley, Oregon, Washing- ton, and some other districts of the United States ; yet is supe- rior to the wheat of England and of most European countries. The fogs give a dark color to the wheat grown at Half-Moon Bay, in the Pajaro and Petal uma valleys, and on the Santa Kosa plain ; but in the other districts a uniform whiteness pre- ^ vails. Our wheat generally has a thin skin, and does not make much bran ; but in the same districts where the skin is dark- ened by the fogs, there also it is thick. Most of the Californian wheat is not well cleaned. It is sent to the market containing oats, barley, chess, alfalfa-seed, and dirt ; and when shipped to New York, must usually be 174 RESOUKCES OF CALIFOKNIA. cleaned there before it can be ground. Our farmers, however, are gradually becoming more careful in cleaning their wheat. In the plumpness and size of the berry, our wheat compares well with that of Europe and the Atlantic states, but can per- haps claim no decided superiority. Comparing the diiferent districts of the state with one another on this point, Suscol probably deserves the first place, and Napa the next. In the Sacramento and San Joaquin valleys, the wheat is often shriv- elled by hot winds, which blow for three or four successive days while the grain is in the milk, and seem to blast it. Great diiferences are observed, however, according to the season. The weight of Californian wheat is usually sixty pounds j)er bushel, seldom less — frequently sixty-two, and sometimes sixty- five ; thus entithng our state to a high position in that respect. The average yield of Californian wheat-fields is from twenty to twenty-five bushels per acre, which is about thirty-three per cent, more than in the states on the Atlantic slope. An old Spanish book of records, of the mission of San Diego, states that, in 1*778, twelve fanegas (a fanega is about two bushels) of w^heat were sown, and three hundred and fifty fanegas were harvested — an increase of thirty-fold. The next year, sixteen fanegas were sown, and the yield was one hundred and sixty fanegas. In 1780, twenty-four fanegas were sown, and eight hundred harvested — an increase of thirty-three-fold. San Die- go is far inferior for wheat-growing to the coast valleys about San Francisco Bay; and previous to the coming of the Ameri- cans the ground was not ploughed, but only scratched, and the limb of a tree was used for a harrow. Colton, in his "Three Years m CaKfornia" (page 442), states that while the priests still had sole control of the missions and mission-lands, previous to 1833, the mayordomo or steward of the Mission of San Jose harvested 4,300 fanegas of wheat from 40 fanegas of seed ; and at the next harvest he had a volunteer crop of 2,600 fanegas on the same land. The first year, ac- cording to this report, the increase was 107-fold, and the next year 65 -fold. At the Mission of Soledad, according to the AGRICULTURE. 17* same author (page 445), 1,700 fanegas were harvested from 19 sown — an increase of 89-fold; and in 1827, an increase of 58- fold was obtained at San Luis Obispo by scratching the seed in with a harrow upon land unploughed, and not even touched by the thing called a plough in those days. Not less than half a fanega is sown to the acre ; so we may suppose that the fig- ures which mdicate the increase of the crop over the seed also indicate the number of bushels to the acre. Now, a tenfold increase is considered a fair crop. Crops of 80 bushels to the acre have often been grown in California. Mr. Hill harvested 82^ bushels from an acre in Pajaro valley in 1853, and obtained 660 bushels from 10 acres. In 1851, Mr. P. M. Scooffy har- vested 88 bushels; and Mr. N. Carriger 80 bushels in Sonoma valley. In 1853, J. M. Horner harvested 1,000 acres of wheat near the Mission of San Jose, with an average of 40 bushels, some of it producing 60 bushels to the acre. The next year he had 2,000 acres, with an average of 40 bushels. Large fields of wheat in Eel River valley, according to the report of the assessor of Humboldt county, averaged 73 bushels to the acre in 1857. In the best wheat districts of the Mississippi valley, the farmers generally believe, or did believe a few years ago, that not more than 45 bushels of wheat ever had been or ever could be grown upon an acre ; and when, on a visit from California, I spoke to experienced and intelligent men among them of 60 bushels, I was told that not more than 50 bushels could possi- bly stand upon the ground. In 1856, the average wheat-crop per acre in California, according to the county assessors' reports, was — 25 bushels in Amador and Santa Cruz counties, 30 in Marin, 28 in San Francisco, 19 in Sacramento, 20 in San Joa- quin, 15 in Sonoma, and 28 m Tuolumne. The next year it was 35 in Amador, 40 in Del Norte, 20 in Alameda, Santa Cruz, San Joaquin, and Tuolumne, 19 in Sacramento, and 30 in Sonoma. In 1859, the average was 30 bushels in San Ma- teo, Santa Cruz, Siskiyou, Sonoma, and Yuba, 32 in Butte, 25 in Napa and Santa Clara, 20 in Contra Costa and Solano, 15 in 17(5 KESOURCES OF CALIFORNIA. San Joaquin, and 14 in Sacramento. In 1860, the reported average was 45 bushels in San Luis Obispo, 35 in Yolo and Calaveras, 34 in Placer, 30 in Sonoma, Stanislaus, Yuba, and Amador, 27 in Santa Cruz, 26 in Fresno and Tulare, 25 in Te- hama, Butte, Humboldt, and Napa, 24 in Nevada, 20 in San Diego, Santa Clara, and Shasta, 18 in San Joaquin, and 15 in Sacramento. In 1855, the worst year for wheat w^e have ever known in California, when both smut and rust raged from Siskiyou to San Diego, the average crop of the state was put down as 15 bushels per acre. Of 12,233 acres sown in Sonoma county, only 3,500 were harvested; and of 2,490 sown in Marin, all but 462 went untouched by the reaper. In Ohio, the average wheat-crop is about sixteen bushels per acre; and in England, with all their manuring and careful ploughing, twenty-one bushels. In California, no manure is applied ; the soil is ploughed but once in most fields, and there is little rest for the land by rotation of crops. It is a singular fact that where wheat is sown under oak- trees, the stalks are usually thicker and taller, and the grain more abundant, than in other places. This may be owing to the facts that the trees protect the ground under them from the frost, and also retain the moisture; and that while the country w^as in the hands of the Mexicans, the cattle had pos- session of the valleys, and, collecting under the trees in the summer-time, their manure enriched tiie soil there. The roots of the oak-trees in the valleys do not run along the surface of the ground, but go deeper for moisture, and thus the plough can run up to the trunk, and put aU the land in order for grain. The principal wheat-growing counties in the state are San' Joaquin, which in 1860 produced 895,000 bushels; Napa, with 652,000 ; Yolo, with 459,000 ; Alameda, with 440,000 ; Santa Clara, with 400,000 ; Yuba, with 223,000 ; Santa Cruz, with 243,000 ; Sonoma, with 275,000 ; and Contra Costa, with 450,000. It is almost impossible that there should ever be an entire AGllICULTUEE. 177 failure of the wheat-crop in California, unless the rain should completely fail. After wet winters, the dry lands and hills will produce the best crops ; in seasons of light rain-fall, tlhi low, moist lands will take the lead. There are so many soils and so many climates in the state, that some must be favor- able. There is no danger that the grain, when nearly ripe, will be beaten down by the hail, as has happened in Europe and the Atlantic states. On only one occasion, within my knowledge or reading, has it happened that the grain has been " lodged" or beaten down by rain, and that was at Suscol and Napa in 1860; and the damage then was slight, for most of the grain recovered, and all of it, if I remember rightly, was reaped by macliines. Wheat is sown from the first of November to the first of April. The most certain crops are those sown early ; the largest are those sown late in favorable years. If the amount of rain is small or moderate, the earliest-sown fields are the best ; but if the spring be wet, the early-sown fields are sur- passed by those sown about the first of February. Wheat is usually sown after barley and oats. The best farmers prefer to sow between New-Year's Day and the middle of February. Most of the sowing is done broadcast, but drills are used to a considerable extent. One ploughing is, by most farmers, con- sidered sufliicient. The harvest comes from the middle of June to the middle of July. The expenses of sowing, harvesting, and threshing, are the same as with barley. § 137. Oats. — The principal varieties of oats cultivated in California are the Australian, English, Bare, Feather, and Tuck- er. The Bare and Tucker oats thrive best on a heavy soil ; the Feather oat prefers a sandy loam. The indigenous wild oat of California is never cultivated ; for, although it produces large and tall stalks, they do not contain so much weight or bear so much grain as the domesticated oat. The average crop is from 30 to 40 bushels to the acre, 30 per cent, greater than in the Atlantic states. The Crescent City Herald re- ported in October, 1857, that Rigg and Reid, in Del Norte 8* 178 KESOUPwCES OF CALIFORNIA. county, had grown 125 bushels of oats to tlie acre; and that John A. Brown, of Crescent City, had a crop of 15^71 bushels to the acre. According to the assessors' returns, the averaE^e crop per acre of 1860 was — 50 bushels in Alameda and Yuba counties; 40 in Butte, Placer, and Santa Cruz; 35 in Napa; 30 in Amador, Sacramento, and' Yolo ; 28 in Humboldt ; 25 in San Joaquin ; and 20 in Klamath, Santa Clara, and Sonoma. The largest oat-growing counties in the state are — Alame- da, which in 1861 produced 449,000 bushels; Contra Costa, 300,000; Santa Cruz, 262,000; Sonoma, 187,000 , and Marin, 174,000. § 138. JIaize. — Maize can be grown to advantage in only a few places in California. Most of the land is too dry and the summer nights too cool for it. The principal maize districts are in the valleys of the upper coast, from Russian River to Humboldt Bay; in Yuba county, upon the moist bottom-lands of the Sacramento River ; and at the Monte, in Los Angeles county, w^here the San Gabriel River sinks and fills the plain with moisture. Sixty bushels to the acre is considered a large crop; the average is not over thirty. Corn can be grov/n wherever the land can be irrigated, but this is a troublesome and expensive mode of cultivation, though it is not uncommon in gardens near San FransiscO. Green maize, grown in the open air, is in the market from June to September. The cultivation of rye and buckwheat differs little from that of the same grains in the Eastern states. § 139. Potatoes. — The potato thrives wonderfully in a few places in Cahfornia, particularly at Bodega, Tomales, and in Pajaro valley. The average produce per acre is perhaps not laro-er than in Ohio or England, but the tubers are larger in size and smoother in skin. The average size of those sold in the San Francisco market is probably fifty if not one hundred per cent larger than of those sold in New York. Potatoes six inches long by three niches through, and weighing a pound, are not uncommon ; many have been seen to weigh four pounds ; and one grew to weigh seven pounds. I saw a clus- AGRICULTURE. 179 ter that had grown together, eight inches long, six wide, and four deep, that weighed eight pounds. The soil at Bodega and Tomales, the chief potato district, is a light, sandy loam, and the mists from the ocean supply the ahiiiidant moisture which the plant loves. In 1860, k>onoma produced 314,000 bushels, Sacramento 263,000, Marin 240,000, and Alameda 73,000. The potato district of Sacramento coun- ty is on the banks of the sloughs of the Sacramento River, near its junction with the San Joaquin. The soil is a very light, warm, rich loam, and the vegetables grown there are among the earliest in the market. According to the assessors' reports, the average crop of Sacramento county in 1860 was 390 bushels l^er acre; of Sonoma county, 100 bushels; and of Marin, 80. The Californian potatoes are mealy, sound, and palatable. The potato-disease has never made its appearance in this state. The immediate coast, at least north of Point Conception, is too cold for the sweet potato, which thrives, however, in the Sacramento valley, especially in the low land about the head of Suisun Bay. The true sweet potato has grown here to weigh fifteen pounds — much larger than any I have ever seen in the states east of the Mississippi. The flavor is not equal to those grown at the East. They lack the mealiness and deli- cate taste which make the Eastern sweet potato so palatable in its season. § 140. Hay.— In 1860, California had 150,000 head of horses and 1,100,000 head of neat cattle, and cut 200,000 tons of hay, or one ton for six head of large stock. In 1849, Ohio had 463,000 horses and 1,350,000 cattle, and cut 1,500,000 tons of hay, or five tons for six head of stock. Ohio, therefore, cuts five times as much hay, in proportion to the number of her horses and cattle, as does California ; and if we suppose that she exports one-fourth of her hay to the slave states, she still makes three times as much in proportion for home use as this state. The cause is, that there every horse and cow must have hay throughout the w^inter, and many of them through the summer ; while here very few cattle are fed with hay at any 180 EESOUECES OF CALIFORNIA. season of the year, and horses not employed are usually turned out into the open plain. The hay of Ohio is cut in cultivated fields, from tame grasses ; that of California is made of wild oats and indigenous grasses, which are grown in the open valleys. The haying season comes about the first of May. The old adage, that "you must make hay while the sun shines," does not apply in California, for here the sun shines all the time, and the haymaker has ordinarily no fear of rain. It happened, however, in 1860, that a considerable amount of hay was spoilt by the late rains in June. The whole process of haymaking in California is managed by machinery. It is cut with the ma- chine-mower, raked together with horse-rakes into cocks or windrows, and finally the cocks are hauled together on hay- sleds which load themselves by slipping under the cocks. The hay is not turned by hand, nor is the field raked by hand. The hand must be used, however, when wagons are to be loaded or stacks built. Hay is usually cured in the cock or windrow. It is not necessary to turn it by hand, as is cus- tomary in the Eastern states. One turning and one day in the sun are enough, w^hen it is raked together and is ready for the stack or the mow. In Ohio, a good field of timothy will yield four tons of hay to the acre ; in California, the wild oat stands so thick in a few places as to yield as much, but the average crop is not over a ton to the acre. The principal hay counties of the state are — San Joaquin, which in 1860 made 37,000 tons; Santa Clara and Yolo, 18,000 each; Sonoma, 17,000; Yuba, 14,000; Sac- ramento, 13,000 ; and Contra Costa, 11,000. Very little maize- fodder is used in the state. Tame grasses occupy, at the present time, a very small place in the agriculture of California. Not one-tenth of the farms in the state have an acre of cultivated pasture ; and even in the largest farms, containing from three hundred to a thou- sand acres under plough, it is rare to find a field of timothy, clover, or alfalfa. The last-mentioned will probably become AGEICULTUEE. 181 the principal grass grown in the state, since it is peculiarly fitted to thrive in a climate and soil so dry as ours. § 141. Tobacco^ Cotton^ Rice. — California produces tobac- co of a fine quality, but the amount grown is small ; and the experience of its cultivation is too brief to furnish much infor- mation. It requires a moist soil, and most of the attempts to cultivate it in dry places in the Sacramento valley and in the vicinity of Los Angeles have failed. The best crops have been ^rown near the coast, north of San Pablo Bay and about the head of Suisun Bay. The tobacco-plant has been converted into a perennial at San Francisco ; one specimen of it growing up eight or ten feet high, like a tree. A little cotton of a good quality has been grown, but I think its cultivation can never be extensive. The cotton states have three times as much rain as California, and I presume that only our moistest lands could produce a good crop of it — such, for instance, as the tule-lands in the valley of the San Joaquin. The question whether rice can be cultivated in the tule-lands has been much discussed, but is not yet decided, though it is the general opinion that some of the tule-lands will produce large and profitable crops. § 142. Hop. — The hop growls luxuriantly and produces abun- dantly in California ; and indeed there is good reason to doubt whether any country has a climate and soil more favorable to it than ours. We have no heavy dews or showers in summer to w^ash ofi* the dust which contains the strength of the flow- ers, or to cover the plant Avith blight. The failures of crops, from these causes, so frequent in England and the Atlantic states, w^ould never occur here. Not only is the crop certain, but it can be cured here with more ease and in better condi- tion than in other countries. The moisture of the air in Eng- land compels the hop-growers to dry the flowers in the sun or in kilns ; and if a rain fixll upon them while drying, they are ruined : and they are injured by both the sun and kiln-drying. In California, they may be dried in the open air, under sheds; 182 EESOTJKCES OF CALIFOENIA. aiad thus prepared, they will be superior to any of the Euro- pean hops. The Chinese sugar-cane grows luxuriantly in this state, but it is not extensively cultivated. Flax, hemp, and the basket-willow, are not cultivated, or in patches so small as to be unworthy of notice. § 143. Kitchen Vegetables. — The vegetables for the kitchen — such as cabbage, cauliflower, beets, parsnips, carrots, rad- ishes, onions, melons, squashes, pumpkins, green j^eas, string- beans, tomatoes, asparagus, rhubarb, okra, cucumbers, lettuce, garden-egg, and so forth — thrive in Cahfornia, many of them beyond example elsewhere. Cabbages weighing fifteen pounds are wonders in the New York market ; in San Francisco they are common. Whole fields of cabbage-heads, weighing twenty pounds each, have been grown ; and hard, sohd heads, with no loose leaves, weighing forty -five and fifty-three pounds each, are on record. One cabbage, which did not make a head, grew to be seven feet wide, throwing out leaves three and a half feet long on each side. In many cases the cabbage has been converted into a perennial, evergreen, tree-like plant, by IDreventing it from going to seed. Several of these are now growing in the state, with stalks from two to six feet high, and a foliage that grows through winter and summer. The largest squash or soft-skin pumpkin produced in Cali- fornia weighed two hundred and sixty pounds, and the vine which bore it had several others weighing over one hundred pounds each; the total weight of its fruit being more than eight hundred pounds ! Elsewhere, sixty pounds is a very large pumpkin or squash ; and there is scarcely a record in the At- lantic states of a greater weight than one hundred pounds, which has been frequently surpassed here. In 1857, one squash-vine on the ranch of James Simmons, in Yuba county, produced one hundred and thirty squashes, weighing in all twenty-six hundred and four pounds ! In the same year, J. Q. A. Ballon, at San Jose, grew two squashes, weighing two hun- ired and ten and two hundred and four pounds respectively. AGP.ICULTUPvE. 183 The largest Califomian onion weighed forty-seven ounces avoirdupois, and measured twenty-two inches in circumference. Our onions generally excel those of the Eastern states in size and weight. Our largest red beet weighed one hundred and eighteen pounds — was five feet long, and a foot in diameter. It was three years old. The first year it grew to weigh forty-eight pounds, and because of its large size was reserved for seed ; but it disappointed its owner, and, instead of producing seed the next year, merely kept on growing, and reached the size of eighty-six pounds; and the following year got to a hundred and eighteen. Such beets can be grown in abundance. A beet of twenty pounds is a wonder in Xew York or London ; here it is too common to attract more than a glance. Beets fre- quently are three feet long, so that it requires no little trouble to dig them out. Our largest common white turnip weighed, I believe, twenty- six pounds ; our largest carrot, ten pounds ; our largest water- melon, sixty-five pounds. Our largest tomato measured twenty-six inches in circum- ference. Our kitchen vegetables, grown in the open air, are in the market during a greater part of the year than in any state east of the Mississippi. We have cabbage, cauliflower, lettuce, turnips, beets, carrots, parsnips, radishes, horseradish, celery, green onions, leeks, salsify, and parsley, throughout the year; green peas, string-beans, water-melons, cantaloupes, and nut- meg-melons, from June to November inclusive ; tomatoes from May to October; garden-eggs, green okra, Lima-beans, and Califomian sweet potatoes, from July to September ; aspara- gus from March to June ; and rhubarb from April to July — the months being meant inclusively in every instance. These seasons for the different species of vegetables are, on an aver- age, twice as long as the seasons on the Atlantic slope of the continent in the same latitude. Our tables are thus supplied with a great variety of fresh and wholesome -vegetables 184 EESOUKCES OF CALIFOKNIA. throughout the year. Another advantage of our climate is, that garden vegetables may be left in the ground all winter. Potatoes are sometimes not dug until the first of January, and turnips and beets are usually left in their beds until they are to be sent to market ; there is never enough cold to freeze them. Potatoes are never buried, but after they are dug are piled up in bags under a shed, or are placed in a storehouse. The cabbage likes a moist air and soil, and thrives best along the coast, from Bodega to Santa Cruz. The melons and toma- toes like a warm climate, and thrive best in the Sacramento valley — and Putah valley, which is tributary to it — where many of the early vegetables for the San Francisco market are grown. § 144. Fruit. — As a fruit-growing state, California takes a high position. In this particular, as in so many others, her climate gives her great advantages. In no part of the world do fruit-trees grow so rapidly, bear so early, so regularly, and so abundantly, and produce fruit of such large size. Nor is there any other country where so great a variety of fruit can be produced in high excellence. In the matter of flavor, our apples, peaches, and strawberries, or most of them, are infe- rior to Eastern fruit ; in the flavor of other species we are at least equal to other countries. The pear, the plum, the apri- cot, the grape, and the olive, are peculiarly thrifty, healthy, and productive, as compared with the same kinds of fruit else- where. The Californian orchards are trained low, the lower limbs being within a foot or at most two feet of the ground. All kinds of fruit-trees are trained on the same principle. Men, therefore, do not walk under the trees in an orchard, or climb after the fruit. It would be as absurd to try to walk under or to climb a bearing apple-tree in California as to walk under or climb a gooseberry-bush. One fruit-tree in a hundred may be trained high, not more. The advantages of low training are, that the trees bear fruit earlier — a matter of the greatest im- portance in CaUfornia, where the interest of money is so high, AGRICULTURE. 1^5 and the price of fruit rapidly falling from year to year ; the trunk is shaded, and protected against the disease called the sun-scald; the earth about the roots is kept moist; and the trees are protected against the wind. The trees are planted from one-sixth to one-half nearer to- gether in the orchards than in the Eastern states. This is an additional protection against sun and wind. The ground is ploughed several times every summer, and kept clean ; whereas in the Eastern orchards it is common to sow grass or cultivate vegetables. Our apple-trees are free from the borers after the first year, and our plum and cherry trees from the curculio, though the plum suffers from the aphis or louse. Fruit-trees in California are generally as large at two years old as they are in New York at three and four years. The in- stances of unusually rapid growth here are without parallel elsewhere. Cherry-trees have grown to be fourteen feet high in one year ; pear-trees ten feet high ; peach-trees to have trunks from two to three inches in diameter. These were all from buds on yearling stocks, and were well provided with branches — not trimmed to gain height. These specimens of rapid growth were observed on an island near the junction of the Sacramento and San Joaquin Rivers. At Petaluma, a cherry-tree two years old from the graft, and three from the seed, had a trunk seven inches and three-quarters round ; a plum-tree, three years from the seed, was eleven feet high, and had a trunk seven inches in circumference ; and a peach-tree, one year from the bud, was eight feet high and eight and a half inches round. Mr. E. B. Crocker, of Sacramento, wrote thus in December, 1858: "In January, 1855, I planted a small almond-tree, with a stem little larger than a goosequill, and which I cut down within a few inches of the ground. It is now a tree twenty feet high, sixteen feet through the top, with branches starting from the surface of the earth. The body below the branches is twenty-four inches in circumference A Glout Morceau dwarf pear-tree, planted in 1855, when it had grown one year 186 RESOURCES OF CALIFORNIA. from the bud, is now ten feet high, four feet through the top, and measures ten inches round the body at the ground, branch- ing about one foot from the surflice. A Beurre Diel dwarf, phmted in^ January, 1856, is now seven feet Ingh, three feet through the top, and ten inches in circumference at the ground. A dwarf May Duke cherry, planted in 1856, is now thirteen feet high, and thirteen and a half inches in circumference at the ground. An Old Mixon peach, planted in 1855, and cut down within a few inches of the ground, is now twenty feet high, twenty-two feet through the top, and the trunk twenty- eight inches in circumference. A seedling peach, seed planted in January, 1858, is now eight feet high and well branched, and the trunk four and a half inches in circumference at the ground. The growth of trees, vines, and shrubs, is about double that of similar kinds on the rich prairie-soils of Northern Indiana." In 1858, a sprig of a peach-tree, a foot long, was stuck into the ground on the Bay-state ranch ; the next year it bore fruit. It may be set down as a general rule that, previous to the time of bearing fruit, trees in California make twice as much wood in a year as they do in the middle states. In Alameda county, plum-trees have grown twelve feet in one year from the bud. The trees commence to bear fruit at about half the age at which they bear in the Atlantic states. An apple-orchard in New York begins to bear in its fifth or sixth year ; in Califor- nia, in its second or third. The variety of climates, and the freedom from frosts, severe cold, and furious storms, protect us against a failure of the fruit-crop. Our apples, pears, apricots, and plums, are larger than the same varieties usually are elsewhere; other fruits are about the same in size. § 145. A2Jples. — The Spanish Californians had a few apple- trees, but they were seedlings of a poor class. The first good apples were imported from Oregon in 1849 ; but the varieties were few, and the trees did not thrive. Either the stock was AGEICFLTTJEE. 187 not the best, or the change of climate had an injurious influ- ence on them. In 1852, a few trees were imported by way of the isthmus of Panama ; other importations followed very rapidly ; and now the state has millions of trees in nursery, and about eight hundred thousand bearing trees in orchard, inclu- ding two hundred varieties, the best of Europe and the Atlan- tic states, both standard and dwarf trees. Apple-trees are usually planted from twelve to thirty feet apart, fourteen or sixteen being the more common distances. This is much closer together than is customary in the Atlantic states ; the reasons for the denser planting here being to pre- vent injury by the wind, and to keep the earth moist by sha- ding it against the sun. The apple-tree comes into bearing in the third year in California, about two years earlier than in the Eastern states. It also grows more rapidly, a yearling tree here being as large as a two-year-old tree in Ohio. Grafts on yearling stocks have been known to grow six and eight feet in a season — twice as long as similar grafts will grovv^ in the mid- dle states. The fruit usually grows larger here than elsewhere. The Gloria Mundl apple, which elsewhere seldom exceeds fourteen ounces in weight, in California frequently reaches twenty ounces, and some have attained the great size of two and even two and a half pounds. The climate seems to have a tendency to ripen apples more thoroughly here than in other states. Those varieties which are grow^n for winter use elsewhere, are here generally con- verted into autumn apples, and only a few will keep to New- Year's Day. A fruit-grower in Alameda has succeeded in keeping several kinds until June. Our list of winter apples is very short, and some years will pass before w^e can in this re- spect equal the middle states. Some varieties have been intro- duced here from Georgia and other Southern states, but we do not yet know how they will succeed. The flavor of our apples is not equal, as a general rule, to that of the apples grown on the Atlantic slope. They are less juicy, and more mealy. Some varieties, however, are better 188 EESOURCES OF CALIFORNIA. here than in the Eastern states. Great variations are observed in different parts of the state ; an apple may be excellent when the tree grows in the hot summer and cold winter high up on the Sierra Nevada ; and be of poor quality if grown in the equable temperature of the coast. The best varieties, so far as ascertained, about the bay of San Francisco, are the Summer Pearmain, Red Astrakhan, Red June, and Early Harvest, for early apples ; the Porter, Graven- stein, and Summer Queen, for late summer apples ; the Bald- win, Roxbury Russet, and Rhode Island Greening, for fall apples; the Golden Russet, the Northern Spy, the Yellow Kewtown Pippin, the White Winter Pearmain, and the Spitz- enberg, for winter apples. The best cider apple is the Smith's Cider. The leading counties in the production of apples are Santa Clara, Sacramento, Alameda, Sonoma, Napa, Marin, Yolo, Yuba, and El Dorado. The trees grow so rapidly and bear so abundantly, that some persons suppose our orchards must be short-lived ; and the old- est American orchard in the state — at the Mission of San Jose — is cited as proof of this theory. That orchard is evidently dying, though only eleven years old ; but its unhealthiness is owing to some influences peculiar to that spot. It has been gradually dying for four or five years, while other orchards six and eight years old are in perfect health. Besides, the fruit- trees of the old missions, many of them thirty years old, are still in excellent health and full bearing, and have not failed at any season during the last score of years to produce a good crop. The indigenous trees in our valleys have a thriftiness of growth and a precocity of development similar to our cul- tivated fruit-trees, and yet have a longevity equal to that of the similar species east of the Mississippi, where the summers are shorter, the winters colder, the annual growth less, and the development of tlie reproductive power later. § 146. Peaches. — ^The peach-tree grows very rapidly, comes into bearing very early, and produces abundantly, in California; AGRICULTURE 189 but nearly all varieties suffer with "the curl," which has given so much trouble during the last two years, that many of the or- chards have been cut down. The varieties most ft-ee from the curl are the Late and Early Crawford, the Late Admirable, and the Smock. In the valleys and near the ocean, the peaches are not equal, either in size or flavor, to the same varieties on the Atlantic slope ; but in the Sierra Nevada they are fully equal to the Eastern fruit. The peach does not thrive in the high winds which prevail about San Francisco Bay. The trees are usually set out in orchard when one year old from the graft or bud ; in the second year after that, they begin to bear. § 147. Pears. — The pear is the most productive and healthy of the fruit-trees of California. It thrives in all parts of the state, and everywhere its fruit is delicate in flavor and large in size. There are pear-trees at San Jose which produce twenty- five hundred pounds or forty bushels each of fruit annually. The pear was more cultivated by the Spanish Californians than any other fruit ; but their varieties were not good, and most of the old trees have been grafted with varieties brought from the Atlantic states during the last eight years. The varieties most prized are the Madeline, Bloodgood, Diane d'ete. Dear- born's Seedling, and Bartlett, for summer pears ; and the Win- ter Nelis, Glout Morceau, Easter Beurre, and Pear d' Albert, for winter. Neither tree nor fruit is troubled by any bug, fire-blight, sun, or rain. § 148. Apricots and Plums. — The apricot thrives well and bears abundantly, especially in the warmer parts of the state. The fruit, however, in some places is much eaten by bugs and bees. The bugs — some of them of the kind commonly called *' Lady-bug," and others similar in appearance and size — eat holes in the apricots before they are ripe ; and the bees, which never break the skin, eat at the hoh^s which the bugs have commenced. The apricot-tree is more healthy than the peach, and produces more abundantly ; and its fruit supplies the place of the peach m many districts. 190 EESOUECES OF CALIFORNIA. The nectarine is affected by the curl, and is not much culti vated. If the cnrculio should not be introduced, the plum will oc cupy a very prominent place in the horticulture of the state. The tree is healthy ; and the fruit is large, finely-flavored, and abundant. The climate is very favorable to drying fruit, and prunes might be made here with a profit. The cherry and the soft-shell almond thrive in all the valleys of the state. The fig-tree is cultivated from Shasta to San Diego, but does not produce abundantly north of latitude 35°. In the vicinity of Los Angeles it is a very thrifty and productive tree. It produces two crops of fruit annually. North of 37° the sec- ond crop is usually killed by the frost or stunted by the cold. The almond and the English walnut both grow Avell and l^roduce abundantly about Los Angeles, but do not thrive so well north of Santa Barbara. The almond suffers, and loses its fruit, with a slight touch of frost. Tlie pomegranate is a healthy and productive bush in Cali- fornia, but its fruit is not profitable. It is cultivated to a small extent in all the large fruit-gardens, § 149. Olives. — For the cultivation of the olive, California has great advantages. The tree is very healthy, and always bears abundantly ; whereas in Italy and Greece, whence most of our olive-oil comes, the crop is frequently destroyed by sum- mer rains, blight, and insects, all of which causes of trouble are unknown here. There it is expected that the crop will fail one year in three, whereas here no failure has ever been known. The number of our olive-trees is small, most of those in bear- ing having been planted half a century ago. Nor is it likely that there will be a rapid increase. The tree does not come into bearing until ten years of age, at least not in Europe ; and although it may live and continue in bearing for five or six centuries, the possibility of a steady income to our remote posterity will not j^ay Californians for investing their money in a business that will yield no income for a decade of years. AGRICULTURE. 101 Most of the bearing olive-trees are in the town of Los An- geles, and at the Missions of San Fernando, San Gabriel, and San Juan Capistrano. The oliv e-tree resembles a willow in the form and color of its bark, the shape and proportions of its trunk and branches, and the size, color, and distribution of its leaves. The trees are grown from cutthigs or shoots, which latter frequently sprout from the large trees near the surface of the ground. A large olive-orchard in full bearing would prove an excellent income, for the fruit and the oil are in demand. § 150. Oranges. — The orange is cultivated in Los Angeles ; and, although the trees now there are covered with insects to such an extent, that most of them bear no fruit, yet I think til ere is reason to hope that the fruit will, at no distant day, be cultivated extensively and profitably. A warmer clime than that of this state is undoubtedly more congenial to the orange than ours ; but in those lands where the climate is warmer, the men are less industrious and intelli- gent. Cultivation, which is the first element in the develop- ment of every species of fruit, is wanting there, while here there is no lack. Not that our cHmate is so cold as to make it doubtful whether we can cultivate the orange in the open air : long experience has settled the fact that the orange-tree will thrive and produce well from Santa Barbara southward. We have no exact information as to the time when the or- ange was introduced into California, nor from what stock the old orange-trees came. Probably tlie first missionaries brought orange-seeds with them from Lower California, that stock hav- ing come from the indigenous trees along the western coast of Mexico. The seeds were planted at various old missions, such as San Diego, San Fernando, San Juan Capistrano, and so forth. The trees grew, were planted out, bore well, received little at- tention or cultivation, and some of them are still standing as monuments to the industry and enterprise of the old priests. There are now, so far as I can learn, about twenty-five hun- dred orange-trees set out in orchard in the state, more than 192 KESO URGES OF CALIFORNIA. two-thirds of them being in the orchard of William Wolfskill, in the town of Los Angeles. About four hundred of the orange-trees in the state are old — from ten to fifty years of age ; the remainder are young, from six to eight years old, at which age they begin to come into bearing. The proper way to raise orange-trees is to make a bed about three feet wide and twenty long, with the earth in it Avell pul- verized ; and in January or February plant this bed with seeds, in rows a foot apart, and the seeds six inches apart in the rows, and about six inches deep. The bed should be weeded care- fully, and kept constantly moist. If in the dry sand of Los Angeles county, the bed should be irrigated once a week. At the end of three years the trees will be four feet high and an inch and a half thick in the trunk. They should then be set out in the orchard where they are to stand, and be planted twenty-five or thirty feet apart each way. The transplanting should be done in any of the spring months, the earlier the better, and should be immediately followed by irrigation. The transplanting should not take place when the young trees are growing, and therefore the trees should not be irrigated be- fore transplanting, especially if the weather be warm ; for warmth and irrigation would have a tendency to start the shoots. The trees begin to bear in their seventh year, when they are about ten feet high, and the trunks from three to five inches thick. At fourteen, years they are in full bearing, and they continue to bear till they are at least fifty years of age, proba- bly much longer. In full bearing, every tree will produce at least one thousand oranges a year, and some trees will regu- larly produce two or three thousand. The tree grows to , be thirty feet high, the top spreading out thirty feet wide. It blossoms early in the spring, and the fruit is ripe in the follow- ing February, although it looks ripe in December. The or- anges will keep well until May, if left on the tree. The fruit is always in demand, and always commands a high price; and previous to 1857, Mr. Wolfskill made more than one hundred AGRICULTURE. 193 dollars apiece annually from his bearing trees; but since that time the bugs have injured the crop seriously. Tlie tree is very beautiful, and grows continuously. The wood is hard and valuable. The tops grow very bushy, and frequently branches have to be cut out to allow the air to have access to the fruit and leaves ; and sometimes the trees have to be supported, to save them from breaking down under the weight of their fruit. The trees, after setting out in the or- chard, should be irrigated thrice every summer, and, unless the land is rich, should be flianured. The bug, a species of Aphis, has fixed itself in most of the bearing trees in the state ; and unless some remedy not now in use be applied, it will probably kill all the trees. Many devices to drive away the pest have been tried in vain. But there must be a bane for this bug : when that bane is once found, the cultivation of the orange will take an important place in the horticulture of the southern part of the state, and therefore every good citizen is interested in finding it. § 151. The Grape. — California is a favorite land of the grape; and indeed many of our vine-growers suppose it to be the best grape country in the world. The grape region of California extends from the southern boundary, at latitude 32° 30', to 41°, a distance of five hundred and ninety-five miles from north to south, with an average breadth fiom east to west of about one hundred miles. The Los Angeles grape district is in an open plain about seventy miles long, and reaching back thirty miles from the ocean — bounded on the east by barren, rugged mountains. The So- noma, Napa, and Santa Clara grape districts, are in flat, nar- row valleys, shut in by steep, rugged ridges of the Coast Mountains, between latitude 37° 30' and 39°. The Sacramento grape district is in a flat valley, about half way between moun- tain-ranges fifty miles apart. The graj^e districts of the Sierra Nevada are situated on the western slopes of those high mt.nn- tains, usually in very small dales. The soil of the vineyards at Los Angeles and Anaheim is a 9 194 EESOUECES OF CALIFOENIA. deep, light, warm sand, which, to the inexperieneed eye, looks as though it were too poor to produce any valuable vegetable growth. In those places where water runs through it for a few days, all the mould is dissolved and carried off, leaving a white and almost pure sand. The soil is so dry, that cultiva- tion^is possible only with the assistance of irrigation. In So- nora and Napa valleys the vineyards are planted in a red, gravelly clay near the foot of the mountains, or in a light, sandy loam in the centre of the valley. Of late, the vine-growers of these valleys have done without irrigation. In Santa Clara valley most of the vines have been placed in a rich, black loam, but their vineyards are unhealthy. The Sacramento vineyards are planted in sandy loam ; those of the Sierra Ne- vada in sandy loam or in gravelly clay. The vine was brought to California by the Spanish mission- aries about the year 1770. So far as is known, only one vari- ety — that now known as the Los Angeles grape — was brought by them in the last century. It is the vine found in all the old vineyards and in most of the new ones south of the bay of San Francisco. It fills three-fourths of the vineyards in the state. The berry is round, reddish-brown while ripening, and nearly black when fully ripe, about five-eighths of an inch in diame- tar at its largest size, covered by a strong skin, possessing an abundance of thick and very sweet juice, with little meat, but with no fruitiness of flavor. It has been asserted that this grape is of the Malaga variety ; but if so, it has changed so much — perhaps while under cultivation in Mexico, whence the first cuttings that came to California were probably obtained — that it no longer resembles its parent stock. About 1820, when the missions were established north of the bay of San Francisco, a new variety, now called the So- noma grape, and said by General Yallejo to be of the Madeira stock, was introduced. It is now extensively cultivated in Sonoma and Napa counties and in the Sacramento valley, and is also found in a few vineyards south of the bay of San Fran- cisco. The berry is bluish-black in color; is covered, when AGlilCULTURE. 195 ripe, with a grayish dust, which brushes off, leaving a glossy, smooth skin ; is about half an inch in diameter at its largest size ; has a thin, sweet juice, with more meat and a little fruiti- ness of a flavor. The Sonoma grape makes a light wine, resembling claret ; the Los Angeles grape makes a strong wine, resembling port and sherry. The two grapes are classed together as the " Mis- sion," " jS'ative," or " Cahfornian" grapes, and were the only varieties cultivated here previous to 1853. In that year the importation of foreign grapes commenced, and now about two hundred varieties are cultivated. The Mission grapes are hardy, healthy, long-lived, productive, and early in coming into bearing ; but they are surpassed in flavor, hardiness, produc- tiveness, earliness of ripening, and earliness of bearing, by many foreign varieties, Avhich, so far as is known, are not infe- rior in any respect. The latter have been tried, however, only three or four years, and therefore we cannot speak positively whether they will prove so long-lived, or whether they will be equal in some other points to the Mission grapes. Still, the superiority of the foreign grapes is so great, that no reasonable man, acquainted with the subject, doubts that they will drive the Mission grapes out of the market. Flavor is a matter of vast importance in fresh fruit, and the want of it is the great defect of the Mission grape, which will not com- mand more than six or eight cents per pound in the San Fran- cisco market, at the very time that fine foreign varieties bring twenty-five and thirty-seven cents. Cuttings of the Mission grapes can now be had for ten dollars per thousand, a price that will not more than pay for prej^aring them for market ; while those of the foreign cost from forty to one hundred and fifty dollars per thousand. For wine, the foreign grape has an equal or still greater advantage. Flavor and fruitiness are no\ less needed there than in fruit to be eaten fresh at the table. The lack of fruitiness is the great misfortune of the wine made from the Colifornian grape, and the evil can only be remedied by the use of the foreign grape. 196 EESOURCES OF CALIFOENIA. For raisins the Mission grape is unsuited, because it is all juice and lacks meat. Again, we want various kinds of grapes to make different kinds of wine, and to give variety to our tables ; and we wish also to have early and late grapes, so that our wine-making may extend through a long season, and that our tables may have grapes upon them from August to Decem- ber. The foreign grapes, it has been observed, are stronger to resist the frost than the Mission grape. The latter is there- fore doomed, if not to destruction, at least to a subordinate position. About two hundred varieties of grape are cultivated in Cali- fornia, including the most noted stocks of Spain, France, Ger- many, Hungary, and the Eastern states. Nearly all of them thrive, and it can scarcely be said authoritatively that any one of them has proved a failure. The Catawba and Isabella do well; the latter furnishing our finest table-grape for some tastes, while others prefer some of the Muscatels. The total number of grape-vines planted in vineyard in the state is about nine and a half millions, or ten thousand five hundred acres, of which more than one-third are in Los An- geles county. One-fifteenth of these may be foreign vines, of which one-half are in Sonoma county. There were probably two hundred thousand bearing vines in the state in 1 848, and they still continue productive. Yery little was done to increase their number until 1856, and then the business of grape-grow- ing and making wine for the market was commenced. The new vineyards then set out were planted with Mission grapes, the only variety of which cuttings in large quantities could be obtained. A few foreign vines had been imported in 1853, '54, and '55, by nurserymen, but there was little demand for them. When it became clear that California would produce wine largely, the foreign varieties came into demand. It was not until 1859 that the superiority of the foreign grapes as a class over the Mission grape was established by trial. The advantages of California for the cultivation of the grape are the following : AGRICULTURE. 197 1. Californian vineyards produce ordinarily twice as much as the vineyards of any other grape distiict, if general report be true. Here, twelve thousand pounds of grapes per acre is a crop as common as six thousand in France, Germany, or Ohio, Why our vineyards should produce so much more than those else- where I know not, but the fact is indubitable. Crops of twenty thousand pounds per acre have been seen here, but never else- where, if witnesses, generally considered credible, are to be believed. 2. The grape-crop never fails, as it does in every other coun- try. This is owing partly to the fact that we have no severe frosts, no hail, and no storms of rain and electricity from the time the vine buds until the grape is gathered, each of which often causes a total loss of the crops in Europe. There is abun- dant time for gathering the grape, while in other vine coun- tries the rain and frost destroy the fruit after it is ripe. The oidium — the disease which has done such o-reat dama^^e in France — appeared in 1859, but has done no injury as yet save in a iQ,\Y small, young vineyards. I have heard of it only in Santa Clara, Sonoma, and Alameda counties, where the vines are planted in a Avet, black loam, or stilf clay. Bugs and in- sects, which do much harm in European vineyards, have as yet done no injury worthy of note in California. 3. Vineyards in other countries require more labor than in California. In Europe, the vine is trained with a stalk four feet high, and supported by a pole, which has to be set down every year, and to which the vine is tied. Here the stalk stands alone. 4. The equability and warmth of the climate render it easy to make wine by fermentation without artificial heat during the winter ; whereas in other grape countries fires must be kept up in the cellars through the winter. 5. The great variety of grapes which thrive here as com- pared with every other grape country. The disadvantages of California consist in the high price of labor (three times as high as in Ohio, and four times as high 198 EESOTJRCES OP CALIFORNIA. as in Europe), the ignorance of the people of the arts of vine- growing and wine-making, the dearness of casks (costing from five to twenty cents per gallon), and the necessity of irriga- tion. Land suitable for vineyards costs from twenty to one hun- dred dollars per acre, whereas it is worth several times as much in France ; but there is a counterbalancing difference in the interest of money, so that the French vine-land at four hundred dollars per acre, bought with money borrow^ed at six per cent, a year, costs little more than a Californian vineyard bought for one hundred dollars, with money at twenty-seven per cent. The vine likes a sandy or gravelly (not very moist) soil, and never thrives in wet, loamy, or stiff clay soil. In California, neariy all the vineyards are planted on flat land ; in Europe, hills are preferred, and in Germany the name for a vineyard is " Weinberg" — a vine-hill. Vineyards are planted with cuttings or with rooted vines. The cuttings are obtained at the annual pruning in January or February, are about thirty inches long, and are all of wood less than a year old. They should be taken from vines not less than four years old. The rooted vines are cuttings which are planted in the nursery and allowed to grow there through one season. These latter may be planted out from November to March, inclusive ; cuttings from January to March. It is not usual to plough more than once before planting, but sev- eral ploughings would be better. The vines are planted either six and a half or eight feet apart each way : the former distance giving one thousand vines to the acre, is customary at Los An- geles ; the latter, giving six hundred and eighty vines to the acre, is preferred in Sonoma and Napa. The vines are planted about two feet deep, perpendicularly, leaving about three or four inches with two buds above the surface. The holes are usually made with a crowbar, and after the vine is thrust down into it, a httle loose sand or pulverized dirt is poured in to fill up the hole. Sometimes holes are dug with the spade. Unless the ground is very moist, the newly-planted vineyard is ii'ri- ^ A G R 1 C U L T L K E . 199 gated ; for the vine, when takiiig root, likes water. During the first year after planting, the vine-grower has nothing to do save to irrigate twice, to plough several times, and to hoe down such weeds as cannot be reached with the plough. There is very little growth of wood the first year, but it fre- quently happens that cuttings bear grapes — one bunch, it may be, to a dozen vines. Rooted vines do not bear the first year. The next year the ground should be kept loose and clean by ploughing and hoeing twice or thrice. Any suckers springing out from buds beneath the surface must be broken off, and a little pruning is done. In pruning, regard is had to the form which the stalk is to have. The vine bears fruit on new wood ; that is, on twigs pro- duced in the same season with the grape. All the twigs are cut off every year, leaving a bare stalk. In the old vineyards of California the stalks are from three to five feet high. Of late, the more general custom is to make the stalks about fif- teen inches high. It is observed that the nearer the grapes to the ground, the earlier they ripen, and the less liable they are to injury from frost and wind. The strongest shoot is selected to make the stalk, and it is tied to a little stake stuck into the ground at its side, and the other shoots are cut off. It is a matter of importance to use the stake so that the vines may grow straight up. Vineyards planted with cuttings bear no grapes the second year ; those planted with rooted vines may bear a few. In the southern part of the state the vineyard must be irrigated at least twice every summer ; in many locali- ties in the northern and middle districts, irrigation is consid- ered unnecessary, though it would undoubtedly be beneficial during the first year. The third year, the ploughing and hoeing is the same as the second. More attention must be given to the pruning. All the twigs are cut off save two or three, which sprout from the top of the stalk, and these are pruned so as to leave but two buds on each, which are to produce all the wood and fruit of the season. This year the vines should produce three or four 200 KESO URGES OF CALIFORNIA. pounds of grapes each ; some vineyards have averaged twelve pounds to the stalk the third year. The fourth year, the live or six twigs all starting from the top of the stalk are left with two eyes each ; and this year the yield should be six or eight pounds per vine. The fifth year, there should be seven or eight twigs, with two eyes each, and the grape-yield should be ten pounds per vine. The sixth year, the vine is in full growth, and there should be eight or ten twigs, and from ten to fifteen pounds of fruit per vine. About the fortieth year the vine begins to decay. After the third or fourth year, if the vine has been well trained, it needs no stake for support, but stands alone. The towns most notable for the cultivation of the vine in California are Los Angeles, Anaheim, and Sonoma — all grape- towns, and the only towns which depend chiefly on the grape for their revenue. Los Angeleshas about 1,900,000 vines, Ana- heim 400,000, and Sonoma 1,500,000. Many of the vines of So- noma are not yet old enough to bear ; those of Anaheim are all now (1862) in their fourth year; while more than one-half of those of Los Angeles have been in full bearing for several years. The Cocomongo ranch, in San Bernardino county, owned by J. Rains, has a vineyard of 165,000 vines, most of them very young yet. This ranch is one thousand feet above the sea-level, and has the reputation of producing the best wine in the state. Hock farm, in Sutter county, has a large vine- yard, owned by Emil Sutter, a son of Captain J. A. Sutter, and the wine produced there has an excellent reputation. Among the largest vineyards in the state are the following: A. Haraszthy, Sonoma 500,000 vines. John Rains, Cocomongo 165,000 vines. B. D. Wilson, San Gabriel 100,000 vines. "William Wolfskill, Los Angeles 85,000 vines. C- H. S. Williams, Sonoma 68,000 vines. Matthew Keller, Los Angeles 61,000 vines. Corbett and Dibblee, Santa Anita 60,000 vines. T. J. White, Los Angeles 50,000 vines. J. R. Scott, Los Angeles 50,000 vines. AGEICULTUKE. liOl There are many vineyards in the mining counties, but they are small and young. In 1858, an acre of bearing vineyard was worth a thousand dollars ; but since then the supply of grapes and native wines has increased to such an extent, that the vine- yards have depreciated fifty per cent. The profits of wine- making several years ago, induced the vine-growers to make their wine hastily and carelessly, and much of it is poor stufli", that has brought all native wines into discredit. The wine- business, just now depressed, will in a year or tw^o become better, and then vine-planting will take a new start, and vine- yards will rise in value. § 152. Wine-makiJig. — The making of wine is considered a a branch of agriculture. In 1861, California probably made about a million gallons of wine, and the amount Avill increase within five years to three million gallons. The best wines are made from foreign grapes, of which, however, not many are as yet produced in the state ; so that the Mission grapes yield the chief supply. The principal classifications of wane are into red and white, light and heavy, still and sparkling. Wine making commences with the ripening of the grapes, about the middle of September. The berry is considered to be fully ripe when the heart has taken a tinge resembling the darkness of the skin ; when the berry is perfectly sweet, and comes off easily from the stem, leaving no juice upon it; and when, on holding a bunch up to the sun, the fibres running from the stem into the berry are nearly or quite invisible. The branches are cut off w^ith a knife, after the dew or fog (if any) has been dispelled, put into a basket, and carried to the press. Here the rotten and unripe berries are carefully picked, out, and the bunches are then thrown upon a coarse wire sieve. A man presses the bunches upon this sieve, through which the grapes fdl, some broken and others un- broken, while the large stems and leaves will not pass, and are thrown away. Below the sieve is the masher, composed of two rollers, ten inches in diameter and three feet long, made of iron or wood. These rollers, turning toward each other, 9* 202 RES0T7ECES OF CALIFORNIA. crush the berries, but do not bruise the seeds, which, if crushed, would give a bitter taste to the wine. If the wine is to be white, the pulp is pressed as it comes from the masher ; if it is to be red, the pulp is left to stand for six or eight days, so that the red color of the skins may be communicated to the juice. This is the only mode in which wines are colored. The juice as it comes from the fresh berry is never red, but some varieties of grape make a yellowish juice. After the pressing, the red and. white wines are treated in the same manner. The juice is put into large casks, usually those of one hundred and forty gallons each, and about one hundred and fifteen gallons are put in each. The casks are thus not filled entirely, but a considerable surface of the wine is left exposed to the air. This is to favor fermentation, to which the atmosphere is necessary. The cask lies upon its side, the bunghole is left open, and in three or four days the fer- mentation begins ; in three or four more its period of greatest activity has passed. The temperature is a matter of the ut- most importance to fermentation, the proper degree being about 65° Fahrenheit ; and if the liquid be kept either warmer or colder than that figure, it will be in great danger of spoil- ing. The fermentation is accompanied by a rising of little air- bubbles to the surface, where they burst, making a noise that may be heard by applying the ear to the bunghole, and which is sometimes so loud as to be heard in the cellar at a distance of ten or twenty feet from the barrel. After the fermentation has been in progress three or four days, the wine-maker pours in six or eight gallons of fresh juice every day, until the cask is full ; and for several days after that he leaves the bunghole still open, and throws out all scum that rises to the surface there. When the scum has ceased to rise, the barrel is closed, and not disturbed for a pe- riod which should not be less than three weeks nor more than three months. After this, comes the " racking off." All the liquor, except about four inches at the bottom, containing sedi- ment, is drawn off through a siphon, or a cock placed above AG EI CULTURE. 203 the level of the sediment. The remamder is filtered through a doubled cotton cloth, and is then poured in with the clear liquor, or used in making brandy. The sediment deposited in the bottom of the cask within the first three months is about one-twentieth in weight of the juice as it comes from the press. After the first racking, the new cask is filled up, the bung is put in, and the wine is not disturbed till March or April, when it begins to feel a more lively fermentation, for that process never ceases entirely. It is said that the wine sympathizes with the vine, and that whenever the latter is in active development, the former feels a peculiar impulse also. Thus, the periods when the vine sprouts in March or April, when it blossoms in June, and when the grape ripens in September, are also the times when the fer- mentation is the most active. At those seasons the bungs must be taken ofi*, or at least loosened, and the barrels must not bo moved. It is an important point with wine-makers to avoid disturb- ing the process of fermentation. Between times, when the wine is at rest, it should be racked off, and placed in a clean cask. At the end of a year and a half the wine has become clear, but it continues to grow better with age for about a score of years, about the expiration of which period it has ac- quired a mellowness and delicacy of flavor and an oiliness of consistency wliich neither gain nor lose by longer preserva- tion. Many kinds of wine are made in California. The light wines come in this state, as in other parts of the world, from the northern, and the strong wines from the southern districts. The wines of Los Angelica have a body like those of Spain, and the wines of Sonoma and the upper Sacramento valley re- semble claret and hock. A wine similar to port is made in the southern part of the state, by leaving tlie grapes on the vines until they are " dead ripe," and somewhat shrivelled by the sun. The juice is then very strong, and, being left with the pulp ten days or two weeks, takes a strong, dark-red color. 204 EESOUBCES OF CALIFORNIA. Wine is defined to be "the fermented juice of the grape," and therefore "Angelica" is not properly a wine, though it is usually classed under that title. It is made by mixing brandy, in proportions varying from one-fifth to one-third, with the grape-juice fresh from the press or but a few hours old. The brandy prevents fermentation. Angelica is a sweet liquor, and is usually considered a proper drink for women ; but it is really stronger than the fermented whines. The wine made of the juice that drips from the masher, or of the first drainings from the press, is considered superior to that obtained by severe pressure from the pulp. After the pulp has been pressed, it is sometimes covered with water, allowed to stand a few days, and pressed again ; and the wine made of this liquor is called " Piquet," a very light w^ne, and generally sourish in taste. Some sparkling wine has been made in California, but thus far without great success. The only house which has engaged extensively in the business is that of Sainsevain Bi-others, w^ho brought an experienced Avorkman from the champagne district of France. They own a large vineyard at Los Angeles, and another at San Jose, and have a large capital invested in the wine-business. Their failure in making the " sparkling Cali- fornia," as they call their effervescent wine, was owing to the strength of the Los Angeles grape, and the " earthiness" of its taste, which earthiness is stronger in the sparkling than in the still liquid. Effervescent wines should not be strong ; and the grapes grown at Los Angeles, or at least the Mission grapes grown there, are too strong. I speak of the experiment as a " failure," meaning thereby that the Sainsevains have not made an article equal to the best brands of imported champagnes; but, for all that, it is a passably good wane. Attempts are to be made this year, and for several years to come, with the lio-hter wines made in the middle and northern parts of the state, and there is good reason to believe that the experiment will prove entirely successful. Sparkling wine is treated like still wine until after the first AGRICULTURE. 205 fermentation, except that it receives much more attention, and is made from a more careful selection of berries, than any other kind of wine. After the first fermentation, the wine is put in bottles, and tliese are placed in racks with tlieir necks down, the racks being made so that the bottles can be raised and lowered ; and the position of the bottles is changed from time to time, to assist fermentation, which continues, though in a suppressed form — the carbonic acid gas being retained in the wine, instead of escaping as it does during the fermentation of still wines in the open barrel. The management of spark- ling wines is very complicated. It varies greatly in different places, and is usually kept as secret as possible. Thus, the Sainsevains keep their process to themselves. Wliite grapes will not make a red wine ; but the skins, if left to ferment with the juice, will give it a dirty-yellow or light-brown color. The general custom, in making wine, is to use the pure juice of the grape, but wine-makers consider it not unwholesome or disreputable to put sugar, water, or brandy, into certain kinds of wines ; all of which, however, are unnecessary and injurious to the finer kinds of still wines. Sugar and water endanger the keeping qualities of the wine, and brandy spoils the flavor. In France, it is common to put sugar or rock-candy "j/(/j wine intended for the sweet tastes of the Americans ; ar.d in bad years, when the grapes are sourish, they sweeten a little for home consumption. Brandy is sometimes used to prevent wine from turning into vine2:ar ; but the mixturj, if stroncj enough to have the desired effect, deserves rathtr the name of adulterated brandy than of wine. Different kinds of pure wines may be mixed without impropriety, but the label sliould not misrepresent the nature of the mixture. It is a fraud to mix a bad wine wdth a fine article, and then sell it by the name of the latter. If a wine-maker sends his wine into the market under his own name, no other person can honevdy nil^ any thing else with it, and still preserve the name of the < rlginal maker. 206 EESOUKCES OF CALIFORNIA. Most of the wines hitherto made in California have been pure, but not fine in flavor. The Mission grape lacks delicacy and fruitiness of taste, and gives an earthiness or harshness to the wine. These defects will probably be remedied by the use of the foreign grapes, and their mixture with the native Mission grape. Still wines, equal to the best still wines of France, have been made from foreign grapes in California; and we presume that we can make equally as good wine, in very large quantities, so soon as we have the grapes. Only about one-tenth of the foreign vines planted in the state are now in bearing. The skin of the grape probably contains tannin, for the red wines have an astringent taste not common to the white. The cellar is a matter of great importance to the wine- maker. From the moment when the grape-juice comes from the press until the wine is brought upon the table to be drunk, it should be kept in a cellar ; and it is only in a cellar that the equability and coolness of temperature proper to favor fermen- tation can be obtained. In France and Germany, it is often necessary to have fires in the cellars; and it would be well to have them occasionally in California. Indeed, wine-makers generally have no cellars, but only houses. In Los Angeles county, most of the wine is kept in adobe houses. The sandi- ness of the land, the frequent irrigation, and the proximity of the vines to the places where the wine is stored, would lead to the filling of deep cellars with water ; so the cellars are dug only three or four feet into the ground ; and an adobe wall three feet thick, and a thick covering, render the cellars pretty cool. In Sonoma, Colonel Haraszthy has dug a wine-cellar in the side of a hill of magnesian limestone. The wine-cellar should be used for wine alone, because the presence of other things — especially salt meat, leather, and putrefying vegetables — may spoil the flavor of the wine. It is probable that, in many of the vineyards, the soil will not produce a first-rate wine. In Europe, the wines from the fiat lands are generally of an inferior quahty. To what extent AGRICITLTUEE. 207 this rule prevails here, cannot be ascertained until we have given the finer foreign grapes a fair trial. Certainly the Mis- sion grape takes up in most of the vineyards an earthiness of taste which must never be found in wines of the best quality. We cannot yet tell what are our best grape-soils, or how they differ from one another in their influences on the wine. It is certainly no easy matter to make fine wine out of the Mission grape, and most of our wine-makers have little experience in the business. Again, they send their wine to the market too soon after it is made. They often use old barrels and bottles, which may give a taste to the wine. They have also been too careless in pressing grapes before they were fully ripe, and without picking out the green and rotten fruit. § 153. Berries. — Alameda county cultivates, chiefly for the San Francisco market, four hundred and fifty acres of straw- berries, one hundred of raspberries, and thirty of blackberries — more than all the remainder of the state. The varieties of strawberries most prized are the British Queen and Long- worth's Prolific. They are planted in rows, thirty inches apart, and the plants are a foot apart in the rows. The straw- berry comes into the market in April, and continues abundant till July, but it may be obtained in any month in the year ; and the only reason why large quantities are not grown from August to October inclusive, is, that they are not in demand, because of the abundance of cheaper fruits. It must always be costly as compared with the tree-fruits, because it is more perishable, requires greater cultivation, costs more for pick- ing, and produces less to the acre. The picking alone costs about two cents a pound, being done by Chinamen, who pick forty pounds in a day, and are paid seventy-five cents a day, they providing their own food. The average yield per acre is about one thousand pounds, and the average wholesale price in 1861, during the season of their abundance, nine cents per pound, making a gross yield of one hundred and twenty dol- lars to the acre. The largest field of strawberries contains eighty acres, the second seventy, and the third sixteen. Yery 208 KESOURCES OF CALIFORNIA. few strawberries are preserved, or used in any way save to be eaten fresh on the table. Most of the raspberry-fields of California are in Oakland and its immediate vicinity. The land about a mile northward from the Oakland wharf is said to be peculiarly favorable to the raspberry. .The average yield is about fifteen hundred pounds per acre, and the wholesale price in 1861 was ten cents per pound. The picking is done by Chinamen, and costs from three to four cents a pound. The bushes are planted in rows five feet apart, and one foot apart in the row. The berries are produced on wood a year old, and at the end of every season all the wood that has borne is cut away. It is not known how long the raspberry-bush will continue to bear, but probably ten years at the least. The largest raspberry-field in the state contains twenty acres. An excellent wine is made of raspberries, and some of the Oakland people have gone into the business, hoping to derive a large profit from it. The berries are bruised, a gallon of water is poured on for three pounds of berries, and after three days the berries are pressed ; three pounds of sugar are added for every gallon of the liquid, which is then put into barrels, and allowed to stand, with the bung open, until active fermen- tation has ceased — a period varying from five weeks to two mouths — and the wine is ready for use, though the longer it stands the better it becomes. Soft water is better than hard for putting on the berries, and hard water should not be used without boiling. An acre of raspberries will }ield six hundred gallons of wine, which, if well made, is worth a dollar or a dol- lar and a half a gallon at wholesale. The raspberry cultivated at Oakland is the Fastolf variety. The fruit ripens during June and July. The Lawton blackberry is also cultivated, about Oakland. The rows are from six to eight feet apart, and the plants from four to six feet apart in the row. The yield of the blackberry and the cost of picking are about the same with the raspberry, but the price is much higher, the blackberry selling at whole AGRICULTURE. 209 sale in 1S61 at twenty -five cents per pound. It is in the mar- ket from the first of July to the middle of September. Wine is made from the blackberry in the same manner as from the raspberry, and sometimes the two berries are combined to- gether. § 154. Ornamental Shrubs. — Professional gardeners say that California is better fitted by Nature than any part of Europe or the Atlantic slopes to have beautiful ornamental gardens. Our shrubs are more numerous, grow larger, remain green longer, and have a longer blooming season, than those of other states. The mayo and malva trees, the rose, the daisy, the pansy, the oelyssum, the clyantlius punceus, the flowering ver- bena, the hollyhock, and the calla or Ethiopian lily, bloom here in the open air every month in the year. The honeysuckle, metrosideros, and myrtle, bloom from March to December ; the geranium and snow-ball from April to October; the violet from October to May ; the pittosporum from November to March ; the spireas and flowering almond from March to June ; and the camelia japonica from January to May, all in the open air. Persons at all familiar with the cultivation of these flow- ers in New York will observe that the blooming season here is, on an average, fully double its length there. Not only do they bloom in the open air, but they retain their leaves through most of the Avinter months, so that our gardens are never bare and clieerless as they are in the Atlantic winters. I have seen a rosebush bearing twenty full-blown roses in January, and that in the open air, with no assistance from artificial heat, and no protection save that of clambering up a brick wall on the southern side of an unoccupied house. Our roses are larger as well as more abundant than in the Eastern states, but their perfume is not so strong. A marked feature of our ornamental gardening is our ability to cultivate in the open air many plants which can only be pre- served in this latitude east of the Rocky Mountains under glass and with the aid of artificial heat. These plants are too nu- merous to be all specially named here ; but some of the more 210 RESOURCES OF CALIFOEXIA. important are the orange, camelia japonica, laurastinus, myo- poriim, ericas, casuarina, daphne, eucalyptus, metrosideros, and thirty varieties of acacia, twenty of them from Austraha. It might be ahnost said that we have no hot-houses in the state, but only green-houses, for it is scarcely ever necessary to make a fire, even to protect the most dehcate of tropical plants. Our climate is very favorable to the growth of evergreens, especially to those strange and beautiful ones from Austraha, w^ith the graceful growth and the brilliant, feathery foliage. Two of the most striking features of our ornamental horticul- ture are the malva and mayo trees. The former, a native of the southern part of this state, grows to be about fifteen feet high, continues green throughout the year, and is always cov- ered with abundant foliage and a wreath of lai'ge crimson flow- ers, resembling the flowers of the crimson hollyhock in size, shape, and color. The mayo-tree is an evergreen, originally from Chile, always brilliant with abundant yellow flowers. Among the most common and beautiful creeping vines grown in California is the Australian bean, which has a dense, bright, evergreen foliage, and abundant flowers throughout the year. It climbs strings, and is therefore well suited to shade verandas and to grow in the front of porticoes. The rose, the honeysuckle, the veronica, the oleander, the laurastinus, the euonimus japonica, and the verbenas — espe- cially the lemon verbena — may safely be said to make twice as nmch wood in a year as they do on the Atlantic coast. The geraniums in San Francisco are almost trees. Rose-sprouts often grow twenty feet in a season, and other plants in propor- tion. There is scarcely any tree or shrub cultivated in the At- lantic states which does not thrive equally as well here, except the weeping willow. California has thus far furnished very little for our gardens. There are many singular plants in our mountains, but few have found favor with our gardeners. The malva and the ce- anothus are the chief ornamental shrubs, indigenous in Califor- nia, adopted for cultivation. AGKICULTURE. 211 We liave not yet had time to produce many ornamental gardens ; but I think the time is not far distant when no place in the world will, within so small a district, have so many fine gardens as the valleys round San Francisco Bay. § 155. Pests of the Farnier. — Certain "pests" of the farmer must be mentioned here, among which are the spermophile, gopher, grasshopper, locust, grape-bug, orange-bug, army- Avorm, Canada thistle, mullen, dock, fern, and so forth. Of the spermophiles and their habits I have spoken in the chapter on the zoology of the state. The amount of mischief which they do is very great. The most effective means of driving them off are poisons, chiefly strychnine and phosphorus. About a> drachm of strychnine is dissolved in a quart of whiskey, and then the solution is poured over dry wheat in such quantity, that the surface of the liquid is just on a level with the top of the grain. In the course of twelve hours the wheat absorbs all the liquor, and a fe\r grains may then be thrown in front of every squirrel-hole. When phosphorus is to be used, the wheat is soaked in boiling water until it is soft, when the wa- ter is drawn off, and the wheat in a pan is put in or over boil- ing water to keep it near the boiling heat. A stick of phos- phorus three inches long is put into the hot wheat, melts in ten minutes, and the wheat is stirred about well, so that the melted phosphorus will touch every grain. The wheat is then poured upon some bran in which it is rolled so that every kernel may be covered, and the grain is ready for its purposes of destruc- tion. A couple of kernels will kill a squirrel ; and if a cat eats the squirrel, it will kill him ; and if a raven picks out the eyes of the cat, he will die too : and such a progressive destruction has been observed more than once in California. The gopher is more readily caught with traps than the sper- ''mophile. In the chapter on zoology I have described the trench used for keeping gophers out of orchards and gardens, and for catching them. Several traps are in common use, but it is not easy to describe them ; so I will not attem|)t it. The grasshoppers are the greatest pests of the farmer in 212 EESOUECES OF CALIFOENIA. California, and I fear thai we have not yet seen the worst of them, though several times during the last fifteen years they have eaten every green thing within large districts. They come in milhons upon millions, and darken the air, moving for- ward at the rate of a mile or two a day, and leaving no grass or leaf behind them. Grains, grass, weeds, kitchen vegetables, and fruit-trees, are alike eaten bare of every green particle. Grasshoppers are abundant in countries where the summers are dry, the winters warm, and the vegetation vigorous ; and if a large extent of land be uncultivated, they will occasionally be so numerous as to destroy every green thing. They are bred in the hills of California, and after dry winters descend into the valleys, usually content to eat the wild grasses, but some- times attack the cultivated fields. There is no known method of killing them after they have entered a field, or of driving them away from it ; but they may be kept out by digging a trench, putting straw in it, wiih some moist straw on top, and then setting fire to it. The grasshoppers do not like the fire and smoke, and will try to avoid them. Under the head of the grape and the orange, I have spoken of tha bugs which infest them. The army-worm has been seen in California, but has done little damage as yet. The curculio and weevil are not known in the state. The Canada thistle, the muUen, and the dock, have been introduced, but have not yet given much trouble. § 156. Neat Cattle. — California has 1,100,000 neat cattle, 900,000 sheep, and 150,000 horses, nearly all bred in the open air and open plains, and fed only on wild grasses. The system of breeding live-stock difi"ers much in California from that which prevails in the Atlantic states, where cattle are kept in fields and stables all the time, and fed with cultivated food. Here domestic animals grow more rapidly, and reach their full develojmient earlier, than east of the Sierra Nevada. § 157. Spanish Cattle. — Most of our neat cattle are of the old Californian breed, brought hither by the Spanish mission- aries from Mexico, about 1770. At what time their stock AGKICULTURE. 213 came originally to Mexico is not precisely knoAvn, but without doubt it was in the seventeenth century, soon after the con- quest by Cortes, and they must have been imported from Spain. They are called " Spanish cattle." In Mexico, as sub- sequently in California, they were allowed to run almost wild, and they took something of the appearance of wild animals. They have nearly the same range of colors as the neat cattle of Europe ; but mouse, dun, and brindle colors — almost infal- lible signs of " scrub" blood — are more frequent ; and the deep red, fine cream-color, and delicate mottling of deep red and white, found only in animals of high blood, are entirely want- ing. Their legs are long and thin, their noses sharp, their forms graceful, their heads high, their horns long, slender, and wide-spread ; and they have a duskiness about the ,eyes and nostrils similar to that of the deer, between Avhich animal and a young Spanish cow there are many points of resemblance. The general carriage of the Spanish cow is like that of a wild animal : she is quick, uneasy, restless, frequently on the look- out for danger, snuffing the air, moving with a high and elastic trot, and excited at the sight of a man, particularly if afoot, when she will often attack him. In some counties it is, for this reason, unsafe to go about on foot. The native Californians are ahvays mounted, and to these the cattle are accustomed; but a man afoot is considered to be a dangerous animal, de- serving of the same treatment with wolves and coyotes. The Spanish cow is small, does not fatten readily, produces little milk, and her meat is not so tender and juicy as that of Amer- ican cattle. The breeding of neat cattle was almost the only business of the country previous to the American conquest, and they were killed for their hides and tallow, which were the chief exports. The meat went to enrich the land ; there was too much of it to be eaten. The breeding of cattle, being the chief occupa- tion of the Californians, determined their mode of life, the structure of their society, and the size of their ranches. No- body wanted to own less than a square league (four thousand 214 EESOUECES OF CALIFOKNIA. four hundred and thirty-eight acres) of land; and the govern ment granted it away without charge, in tracts varying from one to eleven leagues, to anybody who would undertake to erect a house and put a hundred head of cattle on the place. It was common for one man to own five thousand head of cat- tle. The cows were kept for breeding, and the steers were regularly killed as they reached the age of three or four years. All had the freedom of the country, and ranged where they pleased, except that several times a year every man collected his own upon his ranch. There was about one bull to fifty cows. No attempt was made to improve the breed, nor was any profit to be obtained from an improvement. Most of the calves were born about the beginning of the year, and in March the ^rsi^rodeo was held. § 158. Rodeos. — The word rodeo comes from the same root with "rotate," and means a surrounding, a gathering of all the cattle on a ranch, and the separation and removal of those belonging to other ranches. There are general and special rodeos. A rodeo may be for one ranch, or for several ; but every ranchero owning a large ranch and many cattle has his own rodeo. Every large ranchero must have at least one rodeo in the spring, and another in the fall. The general rodeo is held for the benefit of all the cattle-owners in the neighbor- hood ; the special rodeo is held for the benefit of some partic- ular person or persons who desire an opportunity to remove their cattle from a ranch. Every owner of a rancho is required by law to give a general rodeo every spring. When a general rodeo is to be held, the ranchero sends no- tice several days or weeks irf advance to the cattle-owners in the vicinity; and in the cattle-districts the neighborhood ex- tends forty or fifty miles, for cattle will stray that distance. On the day appointed, the ranchero having selected some j^lace where the cattle are to be collected, sends out his mount- ed vaqueros or herdsmen at daylight to drive the cattle to the appointed place, where they are gathered at ten o'clock. By that time, the interested rancheros with their vaqueros have AGRICULTTJRE. 215 made their appearance, and are on tbe ground, all mounted, and prepared for the day's work. The ranchero who gives the rodeo is present to entertain his visitors, and his men are instructed to keep the cattle together. The herd may be very large. I have seen eight thousand head of cattle in a rodeo, forming a solid body about a quarter of a mile in diameter in every direction. The visiting rancheros who have come from the greatest distance are permitted to enter the mass first, select their cattle, and drive them out. Each man has a position chosen at a distance of half a mile or a mile, whither he drives his cattle ; and there are several men there mounted, to prevent them from returning to the main herd. When a ranchero sees one of his cows in the herd, he calls to a friend, and the two chase her out. She does not wish to go, and tries to hide herself among the other cattle. The horses, accustomed to the rodeo, soon recognize the cow that is to be parted out, and enjoy the work. They turn with every turn of hers, and she is soon tired and compelled to go out. If the cow be accompanied by a large unmarked calf, the latter is often caught with the lasso, thrown down, and then marked with the knife. While these rancheros are riding about among the herd and seeking their own, the cattle are driven by a few vaqueros belonging to the ranch so as to move about in a circular manner. As the cattle are thus moving round in one direction, the rancheros of the immediate neighborhood, whose time has not yet come for entering the centre of the rodeo, ride round in a direction contrary to the course of the herd, and thus are enabled to see them to more advantage than if they were standing still. After the ranche- ros from a distance have parted out all their cattle, those of the vicinity ride in, and the whole day is thus spent in racing and chasing after cattle. The man who gives the rodeo does not attempt to examine the cattle which are taken away. He takes it for granted that every one will drive off only his own animals. Sometimes sev- eral days are necessary to complete the general rodeo of a 216 BESOURCES OF CALIFOKNIA. ranch, and the work is continued from day to day until fin- ished. All the rodeos of a neighborhood are usually held in a regular and close connection. The rancheros from a distance, therefore, stay imtil they have attended all the rodeos in a district to which they suppose that any of their cattle have strayed ; and they are usually the guests of the man upon Avhose ranch the rodeo is given. When a cow is driven out, her calf follows. Every ran- chero knows his cattle by the brand, which law and custom re- quire him to use. Of course, when a man has four or five thou- sand head of cattle, he cannot recognize them all by sight; he can only distinguish them by marks. He knows his cows by their brands, and his calves by their follo\ying the cows. The spring rodeos are the busiest seasons of the rancheros, and are for them the chief occasions of general meeting, exci- ting adventure, conversation, and festivity, in the course of the year. Frequently three or four hundred men will meet at these places, mounted on their best horses, and ready for fun. All the work of the rodeo is exciting. Lively scenes are enacting at every moment, and in every direction. Calves will try to get away from the herd, and escape to the hills. Cows which have been driven out will endeavor to get back. These nmst be chased by the horsemen. Frequently the lasso must be used. Many of the vaqueros are fond of showing their skill before so many spectators, and astonishing feats of horseman- ship are performed. When a ranchero returns from a rodeo, with his cattle which had strayed away, he drives them into his corral, and brands and marks his calves; so that if they should return to their former range, he will know them the next year. If those that have been on other ranches are too numerous to he branded and marked in one day, some of his vaqueros stay with them on horseback, and herd them until all can be marked. When a cow has be- come accustomed to a ranch, she likes to return to it. After all the calves are marked, the owner does not care much whither they go, provided that they do not stray beyond the limits of AGKICULTURE. 217 the ranches, the rodeos of which he attends. It is only in times of extraordinary scarcity of grass, that the rancheros are particular to drive tlie cattle of other owners off their lands. The rodeo season being over — that is, when the ranchero has all his cattle on his own ranch, and his alone — he com- mences the work of branding. His vaqueros drive about two hundred cows with their calves into the corral every morning, and two or three good vaqueros will brand these calves in a day. The vaqueros enter the corral with their horses, which they need when the calves are large and strong, for many of them are three and four months old. If the calf be small, the vaquero may be afoot to lasso him. One vaquero throws a reata over the calf's head, and another catches him by the leg ; they throw him down, and one holds him, while the other gets a hot branding-iron and burns the owner's mark upon its hip. Thus the woi-k goes on from day to day, and from week to week, until every calf on the ranch is marked. § 159. brands. — The law requires that every horse and cow shall be branded, with a brand belonging to their owner. The brand is made of iron, sometimes representing one or two let- ters, sometimes other arbitrary signs, such as a cross, a circle, a triangle, or any other design. Tiie brand may be six inches long by four wide, and tlie thickness of the iron is about a third of an inch. There is an iron handle, with a wooden crosvs-piore ut the end, so that the brand can be handled when hot, and held down tirndy upon the prostrate calf, until the figure is indeiibly burned into the skin. A copy of every brand must be burned upon leather, and deposited in the county re- corder's ofllce. Every miiior and servant on a ranch must use the brand of the ov/uer of the ranch. The brand must be burned, under j)enalLy, i,j)on all horses and neat cattle, before the age of eighteen mo:.ths. The braiul is buru'-d upon the hip, and inilicates ownership; when the animal is soM, the brand is burned upon the shouhlei', and indicates sale. The purchaser then jjiits his brand upon the hip; and thus the skin of a Californian horse or cow contains the history of its owner- 10 218 RESOURCES OF CALIFORNIA. ship. Many of the brands are well known to the rancheros over a large portion of the state ; and by looking at the ani- mal, they will tell where it was born, and who have owned it at different times. The hips and shoulders on both sides are often covered with brands. Sometimes the brands grow with the animals ; in other cases they remain nearly of their original size. A brand well burned into the skin is perceptible as long as the animal lives, though it grows less and less distinct witn the advance of years. In the fall there is another season of rodeos, to brand such calves as may have escaped notice at the spring rodeos, or may have been too small to be branded. The rancheros sometimes have a mark in addition to their brand, such as slitting the ear or cutting a notch in the dew- lap. A drawing of the mark must be deposited in the county recorder's office. It is contrary to law to cut off the end of the ear, or to cut it on both sides so as to bring it to a point ; for those modes of marking would give opportunities to cut away the marks of other people. The bull-calves are usually altered at the rodeos, as well as branded and marked. The cattle on many ranches are touched only twice in their lives by the hand of man — first, when they are branded ; and next, when they are slaughtered. § 160. Early Maturity of Calif ornian Coics. — The cows calve almost invariably before they are two years old, frequent- ly before they are eighteen months, and sometimes before four- teen months. They generally arrive at maternity a year sooner than in the Atlantic states. It is said that suckling heifers have been seen to take the bull. The Spanish rancheros have eight or ten bulls to a hundred cows ; the Americans usually four or five. The calves suckle from six to ten months ; that is, from January or February, when they are born, until No- vember, when the pasturage is very scanty. The Spanish cows have small udders, and yield httle milk ; and notwithstanding their great number in the country, butter, milk, and cheese were very rarely seen on the table previous to the coming of AGRICULTURE. 219 the Americans. American cows are the only ones used for the dairy, but many of them are now kept also for breeding alone, and, like the Spanish cows, they are never milked. § 161. Corral and Reata. — The corral is an important part of all cattle-ranchos, and on many of them it is the only enclo- sure. It is a pen, from thirty to fifty yards square, surrounded by a high, strong fence. It is used whenever horses or cattle are to be branded. The reata^ used for lassoing, is a rawhide rope, about five- eighths of an inch in diameter and thirty yards long. It is made of four strips of cowhide, from which the hair has been scraped ; and after plaiting, it is greased and dragged along on the ground after a saddle, to render it pliable. Rawhide is better than any other material, because it has just the proper w^eight and stiffness for the purpose. A running noose, which slips very easily, is arranged at one end. When the reata is to be used, the noose is made from four to six feet long ; one side of the noose and the reata just outside are taken in the right hand, so that while in the hand the noose will not slip ; the remainder of the reata is held coiled up in the left hand, ready to be let go. The vaquero swmgs the noose round his head, in such a way as to keep it open ; and when he has a good swing, he lets go, and away it Avill fly, its whole length. If it catches the object aimed at, the noose draws tight. It is not an uncommon thing for a vaquero to catch a cow at a dis- tance of thirty feet, while she and his horse are both running rapidly ; but usually he will get within fifteen or twenty feet, if he can, before throwing his reata. A good vaquero, stand- ing in front of another man, can push the latter back, and the moment his foot leaves the ground, throw a reata under it, and thus lasso him by the leg. When cattle or horses are to be branded, they must be thrown down ; and this is generally accomplished by catching the head with one reata, and a hind- leg with another. § 162. Occasional Starvation. — Nineteen out of twenty of the cattle of California never get any food, save such as grows 220 EESOUECES OP CALIFORNIA. indigenously in the open country, and they always suffer for it. From March to July the pasture is abundant and ex- cellent, and the cattle are fat ; from July to October, in ordi- nary years, the grasses and clovers, though dry and brown, are nutritious, and the cattle still remain in good condition ; but from October to January they grow lean rapidly, and almost every year a considerable number of them die by starvation. Either the grass may be all consumed, or it may be deprived of its nutriment. The first case happens when the grass is very scanty, because of a small fall of rain during the winter ; the second occurs when a heavy rain, lasting a day or two, comes before New Year's day, and is followed by cold dry weather. The rain takes away the palatable and nutritious qualities of the old grass, and the cold and dry weather pre- vents the starting of the new grass, and between the two the cattle suffer. In 1856, seventy thousand head of cattle died in Los Angeles county alone by starvation, one-third of the entire "uumber in the county. The state has not one large cattle-ranch surrounded by fence, and therefore, if a man owns good pas- ture land, the cattle of other people come and eat the grass, and later in the season his own must suffer. It is impossible for the vaqiieros to drive away the strange cattle, because they enter the ranch on every side every day, and if the grass be much better than on adjoining ranches, they will, if driven away one day, return the next. The j^roper and profitable method of managing an extensive cattle-ranch, is to have it all fenced in and divided ofi' into a few large fields, in which the cattle could be pastured at different seasons. It would also be a source of profit to have hay for them or green alfalfx in the early winter, so that there would be no danger of a reduction to skin and bone : for it costs thrice as much to replace as to preserve a pound of flesh. Spanish cattle, when slaughtered between September and February, are usually very thin, and in the Atlantic States it would be grossly impolitic to send such animals to the market. § 163. Imported Cattle. — The great majority of the cattle AGKIOITLTURE. 221 in the state are of pure Spanish blood, but there is a consider- able number of American cows and half-bloods, which are constantly increasing in number, while the Spanish cattle are decreasing. Most of the American cattle are in the Sacra- mento basin and the coast valleys north of Monterey, while along the southern coast they are very few in number. During the last four or live years about seventy-five pure- blood Durhams, twenty-five Devons, and four Ayrshire bulls and cows, have been imported across the Isthmus of Panama. The freight on the steamer and railroad, from New York to San Francisco, for a bull or cow, is two hundred and seventy-five dollars. The food is carried free of charge, but the owner must find a person to feed and take care of the animal during the voyage. Some of these imported animals are of the best English stock. The better the blood the larger the beeves grow, and the more readily and rapidly they fatten. The Spanish cattle are too uneasy ; they run about so much that they lose flesh. The half breed American cattle are more quiet, the full-blood Ameri^ can still more quiet, and the Durham the best of all. But as our beef cattle get no food save such as they pick up in the open country, I doubt whether it will pay to import these pure-blood Durhams to improve the breed. The excellence of the Durham is caused by care in breeding, protection against the weather, and an abundance of good food ; and the excellence cannot be main- tained without a continuance of the same system of manage- ment. The Durham will, in a few generations, cease to be a Durham, if he gets no food save such as he can pick up in the valleys and hills ; but if carefully fed, he will, of course, do as well here as elsewhere. It is said that the Durham needs suc- culent food ; if so, the blood will soon degenerate on the dry grasses of California. The Devon stock, which has been praised by the importers of it as peculiarly fitted to thrive on our in- digenous grasses, has not found much favor. Our dairy cows are the only ones which are well taken care of; and therefore the Ayrshire blood is really more needed, and likely to be better preserved, than either the Durham or Devon. Roots 222 EESOUECES OP CALIFORN-IA. are seldom cultivated for cattle ; hay, barley, and wlieat-bran, are used for feeding them when kept in the yard. Beeves are never stall-fed in California. § 164. Dairies. — The chief dairy districts of the state are the valleys in the vicinity of the bay of San Francisco. The business is very profitable, but requires a considerable capital. The climate near the coast is very favorable for making butter and cheese. In 1860, according to the assessors' reports, Santa Clara county produced 220,000 lbs. of butter and 300,000 lbs. of cheese; Marin, 226,000 lbs. of butter and 170,000 lbs. of cheese; Sonoma, 220,000 lbs. of butter and 103,000 lbs. of cheese; Sacramento, 148,000 lbs. of butter and 122,000 lbs. of cheese ; Yuba, 92,000 lbs. of butter and 5,745 lbs. of cheese ; and Alameda, 79,000 lbs. of butter and 103,000 lbs. of cheese. § 165. S^Kcnish Horses. — California has about one hundred and fifty thousand horses, of which about one-tliird are Ameii- can ; one-third wild Spanish ; and one-third tame Spanish. The Spanish horses are of the old stock imported, sent early in the sixteenth century from Spain to Mexico, and thence brought to California about eighty years ago. Like the neat cattle, the Spanish horses run wild, and partake, to some extent, of the wild nature. They show their base blood by their colors — mouse color, dull duns of various shades, and calico color, or mixtures of white with red or black, in numerous large spots or blotches, are common ; while chestnut, bright sorrel, blood- bay, and dappled gray, are very rare among them. They are quick, tough, healthy, and unsurpassable for the uses of the rider and the vaquero; but small, lacking in weight, strength, and beauty, and unfitted for the heavy, steady work of the plough, cart, or wagon. They are wanting in the docility, kindly disposition and steadiness of the Avell-bred horse ; and they have little of that kind of sense which leads an American horse to be quiet and gentle, even in circumstances strange to him. For California, as it was in 1845, there were no better horses than the Spanish-Mexican. They have a wonderful tough- AGRICULTURE. 223 ness, and some of their exploits in the way of travelling are un- surpassed in the annals of the turf A number of instances are on record where Californian horses have carried a rider one hundred miles in a day, and that with no food save grass. Sixty miles a day is not an uncommon ride, nor is it considered a, severe one. Fremont, on one occasion, rode four hundred miles in four days, riding different horses, but driving them before bim from the beginning to the end of the journey. More than half of the brood-mares of the state are wild Spanish ; that is, they live entirely m the open plain, are un- broken, and many of them have never been touched save when they vforr. to be branded. They are in bands called manadas^ numb<;^ri^g from thirty to sixty mares, which are under the guidance of one stallion or garanon. He knows every one of his band, kee])s them together, conducts them to what he considers the best pastures, and drives away geldings, stallions, mules, and whatever animals he may dislike. When a vaquero tries to drive the manada into a corral for the purpose of catch- ing some of the band, the garanon will frequently divide them and scatter them about, and render it impossible for the vaquero to get them together ; for while he drives in one place, the stallion is equally busy at another, and the mares fear his teeth and heels as much as the swinging reata of the horseman. The garaiion is usually from five to nine years of age. He guards his manada with the most jealous care. It sometimes hap- pens that one garanon tries to take away a mare from the band of another, and then a fight ensues, in which the weaker has to suffer a severe biting and kicking, and then lose the ob- ject of the battle too. The manada keeps together for year after year, but when it gets too large, the vaquero will divide it and give a portion to the chargeof another garanon. All the mares foal before they are three years old, whereas in the Atlantic States they seldom foal until a year later. They also breed more regularly than elsewhere, for when mares are kept in stables, they frequently pass seasons without breeding. The foals are branded at the age of three or four months, and 224 EESOUP. CES OF CALIFORNIA. are weaned at the a^e of eight or ten months. The fillies con- tinue to run with the nianada, and become part of it. The colts are altered when branded, and continue to run with the manada until they are three or four years of age, Avhen they are broken and put into the caballada^ or herd of broken horses. The Mexicans never broke their mares, and considered it dis- creditable and a mark of great poverty to ride one. § 166. Ilorse-hreakinrj. — Tiie jMexican system of breaking horses is peculiar. They are broken only to the saddle; for horses were never used before wagons by the Spanish-Califor- nians. The horse having ran free all his life, is too wild to be caught without a lasso, or to be approached at iirst while he is on his feet. He is therefore caught by the neck with one reata, by a hind-foot with another, and then thrown down by pulling the reatas in different directions. Avaquero goes to the horse as be lies down and puts d^jaqulma^ or a kind of halter, on his head. The jaquima is provided with a piece of leather, which can be pulled over the eyes so as to blind the horse, but it is first lifted to let him see. The reatas are taken from the neck and leg of the prostrate horse, and a long rope having been fastened to the jaquima, he is allowed to rise. This is the first time he has been haltered and he dislikes the restraint, » but he exerts himself in vain to get loose. After he has tired, himself in vain efforts, the vaquero goes up for the purpose of pulling down the blind. The horse is terrified at so near an approach of a man, and trembles with excitement. If he pulls back hard the vaquero sees there is little danger, and slowly advancing and putting his hand to the blind pulls it down over the horse's eyes. But if the horse stand up, it is probable that he will rear up when the vaquero comes near, or strike at hitn with a fore-foot. Such animals are very dangerous, and are usually allowed to tire themselves by standing without food, or else they are drawn up to a fence or tree, behind which the vaquero can protect himself So soon as the blind is down, the horse is perfectly quiet. Pie can be rubbed, and saddled, and. mounted without a motion. The first thino: after blind- AGRICULTURE. 225 ino- is to put a saddle on liim. It is fastened well, the blind is raised, and the full length of the rope given to him. He does not understand the saddle. It may be a carnivorous beast for all he knows. He is terrified at it. He jumps, and snorts, and kicks, rears and pitches, throws himself down, worries himself out, and falls into an agony of despair. After an hour or so of such work, the vaquero advances again, puts down the blind, and the horse stands trembling with fear and exhaus- tion. He is now to be ridden. The rope is fastened under the chin, so that it can be used for a bridle-rein ; the horse's ears are pushed down under the upper part of the jaquima, so that he shall be deaf as well as blind; the saddle-girth is tightened, and the rider mounts. Over the saddle he has a second girth, which is loose enough to allow him to get the point of his knee, bent at right angles, under it. This girth ties him upon the horse. The more he presses the knee outward, the tighter the girth holds him ; whereas by turning his knees inward and straight- ening his legs, he can be free in an instant. Having put his knees under the girth (he does not care for the stirrups and cannot use them) he reaches forward, takes the ears out from under the jaquima, and raises the blind. The horse, as soon as he sees the man on his back, is stricken with a new terror. He immediately commences to jump stiff-legged. He springs up into the air and comes down on his fore-feet with his legs stiff. This is the way in which horses try to shake off panthers, and they resort to the same method with men. The shock would be severe if the man were not tied down to the saddle, but he moves with the horse and is not hurt with the shock. Some- times a horse will jump thus for hour after hour, and the rider is very well satisfied, for there is no danger in the jumping, and it is very tiresome to the animal. Some horses, after jumping for a few minutes, will commence to run. To this the rider makes no opposition, but practises the horse with the reins to accustom him to guidance. The most dangerous horses are those which rear up and fall backward. In such case the vaquero must be ready to throw off the girth from his knees, 10* 226 EESOTJRCES OF CALITOKNIA. and alight upon his feet as the horse fells. After riding for a couple of hours, the vaquero reaches forward, pushes the blind down over the horse's eyes and dismounts. To dismount with- out first putting down the blind would be very dangerous, for the horse would probably kick him. He takes off the saddle, hoists the blind, ties him to a fence or a tree with his head up, and gives him neither food nor water. The next morning he is very stiff and hungry. The vaquero does not feed him, but pulls down the blind, puts on the saddle, mounts him again, and the scenes of the previous day are re-enacted, though the jumping is less furious. After a couple of hours of exercise, the horse is tied where he can get water and grass. Every day he is ridden. In five or six days he quits jumping. In three months the blind is laid aside. In four months a bit is put in his mouth. This is strange to him, and he jumps stiff-legged. If the first bit used is American, he will jump again when the harsher Spanish bit is used. When any thing is wrong he jumps stiff-legged. During the first month or two his nose will be very sore where the jaquima or halter crosses it, caused by the pulling of the halter in holding and guiding the animal. At the end of a couple of months he learns to follow the guidance of the jaquima almost as readily as afterward the bit. After he has been ridden daily for six months, he has become tame and quiet, and he commences to fatten up again ; for during the first three or four weeks he worries himself so much, with his vain plungings, that he loses flesh rapidly. The Californian horse, when once broken, is kindly in disposition. He rarely bites or kicks, no matter how roughly he may be used. After having been broken to the saddle, he must be taught the uses of the reata. The vaquero always carries his reata with him, and the horse soon learns to see it swinging about the rider's head. The reata is first thrown at small calves and then at larger ones, and the horse gradually learns that he can best hold a lassoed animal by presenting his head toward it, and bracing himself back with his fore-feet. The reata is fast- ened to the horn of a saddle, strong enough to hold a bulL AGKICTJLTUEE, 22 1 The horse learns to watch the reata ; if it catches, he slackens his pace, or stops suddenly ; if it does not catch, he continues al full speed, while the vaquero pulls up the reata and prepares to throw it again. The saddle and bridle are both pecuhar, and necessary to the trade of the vaquero. The saddle-tree, or fuste^ is made of four pieces of wood, two of which are longi- tudinal and rest on the sides of the horse ; one forms a high back ; and the fourth is a fork, which rises in a large strong horn. The pieces are strongly fastened together, and the whole framework is covered with wet rawhide, which shrinks when dry, and contributes much to its strength. A good fuste is stout enough to hold the strongest bull. The girth is four inches wide, and is made of a number of little ropes of horse- hair, connecting two iron rings four inches in diameter. One of these .rings is fastened on the right side of the saddle, by straps running over the front and back of the fuste ; and a similar ring is fastened in like manner on the left side of the fuste. In this latter ring is a rawhide strap three feet long. When the saddle is to be fastened, this strap runs through the ring at the loose end of the girth, then through the upper ring, then down to the girth ring again ; and the vaquero pulls, and usually draws so tightly that the wide girth cuts into the horse's belly and evidently displaces its contents. When a vaquero is preparing for a day of lassoing, there is no danger that the saddle will slip. The girth has no buckle about it, and is made wide to give it strength and to prevent it from hurting the horse. It is placed farther back than in American saddles, and rarely cuts the skin, just behind the fore-legs. Sometimes in lassoing, the animal caught will get off sideways from the horse, and the saddle must be so firmly in its place, that it cannot move ; and sometimes the vaquero will drop his reata after having caught his cow or horse, and then while his horse is going at full speed he must reach down, supporting himself with one hand on the horn of the saddle and with the other seize the reata. For such feats, the girth must not bo loose. The stirrups are of wood, about three inches wide, and 228 RESOURCES OF CALIFORNIA. are covered in front with pieces of thick leather, called tapW' deras^ which prevent the feet from slipping through. The fiiste is usually covered by large flaps of leather called mochilas, and along the stirrup-straps are pieces of leather called suda- deras^ to protect the legs of the rider from the sweat of the horse's side. Cruppers and martingales are never used by the Spanish-Californians. The bridle is so made that a hard pull ,on the rein hurts the horse, and a severe jerk will throw him back on his haunches. The bit has an arm projecting about two inches up in the mouth. On ordinary occasions this arm lies flat on the tongue, but when the rein is pulled it rises and presses against the roof of the mouth. The slightest pull, therefore, on a Spanish bridle is felt by the horse, and he will stop instantaneously, though at full speed, if the reins be jerked severely. It may be cruel to the horse, but it is very conve- nient to the rider, and necessary to the vaquei'o. The common gait of the Californian horse under the saddle is the gallop. He never paces or racks, and rarely tries a sharp trot, but rests himself with a walk or a slow trot. His gallop has an easy motion which does not tire the rider in fifty miles. He has an excellent speed for a race of a quarter a mile, but he cannot run two-mile heats with the thoroughbred, though for a gallop of a hundred miles he has probably no superior. Many of the Californian horses have of late years been bro- ken to the wagon and the plough, and they do very well for farm work, though not equal to American horses. § 167. Blood-horses. — The American horses, that is the com- mon stock of horses brought from the Atlantic States within the last twelve years, and their oftspring, are large, fine animals, not so healthy and tough as the Californian horses, but larger, more active, stronger and more handsome in shape and color. A large number of stallions and mares of fine blood have been imported, including about fifty thoroughbreds or English racers, two dozen Morgans or American trotters, and a dozen Clydesdale and Flemish, or heavy cart and truck horses. Some of these horses are valued as high as ten thousand dollars AGKICULTURE. 229 apiece. The Clydesdale and Flemish are considered the most valuable for crossing with the Californian mares, the offspring being lai'ge, strong farm-horses, worth twice as much in the market as the pure Californian. The thoroughbred horses in California are of the purest blood, and some of them have few superiors in speed in any country. § 168. 3£ules. — Nearly all the farm work of California, where draught animals are necessary, is done with horses. Mules are too dear and oxen are too slow. A great number of mules and horses are used in packing merchandise in those districts where there are no good wagon-roads. For the or- dinary uses of the farm the mule is preferable to the horse, being longer-lived, more healthy, not so much injured physi- cally or morally by ill-treatment, and contented Avith much cheaper and simpler food. But the mule is not considered handsome, and the small farmer wants a horse which he can ride, and with which he can take his fixmily out, so he never gets a mule. Mules are now used on very few farms, but I think they will gradually gain in fovor. Few mules are bred in the state at present, but there are some excellent jacks in Contra Costa county and in the San Joaquin valley. § 169. Camels. — Some camels have been introduced into California, but they are as yet few in number, and have been here but a short time. Our experience with them is therefore small, and we do not know what value they are to have in the future. They a^-e healthy, increase, thrive on our wild pas- tures, are strong and active, climb our rugged mountains as well as horses or mules, carry loads of one thousand pounds each, go three or four days at a time without water, and are readily managed ; but they have not been tried in a regular business way, and such trial is necessary before we can tell what they are to be. § 170. Sheep. — The climate of California is peculinrly favor- able to the growth, increase, and health of the sheep. Our mild winters permit them to grow throughout tlie year; and it is an accepted principle : mong those familiar with the sub- 230 EESOUECES OF CALIFOKNIA. ject, tiiat a sheep, born and bred in California, is, at two years of age, usually as large and heavy as one of three years, born and bred in the Atlantic States. The ewes produce twins and triplets more frequently here than east of the Kocky Moun- tains. The health of the herds is better. 'No fatal disease has ever prevailed to any serious extent. The " scab" exists in many herds, but in a mild form, and few have died of it. It is the general opinion of sheep-breeders that the sheep bred in Cahfornia will produce more wool than those of other states. The heaviest unwashed fleece on record, is that of " Grizzly," a French Merino buck. It was fourteen months old, weighed forty-two pounds, and was sheared by Flint, Bixby & Co., in Monterey county, in 1859. Sheep in California are never kept under shelter, and except a few of fine blood, seldom get any food save such as they can pick up on the open hills and plains. Sometimes lambs are lost with cold, but this is very rare when they are well managed. At night the herds are driven into corrals or pens, to protect them against the coyotes, and to keep them from being lost. On the large sheep ranches, one herdsman is em- ployed for a thousand sheep. There are a few shepherd-dogs in the state, some brought from Australia, others from Scot- land. The word " corral" is understood by these dogs, and when they hear it, they immediately drive the herd to the corral. At the sight of a wolf, they hastily collect the sheep into a dense body, with their tails out and the lambs in the centre. If a sheep turns his head out, the dog bites his knees and makes him turn about. The dog seems to understand that the wolf cannot do much harm by biting the rump of a sheep, but would soon kill it after catching its throat. In most other sheep countries, tlie sheep-breeder is at great disadvantages as compared with California ; the land is dear ; it must be cultivated ; the sheep must be fed by hand every day during a considerable part of the year ; the herds must be under shelter in the winter ; four or five men are required, on an average, to attend to a thousand sheep ; the herds are not AGKICULTURE. 231 SO healthy, do not increase so rapidly, do not grow so large within the first two years, and do not produce so much wool. The land of the sheep ranches in California is not worth more than five dollars per acre, on an average probably not more than three dollars. It follows that sheep-breeding should be very profitable here, and so it is. The ewes, when properly taken cai'e of, have lambs before they are a year old — increase one hundred per cent, every year. The cost of keeping large herds is variously estimated from thirty-seven to fifty cents per head annually, exclusive of the interest of the land used for pasturage. The wool of a good sheej) will pay twice the cost of keeping it ; and the wool and lamb together, of a fine- blood ewe, are worth eight or ten times the cost. It is the present custom to sell the wethers for mutton when a year old, but this is bad policy, save with the poorest sheep. The old missions had large herds of sheep, but after the management of those large establislnnents was taken from the priests and given to civil officers, in 1833, the sheep were neglected and most of them were killed. Twenty years later very few were left in the state, but there was a demand for mutton, so large herds were driven from New Mexico. These were a very poor stock, but they were for a long time the only sheep that could be had, and they now form the great majority of the sheep in the state. The first attempt to breed sheep as an exclusive business in California, since the Ameri- can conquest, was commenced in 1853, by a poor man who had nothing save nine hundred ewes ; and they increased so rapidly and proved so profitable, that now, if report be true, he has ten thousand sheep, sixteen thousand acres of land, and other property to the value of one hundred thousand dollars. Within the last three years many sheep of fine blood have been imported, and these will gradually swallow up the Mexican stock. The imported kinds are American, Southdown, Aus- tralian Merino, Fiench Merino, and Spanish Merino. Of the two latter varieties there are few save bucks. The prices of sheep fluctuate, but the relative prices of the different breeds 232 KESOUECES OF CALIFORNIA. remain about the same. Thus when a Mexican ewe is worth about three dolkirs, an American is worth five dollars, a half- Merino six dollars, a Southdown six dollars, and an Australian Merino twelve dollars. The Mexican sheep produces on an average two pounds of wool per year, worth from five to seven cents per pound ; the American four pounds, worth from fifteen to twenty cents ; the half-Merino six pounds, worth from eighteen to twenty-four cents; the Southdown five pounds, worth twenty or twenty-one cents; the Australian Merino seven pounds, worth twenty or twenty-one cents. These weights indicate the weights of the unwashed fleeces, and the prices paid in this market for unwashed wool. The Californian wool, especially that grown in the southern part of the state, is filled with grease, dust, and sand. In one case, a fleece weighing sixteen pounds was reduced by washing to six ]^ounds. The finer the wool, and the forther south it is grown, the greater the proportion of dirt. The wool grown in the northern part of the Sacramento valley, is cleaner than that of Alameda county, and that of the latter place is superior to the wool of San Luis Obispo. There are a few Chinese sheep in the state, and much value was for a time attached to them, because the ewes very frequently produce triplets, but it re- quires a good ewe to suckle two lambs well, and twins are sufliciently abundant among American sheep. Sheep-growers are divided in opinion as to whether the Fi-ench or Spanish Merino be the best sheep for the state. The French Merino grows large, and averages more wool to the sheep than any other kind, but it is said that the Spanish Mei'ino, though smaller, will produce more wool to the acre. About a thou- sand sheep are kept in a herd. One sheep-owner in Monterey county has 30,000 head ; and others have 15,000 and 20,000 head each. The largest sheep county is Monterey, which has about 150,000; Solano has nearly as many, and after these come Los Angeles, San Bernardino, and San Luis Obispo. There are about 900,000 sheep in the state, and their number is rapidly increasing. One of the drawbacks of wool-growing AG lil CU LTU KE. 233 in California is, that in tlie summer the wool gets full of the little burs of the bur-clover, which gives much trouble in wash- ing and carding. By sheering early this trouble is to some extent avoided. Of course the sheep gi'ow lean in the late f:il!, as do the horses and neat cattle, and some of tliem die of starvation. The same remarks may apply to high-bk)od sheep as to other high-blood animals — they must degenerate if they get no cultivated food ; but the stock may be kept up by cross- ing with high-fed bucks of pure blood. § I7l. Swine. — Swine are not favorite animals in Califor- nia. They increase rapidly and are healthy, and their meat commands a high price, but they do not thrive upon the dry- pastures ; they are not permitted to run at large in many coun- ties ; the mast is scanty in the agricultural counties, and grain suital)!e for feed is dear. It is probable that in a few years gi'eat numbers of swine will be bred in the tules, the roots of wiiich they like to eat ; but the tule-lands at present are in wide undivided tracts, and the swine which have access to them soon get lost. The present number of swine in the state is about six hundred thousand. § 172. Poultry. — Poultry command very high prices in this state, but all attempts to breed them on a large scale, have proved unprofitable. Hens are worth from fifty to seventy- five cents each, and eggs from twenty-five to fifty cents per dozen. Chickens are healthy and increase rapidly in small poultry-yards or farms ; but when more than five hundred are collected a fatal epidemic appears, and they die off. The dis- ease seems to be a kind of apoplexy, for it attacks the fattest chickens, and they die suddenly. One large hennery, on the French plan, has been established about eight miles from Oak- land, and it contains one thousand five hundred hens, with accommodations for five thousand. The poultry-yard covers four acres of ground, and one acre of it is separated from the remainder. The hens lay in the lower story of a frame house, which is open on one side. The nests are in a long trough, a foot square, open on top, and separated into nests by partitions. 234 EESOFRCES OF CALIFOENIA. Each nest has some hay in it and a mock egg of porcelain. Several times in the course of a day, the eggs are taken out and placed in a covered box near at hand. Four or five hens may use the same nest in the course of a day, and if the eggs were left in the nest the warmth might start the development of the chick, and injure the egg for either hatching or eating. It is considered bad policy to let a hen sit on eggs while lay- ing, even if she is to hatch them herself, for some will be far- ther advanced in incubation than others, and then the propor- tion of loss will be great. Over the laying department is the roosting place, which is eighteen feet high, and his the perches so fixed that the droppings of one hen do not fall on another A stairway leads up from the ground to the roosting chamber In the lower story of another house is the hatching dejDart- ment, with nests for six hundred hens. The nests are about a foot square, with a door in front, opening on a level with the floor. They are numbered and divided into sections, each of which has one door, and has hens which commenced sitting at the same date. The hens are fed by sections ; ten, twenty or thirty being let out at a time, and called to eat. When first called they do not understand it, and after they have eaten, they have difficulty in finding their places ; but in three or four days they come out immediately as soon as the door is opened, and when the signal for closing is given, they go to their places without the least confusion. About a dozen eggs, usually not more than four, and never more than ten days old, are given to each sitting hen, and of this dozen, nine or ten are hatched on an average. Every nest has snuff" in the bottom of it to keep out the lice. When the hen has hatched out her bi'ood, she and they are transferred to the "young-chick room," over the hatching room, where every hen is put in a pen. During the first twenty-four hours the little chicks get nothing to eat ; then they are fed twice on fine bread, after that on boiled rice and corn-meal. They are fed four times a day. When five days old, the chicks, with their mother, are placed in the smaller enclosure of the poultry-yard, which has several ageicultijRe. 235 streams of clear water running through it, bushes andmustard- phmts for shade, and boxes into which the hens can retire for protection against the cokl and rain. AVhen the young brood enters the yard, the oldei- occupants, or some of them, make war on it, and one chick in a dozen is slain in these hostilities. After the hen has proved by fighting her right to be there, peace is restored, and she and her little ones are ready to make war on any subsequent intruders. After the chickens are three months old, they are turned into the large yard, where tliey have to struggle for their food and lives, with all the old hens and cocks on the place. In the large yard the chickens are fed twice a day, and four ounces to each chicken per day. The food is wheat, rice, oats, barley, raw meat, cabbage-leaves, sorrel, chalk, oyster-shells, and green mustard. Regularity in the time of feeding is considered a matter of much import- ance. There should be one cock to a dozen hens. The hens commence laying when about eight months old and lay most in their second year. They will continue laying till their fifth or sixth year, but they are usually killed about the end of the fourth year. Hens that eat eggs and that crow are killed. Hens which want to sit when their services are not needed in that way, are shut up in the callaboose, kept there one or two days, with no food save green vegetables, ducked several times in cold water and then let out cured. In eight or ten days they are ready to commence laying again. A hen will lay fifteen or eighteen eggs before wanting to sit. One man near Oakland, devotes himself entirely to the busi- ness of breeding rabbits, and according to rumor, finds it very profitable. Goats, pigeons, and pheasants are bred in California, but on only a small scale. § 1*73. Bees. — There were no bees in California until witliin the last seven years, and it was supposed they could not live here, because of the dryness of the vegetation during the last half of the year ; but for these insects, as for larger animals, it was found on trial, that our climate is peculiarly favorable, 236 RESOURCES OF CALIEOENIA. and that they thrive better here than east of the mountains. A good hive here will make two hundred pounds of honey, or may be made to produce twenty swarms in a season, an in- crease ten times as great, and a production of honey five times as large as that in the Eastern States. Mr. H. Hamilton, a bee-keeper of Stockton, reports that he had thirty-five swarms of bees on the first of February, 1860 ; and by the first of October, they had increased to five hundred hives, and pro- duced twenty thousand and seventy-five pounds of honey ; a production said to be witliout parallel. Bees are not idle during six months of the year, as in New York, but busy during nine or ten months. They find their food in wild and cultivated flowers, in the blossoms of manzanita bushes, fruit-trees, grasses, clovers, and grains, in grapes, fruits, and honey-dew. They ^seem to thrive in the driest portions of the state, where there are no cultivated fields and no flowers or green herbage. They are very fond of apricots, which they eat in places where the skin has been previously cut through by bugs. When the latter have made a hole, the bees come and eat side by side with the bugs, which are of the "lady-bug" kind, and other similar species. Many of the bees lose their lives in conse- quence of their fondness for the apricot. Either they eat too much, or they eat the meat after it has passed into the alco- holic fermentation ; but whether intoxicated or surfeited, they are unable to get home, and they perish during the night. In places where the honey-dew is abundant, especially in the mountains on the eastern border of the Tulare valley, the bees make honey very rapidly. When the food for bees was becomins: scarce in the midsummer of 1860, in the Santa Clara valley, a man owning seventy hives sent them to the vicinity of Yisalia, so that they could get honey-dew. Indeed it is the custom of several bee-keepers in California, to move their bees about from place to place, according to the pasture and the season. Hitherto little honey has been sold in the market, the chief object of bee-keepers being to produce swarms, which for a time were worth one hundred dollars each This busi- AGEICULTUKE. CS7 ness yielded so large a profit that a dozen men devoted them- selves to it exclusively, and some of them, who commenced five years ago with only three or four hives, now have com- fortable f( rtunes. The liives have increased so rapidly, how- ever, that they have fallen greatly in value, and are now worth from ten to thirty dollars each ; and honey, M^hich is worth one dollar per pound, will come into the market. The honey made in the mountains is very similar in quality to that of the East- ern sta^yfs ; that made in the valleys is not so good. Many swarm.fl. have gone off and found homes for themselves in the woods, so it is not rare to find " bee-trees." Most of the bees in th'i Sacramento basin during 1861, were destroyed by the floo'J of 1862. § 1 74. Silkicorms. — A few silkworms have been hatched in California, and have been found to thrive extremely well, but the high price of labor has prevented any extensive experi- ment in the production of silk. Our climate is very favorable to them in three respects, equability of temperature, exemption from electrical convulsions, and dryness in summer. The silk- worms should be kept at a temperature of about 75° Fahren- heit, and this is very near the summer temperature of some of the valleys near the coast. Extreme heat and extreme cold are both very prejudicial to them. A considerable pi'oportion of them will die if the thermometer falls to 45° or rises to 100° ; thunderstorms kill a large portion of the worms every year in France, Italy, and China ; in California such storms are un- known. In all the countries where silk is now produced ex- tensively, there are showers which wet the mulberi-y leaves, and this moisture gives a diarrhoea to the worms whereby many are killed. These are important advantages, and may enable us to compete soon with Europe and China in the 2:)ro- duction of silk. Note. — I owe acknowledgments for information about grain to J. W. Os- born, of Napa; about fruit to A. A. Cohen, of Alameda; about the grape to Charles Kohler; about the orange to John Frohling; and about the quality of wheat from different districts to Isaac Friedlander, of San Francisco. !38 KESOUECES OF CALIFORNIA. CHAPTER VIII. MINING. §175. Chief Lidustry. — Mining is the chief industry of California. It employs more men and pays larger average wages, than any other branch of physical labor. Although it has been gradually decreasing in the amount of its production, in the profits to the individuals engaged in it, and in its rela- tive importance in the business of the state, it is yet and will long continue to be the largest source of our wealth, and the basis to support the other kinds of occupation. § 176. 3Ietals obtained. — Our mines now wrought are of gold, silver, quicksilver, copper, and coal. Ores of tin, lead, and antimony in large veins, beds of sulphur, alum, and as- phaltum ; lakes of borax and springs of sulphate of magnesia, are also found in the state, but they are not wrought at the present time, though they will probably all become valuable in a few years. Platinum, iridium, and osmium are obtained with the gold in some of the placer mines, but are never found alone, nor are they ever the main object sought by the miner. The annual yield of our gold mines is about forty millions of dollars, of our quicksilver two millions of dollars. Our silver, copper, and coal mines have been opened within a year, and their value is yet unknown. All our other mining is of little importance as compared with the gold. § 177. Gold Mines. — Our gold mines are divided into pla- cer and quartz. In the former, the metal is found imbedded in layers of earthy matter, such as clay, sand, and gravel ; in the latter it is incased in veins of rock. The methods of mining must be adapted to the size of the particles of gold, and the MINING. 239 nature of the material in which they are found. In placer mining, the earthy matter containing the gold, called the " pay- dirt," is washed in water, which dissolves the clay and carries it off in solution, and the current sweeps away the sand, gravel, and stones, while the gold, by reason of the higher specific gravity, remains in the channel or is caught with quicksilver. In quartz mining the auriferous rock is ground to a, very fine powder, the gold in which is caught in quicksilver, or on the rough surface of a blanket, over which the fine material is borne by a stream of water. About two-thirds of our gold is obtained from the placers, and one-third from the quartz. A mine is defined and generally understood to mean " a subterraneous work or excavation for obtaining metals, metallic ores or mineral substances ;" but this definition does not apply to our placer mines, which are places where gold is taken from diluvial or alluvial deposits. Most of the work is not subter- raneous ; it is done in the full light of day. In some of the claims the pay-dirt lies within two feet of the surface ; in others it lies much deeper, but all the superincumbent matter is swept away. "Water is the great agent of the placer miner ; it is the ele- ment of his power ; its amount is the measure of his work, and its cost is the measure of his profit. With an abundance of water he can wash every thing ; without water he can do little or nothing. Placer mining is almost entirely mechanical, and of such a kind that no accuracy of workmanship or scien- tific or literary education is necessary to mastery in it. Amal- gamation is a chemical process it is true, but it is so simple that after a few days' experience, the rudest laborer will man- age it as well as the most thorough chemist. It is impossible to ascertain the amount of gold which has been taken from the mines of California. Records have been kept of the sums manifested at the San Francisco Custom House, for exportation, and deposited for coinage in the mints of the United States ; and there is also some knowledge of the amounts sent in bars and dust to England ; but we have 240 RESOURCES OF CALIFORNIA. no account of the sums carried by passengers to foreign coun- tries and coined elsewhere than at London, or used as jewelry, or of the amount now in circulation in this state. According to the books of the custom-house of San Francisco, the sums manifested for export were as follows : In 1840, $4,921,250; in 1850, |2'7,676,346 ; in 1851, $42,- 582,695; in 1852, $46,586,134 ; in 1853, $57,331,034 ; in 1854, $51,328,653; in 1855, $45,182,631 ; in 1856, $48,887,543; in 1857, $48,976,697 ; in 1858, $47,548,025 ; in 1859, $47,640,462 ; in 1860, $42,303,345; in 1861, $40,639,089; a total of $551,603,- 904 in twelve years. The exportation of gold commenced in 1848, but we have no record of the sums sent aw^ay in that year. Previous to 1854 very large sums were carried away by pnssengers, who gave no statement at the custom-house ; since that year, the manifests show the exportation correctly within a few millions. I am entirely satisfied that the total gold yield of California has been not less than seven hundred millions of dollars ; but I have not room here to state the reasons for this opinion. My estimate is considerably less than that of most business men of the state, and less than that made by Hunt's Merchants' Magazine. There Avas undoubtedly a regular increase in the annual yield of the mines from 1848 to the end of 1853 ; and there has been a gradual decrease since the beginning of 1854 — a decrease perhaps not very regular but still certain. Since 1854 considerable sums exported from San Francisco and in- cluded in our tables, came from mines beyond the limits of California, such as the mines in Southern Oregon, in the east- ern part of Washington Territory, in British Columbia, auil in Nevada Territory ; and while the Californian gold yield has been decreasing, these extraneous sui>plies have been incre: s- ing. Several millions must be deducted from the annual shipments since 1858, for foreign gold. The gold yield wii undoubtedly continue to fill, but to what point and at what rate no one can knoAV. I believe that in 1870, the yield will not exceed thirtv millions of dollars. MINTING. 241 § ITS. Placer M'mes. — Placer mines are divided into many classifications. The first and most important is into deep and shallow. In the former the pay-dirt is found deep, twenty feet or more beneath the surface ; in the latter, near the sur- face. The shallow or surface diggings are chiefly found in the beds of ravines and gullies, in the bars of rivers, and in shal- low flats ; the deep diggings are in hills and deep flats. The pay-dirt is usually covered by layers of barren dirt, which is sometimes washed, and sometimes left undisturbed, while the pay-diit is taken out from beneath it through tunnels or shafts. So far as our present information goes, we have reason to be- lieve that no gold country ever possessed so large an extent of paying placer mines, with the pay-dirt so near the surface, and with so many facilities for working them as California. In Australia the diggings nre very deep and spotted, that is, the gold is unevenly distributed, and the supply of water for mining is scanty. In Siberia the winter is terribly cold during six months of the year. In Brazil the diggings were not so extensive nor so rich as in this state. Here we have numerous large streams coming down through the mining districts, very large bodies of pay-dirt, and a mild climate. After dividing placers into deep and shallow, the next clas- sification will be according to their topographical position, as into hill, flat, bench, bar, river-bed, ancient river-bed, and gulch mines. Hill diggings are tliose where the pay-dirt is in or under a hill. Flat diggings are in a flat. Bench dig- gings are in a " bench" or narrow table on the side of a hill a- ove a river. Benches of this kind are not uncommon in California, and they often indicate the place where the stream ran in some very remote age. Bars are low collections of s.uid an