HISTORY VERMONT NATURAL, CIVIL AND STATISTICAL, ~n ~~tgre rart", WITHI A NEW MIAP OF TIE STATE, AND 200 ENGRAVINGS. BY ZADOCK THOMPSON, Inb tt t rlingt[t: PUBLISHED FOR THE AUTHOR, BY CHAUNCEY GOODRICH. 1842. Entered according to act of Congress, in the year 1842, by ZADOCK THOMPSON, in the Clerk's office of the District Court, for the District of Vermont. PREFACE. EVER since the publication of his Gazetteer of Vermont in 1824, the author has contemplated a larger work, which should embrace, not only the Gazetteer, but a general History of the state, both Natural and Civil. He accordingly commenced collecting and laying aside materials for that purpose, and during the four years last past, he has devoted the greater part of his time to the preparation and publication of the work. His means and facilities for the researches and investigations in which he has been engaged, have not been such as he could have wished; but he has endeavored to improve these, such as they were, to the best advantage; and now, through the blessing of a kind Providence, he is enabled to lay before his fellow citizens the result of his labors. That his work, embracing, as it does, subjects so multifarious and dissimilar, has many imperfections, he is fully sensible; but he ventures to indulge the hope that it may be found to answer the reasonable expectations of all, and especially of those who can duly appreciate the labor and difficulties of a work of this kind. For convenience in printing, the three several parts into which the work is divided, have been separately paged, and, to the two first parts, separate indices have been prepared. On account of the alphabetical arrangement of the third part, an index to that was thought to be unnecessary. Part First is devoted to the Natural History of the state, and is almost wholly the result of original investigations. The only general account of our Natural History, which has hitherto been published, is that contained in Dr. Williams' History. Though highly interesting and useful, that account was prepared at a period and under circumstances which necessarily rendered it imperfect, and in many respects erroneous. Misled by the vulgar names, and depending upon the representations of the hunters, he has in, perhaps, a majority of cases, applied the scientific names of European animals to ours, which, though bearing considerable resemblance to them, are specifically distinct. The first chapter of this part contains the result of several years' meteorological observations made by the author at Burlington, and also of observations made at several other places within the state. The author's views will be found here, respecting the formation of ice, earthquakes, the cause of the coldness of our climate compared with that of Europe, &e. The descriptions in the four following chapters have been nearly all made by the author, directly from Vermont animals. In some cases, where Vermont specimens could not be procured, and the animal was known to exist in the state, a borrowed description has been introduced, but in all such cases the source from which it was derived has been indicated, by placing the name of the author at the close of the description. In making out his account of the Birds, he was much assisted by a list of Vermont Birds, kindly furnished by Dr. THOMAS M. BREWER, of Boston; and in determining several species of Reptiles and Fishes, he has been kindly aided by Dr. D. H. STORER, also of Boston. For the full descriptions of our Molluscous Animals, in the sixth chapter, he is indebted to the kindness of Prof. C. B. ADAMS, of Middlebury College, and the full and excellent Catalogue of Vermont Plants has been P REFACE. generously prepared for this work by WILLIAM OAKES, Esq., of Ipswich, Mass., who ranks among the first botanists in the country. The eighth chapter remains to be written after a Geological Survey of the state shall have been effected. Part Second contains a connected Civil History of the state from the first discovery of its territory down to the year 1842. That portion of the history, which precedes the admission of Vermont into the Union, being of a very peculiar and interesting character, has been treated more fully than in any previous history of the state. The materials for this portion have been principally derived from Dr. WILLIAMS' History, the Hon. WILLIAM SLADE'S Vermont State Papers, and a valuable series of papers recently published at Bennington, in the State Banner, under the title of Historical Readings, and understood to be from the pen of the Hon. HILAND HALL, one of our Representatives in Congress. Of these works he has made free use, which he would here publicly acknowledge, as he has often copied their language as well as their facts, and has not been particular to disfigure his pages with quotation marks. From the admission of Vermont into the Union, only a rapid sketch of the politi~al history of the state has been given; but to compensate for deficiencies here, he has added, in separate chapters, the history of the political, the literary, and the religious institutions, with a closing chapter upon the state of society. The assistance, which he has received, in the preparation of these, will be found duly acknowledged in the progress of the work. Part Third is, to a considerable extent, a reprint of the author's Gazetteer, published in 1824. Many additions and corrections have, however, been introduced, together with the most important statistics collected at the last census, and the history of the towns has, in most cases, been brought down to the year 1841. The JMap has been prepared with much care, and will, it is believed, be found more correct than any map of the state hitherto published. It is engraved upon steel, and that, and all the other engravings have been executed expressly for this work, by Mr. J. H. HILLS, of Burlington, and in a manner, which we think highly creditable to him as an artist. From the beginning of his undertaking, the author has endeavored to keep two objects constantly in view;-first, to embrace in his work everything of special importance relative to the Natural and Civil History of the state; and, secondly, to publish it in so condensed and cheap a form as to place it within the reach of all the families in the state. In his endeavor to effect these objects he has spared neither labor, nor expense; nor has he had any special regard to a pecuniary recompense from the sale of his book, as will appear from the fact that he has added more than 150 pages to the aniount required in order to fulfil the conditions of his prospectus the whole number of pages being 656, and the number promised only 500. His work, such as it is, he now submits to his fellow citizens. If it shall answer the purposes for which he has designed it, the author will expect his highest reward in the reflection that he has not added to the number of useless books. Burlington, Oct. 3, 1842. THOMPSON'S VERMONT. NATURAL HISTORY OF VERMONT. CHAPTER TI DESCRIPTIVE AND PHYSICAL GEOGRAPHY OF VERMONT. SECTION 1. Vermont is in the township of Canaan, Situation Boundaries, Extent and Diis and the most western in the township of Situation, Boudaries Etent and Diis-Addison. This state lies nearly in the middle of the north temperate zone. The Situation.-Vermont is situated in the longest day at the south line of the state, northwestern corner of New England, is 15h. 9m. 9s., and at the north line, 15h. and lies between the parallels of 42~ 44' 25m. 50s. and 4.5~ of north latitude, and between 30 Boundaries.-Vermont is bounded on 35' and 5~ 29' of east longitude from the the north by the province of Canada, on Capitol of the United States at Washing- the east by New Hampshire, on the south ton, or between 71~ 33' and 73Q 25' of by. Massachusetts, and on the west by west longitude from Greenwich Observa- New York. The north line of the state tory.* The most eastern extremity of runs upon the parallel of latitude 45' north. This line was first surveyed by * Where it is not otherwise specified, the longi- north. This line was first surveyed by tudes given in this work are in all cases reckoned commissioners appointed by the provinces from the Capitol of the United States. The longi- of New York and Canada, in the year tude of the Capitol from Greenwich, according to 1767. It was afterwards run, but very the most recent observations, is 77~ 1J 48/'. It is erroneousl by I. Collins and I. Carden. very much to be lamented that the longitude of erroneously, by I. Collns and I Caden places in Vermont is so imperfectly known. We in 1772. In 1806, Dr. Samuel Williams are not aware that a single point within the state made some observations with the view of has been determined with any pretensions to ac- ascertaining thetruenorthlineofthestate curacy. True, a few solar eclipses have been ob- e served and some calculations have been made, for and still further observations were made in the purpose of deducing from them the longitude of 1818, by Messrs. Hassler and Tiarks, surthe places; but the only observations within our veyors under the treaty of Ghent. Acknowledge, which have hitherto been regarded as entitled to any degree of confidence, were those of thelogitude oftheUniversity. But the opportuthe solar eclipse of 1811, made at Burlington by Prof. nity proved unfavorable, the sun being hid by clouds James Dean and John Johnson, Esq., and at Rut- durin the greater part of the eclipse. Of the beland by Dr. Williams. The longitude of the Uni- ginning he had a tolerable observation, and from this versity Dof Vermontc, deduced from these3 o tservat- alone he carefully calculated the longitude by Dr. tions by Dr. Bowditch, was 73~ 14' 34", and of Rut- Bowditclis precepts, and the result was 73~ 10, 36" observatory, an in accordance27 with thesfrom Greenwich thfor the longitude of the University, or about 4m. less observatory, anti in accordance with these has the was obtained from the preceding observations longitude of the different parts of the state been and, as he is inclined, from other circumstances, to laid down upon our maps. In 1838,the author pre-think it as near an approximation to the true lmpared, with much care, for observing the large solar gitude as any yet obtained, he has adopted it in this eclipse of that year, for the purpose of determining work. PT. I. I 52 NATURAL HISTORY OF VERMONT. PAlx IL BOUNDARIES. EXTENT. —AREA, DIVISIONS. cording to the latter, the 45th parallel lies former being about 175 miles, and the lata little to the southward of the line pre- ter, following the course of the Connectiviously established, but it is not yet finally cut, 215 miles." The state is divided into settled. The eastern boundary was es- two equal parts by the parallel of 44d. tablished by a decree of George IlI, July 9m. north latitude, and also by the meri20th, 1764, which declared the western dian in 4d. 19m. of east longitude. These bank of the Connecticut river to be the two lines intersect each other near the western boundary of New Hampshire. western line of Northfield, and about 10 The southern boundary is derived from miles south westerly from Montpelier, and a royal decree of March 4th, 1740, and the point of intersection is the geographiwas surveyed by Richard Hazen, in Feb- cal centre of the state. ruary and March, 1741. This line, which Divisions.-The Green Mountains exwas the divisionalline between Massachu- tend quite through the state from south setts and New Hampshire, was to run due to north, and, following the western range, west from a point three miles to the north- divide it into two very nearly equal parts. ward of Patucket falls, till it reached the These form the only natural division, province of New York. It was run by with the exception of the waters of lake the compass, and ten degrees allowed for Champlain, which divide the county of westerly variation of the magnetic needle. Grand Isle from the counties of Franklin This being too great an allowance, the and Chittenden, and the several islands line crossed the Connecticut river 2' which compose that county, from each 57" to the northward of a due west line. other, and from the main land. For civil In consequence of this error, New Hamp- purposes the state is divided into 14 counshire lost 59,873 acres, and Vermont 33,- ties, which are sub-divided into 245 town897 acres, and the south line of the state ships, and several small gores of land, is not parallel with the north line. The which are not yet annexed to, or formed western boundary was settled by the gov- into, townships. The names of the counernments of Vermont and New York at ties, the date of their incorporation, the the close of their controversy, in 1790. shire towns, and the number of towns in This line passes along the western boun- each county at the present time (1842,) daries of the townships of Pownal, Ben- are exhibited in the following table: nington, Shaftsbury, Arlington, Sandgate, Rupert, Pawlet, Wells and Poultney, to Counties. Incorporated. ShireTowns. Ns Poultney river; thence along the middle Addison, Feb.27, 177 Middlebury, 22 of the deepest channel of said river, East Bennington Feb.11, 1779 Bennington 17 bay and lake Champlain to the 45th de- Manchester, gree of north latitude, passing to the east- Caledonia, Nov. 5,1792 Danville, 18 ward of the islands called the Four Broth- Chittenden, Oct.22, 1782 Burlington, 15 ers, and to the westward of Grand Isle Essex, Nov. 5,1792 Guildhall, 17 and Isle la Motte. The portion of this line Franklin, Nov. 5, 1792 St. Albans, 14 between the southwest corner of the state Grand Isle; Nov. 9, 1802 North Hero, 5 and Poultney river, was surveyed in 1813 Lamoille Oct.26, 1835 Hydepark, 12 and 1814, and the report and plan of the Orange, Feb. 1781 Chelsea, 17 survey are in the office of the Secretary Orleans, Nov. 5, 1792 Irasburgh, 19 of State at Montpelier. Rutland, Feb. 1781 Rutland, 26 Extent and area.-The length of Ver- Washington Nov. 1, 1810 Montpelier, 17 mont from north to south is 157A miles, Windham, Feb.11, 1779 Newfane, 23 and the average width from east to west Windsor, Feb. 1.781 Woodstock, 23 67A miles, which gives an area of 9,0564l 7 miles, which gives an area of 9,056 * Dr. Williams (vol. I, p. 24) seems to have, insquare miles, or 5,7935,9(60 acres. The advertently, taken the mean of the two ends of the length of the north line of the state is 90 state for its mean width and thus computed tho miles, and of the south line 41 miles, but, area at 10,'371-4 square miles, or 1181m. too much; on account of the great bend of the Con- lhut this is the area which has usually been given teecticu to mea in our geographies and other works respecting Vernecticllt to the westward, the mean width mont. As the area of countnies forms the basis of of the state is considerable less than statistical tabies, it is a matter of somie consequence the mean between these two lines, as that it should be correctly statel. Suppose for exabove stated. The width of the state ample, we wish to know how Vermont compares above stated. The widthoft with the other states in density of population, we from Barnet to Charlotte through Mont- divide the population of each state by its area anld pelier, which is 50 miles nearer to the the quotient is the average numhler of persons to each square mile in the states respectively. Now northern than to the southern boundary, if we take the last census and the area at 10,237, is only about 60 miles. On account of the population is only about28 to a square nnile, hut the irregularities in the western and east- if we take the true area, 9,056, it is 3'2 to the square ern boundaries, both these lines are lon- mile,which would eftfect very materially its relation r boundarithln thesmea. lines' are I on- sta to the other states. According to the census of 1820, ger than the mean length of the state, the Vermont was set down as the 10th state in density CTse. 1. DESCRIPTIVE GEOGRAPHY. FICE OF THE COUNTRY. PRINCIPAL SUMMITS. DIAGRAM Of the relative altitudes of some of the principal hTeights in Vermont above the sea. 4279 The Chin, or North Peak of Mansfield Mountains... 4183 Camnel's Hump, - -........... 4086 Shrewsbury MAountain,.. —- -...-*. ——. 3983 Tho Nose, or South Peak of Mansfield Mountains, --......... -- 3924 Killington Peak, -- -~ 3706 Equinox Mountain, Manchester, - -.. -. -. 3320 Ascutney Mountain, 3063 Middlebury turnpike, -.. 19421Peruturnpike, 1882 Keyes turnpike, - -- -- -- - --- - 951 Summit levelat Roxbnry,.. 908 Summit level at Williamstown, ——......791.Manchester villiage...... ——. 485Montpelier villiage,.......... 4301Norwich University,......... 3701University of VermAont,....: 90jSurface of Lake Champlain, SECTION II. of the roads, more particularly in their Face of the counttry. more judicious location near the streams, the difficulty of crossing the mountain has Mountains.-The surface of Vermont is nearly vanished. In the southern part of generally uneven. A few townships along Washington county, the Green Mountains the margin of lake Champlain may be separate into two ranges. The highest of called level; but with these exceptions, these ranges, bearing a little east of north, the whole state consists of hills and val- continues along the eastern boundaries of leys, alluvial flats and gentle acclivities, the counties of Chittenden and Franklin elevated plains and lofty mountains. The and through thie county of Lamoille to celebrated range of Green Mountains, Canadaline; whilethe other range strikes which give name to the state, extends off much more to the east through the quite through it from south to north, keep- southern and eastern parts of Washinging nearly a middle course between Con- ton county, the western part of Caledonia necticut river on the east and lake Cham- county and the north western part of Esplain on the west. From the line of Mas- sex county to Canada. Thislast is called sachusetts to the southern part of Wash- the height of lands, and it divides the ington county, this range continues lofty, waters, which fall into Connecticut river, and unbroken through by any considera- in the north part of the state, from those ble streams; dividing the counties of which fall into lake Champlain and lake Windham, Windsor and Orange from the Memphremagog. This branch oftheGreen counties of Bennington, Rutland and Ad- Mountains, though it no where rises so dison. In this part of the state, the com- high as many points ofthe western branch, munication between the eastern and west- is much more uniformly elevated; yet ern sides of the mountain was formerly the acclivity is so gentle as to admit of difficult, and the phrase, going over the easy roads over it in various places. mountain, denoted an arduous business. The western range, having been broken But on account of the great improvement through by the rivers Winooski, Lamoille and Missisco, is divided into several seeof population, whereas, if the true area had been to, s ive in ee sused in the computation, she would have ran- tions, these rivers having opened passaed as the eighth. ges for good roads along their banks,whilo 4 NATURAL HISTORY OF VERMONT. CHAP. L MOUNTAINS. RIVERS AND STREAMS. the intervening portions are so high and Rivers and Streams.-The rivers and steep as not to admit of roads being made streams lying within the state of Vermont over them, with the exception of that por- are very numerous, but small. They, in tion lying between the Lamoille and Mis- most cases, originate among the Green sisco. This part of the Green Mountains Mountains, and their courses are short presents some of the most lofty summits and generally rapid. Connecticut river in the state; particularly the Nose and washes the whole eastern border of the Chin in Mansfield, and Camel's Hump in state, but belongs to New Hampshire, the Huntington. These, together with other western margin of that stream forming important mountains and summits in the the boundary line between New Hampstate, are exhibited in the foregoing table shire and Vermont. The Connecticut reand cut, and will also be described in the ceives the waters from 3,700 square miles Gazetteer, under their respective names. of our territory. It receives from VerThe sides, and, in most cases, the sum- mont, besides numerous smaller streams, mits of the mountains in Vermont, are the waters of the eleven following rivers, covered with evergreens, such as spruce, viz: Wantasticook, or West, Saxton's, hemlock and fir. On this account the Williams', Black, Ottaquechy, White, French, being the first civilized people Ompompanoosuc, Wait's, Wells', Paswho visited this part of the world, early sumpsic, and Nulhegan. Clyde, Barton gave to them the name of Verd MJont, or and Black river run northerly into MemGreen Mountain; and when the inhabi- phremagog lake. Missisco, Lamoille, tants of the New Hampshire Grants as- Winooski and Poultney river and Otter sumed the powers of government, in 1777, creek flow westerly into lake Champlain, they adopted this name, contracted by the and the Battenkill and Hoosic westerly omission of the letter d, for the name of into Hudson river. Deerfield river runs the new state.' southerly from Vermont and falls into the Connecticut in Massachusetts; and the * This name is said to have been adopted upon Coatacook and Pike river head in the the recommendation of Dr. Thomas Young-(see part id, page 106.) The following account of the north part of the state and run northerly christening of the Green Mountains, is given by the into Canada, the former uniting with Rev. Samuel Peters in hisi life of the Rev. Hugh Massuippi river at Lenoxville and the latPeters, published at New York in 1807. ter falling into the head of Missisco bay. " Verd-Mont was a name given to the Greener faling int o the hea d of Missisco bay. Mountains in October, 1763, by the Rev. Dr. All these streams and many smaller ones Peters, the first clergyman who paid a visit to the will be described in the Gazetteer under 30,000 settlers in that country, in the presence of their respective names. Col. Taplin, Col. Willes, Col. Peters, Judge Pe- No country in the world is better supters and many others, who were proprietors of a plied with pure and wholesome water large number of townships in that colony. The than Vermont. There are scarcely any ceremony was performed on the top of a rock farms in the state which are not well wastanding on a high mountain, then named Mount tered by springs, or brooks; and none, Pisgah because it provided to the company a clear with the exception of those upon the islsight of lake Champlain at the west, and of Con- ands in lake Champlain, which are not in necticut river at the east, and overlooked all the the vicinity of one, or more, considerable trees and hills in the vast wilderness at the north mill stream. But while Vermont is so and south. The baptism was performed in the abundantly supplied with water, there is, following manner: Priest Peters stood, on the probably, no part of our country in which pinnacle of the rock, when he received a bottle of so little stagnant water is found. The spirits from Col. Taplin; then haranguing the waters of the lakes and ponds are usually company with a short history of the infant settle- clear and transparent, and nearly all the ment, and the prospect of its becoming an impreg- springs and streams are brisk and lively. nable barrier between the British colonies on the It is a common remark that the streams south and the late colonies of the French on the in this state have diminished very much north, which might be returned to their late own- in size, since the country began to be ers for the sake of governing America by the dif- cleared and settled, and t is dountry began to be ferent powers of Europo, he continted,' We have here met upon the rock Etam, standing on Mount true to some extent. Many mills, which Pisgah,which makes a part of the everlasting hill,the e then poured out the spirits and cast the bottle spine of Asia,Africa and America,holding together upon the rock Etan,." the terrestrial ball, and dividing the Atlantic from There is no doubt that the name Verd.Mont had the Pacific ocean-to dedicate and consecrate this been applied to this range of mountains long preextensive wilderness to God manifested in the vious to the above transaction, (if, indeed, it ever flesh, and to give it a new name worthy of the took place;) hut we do not find that the name Verd oAthenians and ancient Spartans,-which new Mnt, or Verniont, was ever applied to the territory generally known as the New Hampshire Grants, name is Verd Mont, in token that her mountains previous to the declaration of the independence of and hills shall be ever green and shall never die.' the territory in January, 17T7. CHAP. 1. DESCRIPTIVE GEOGRAPHY. 6 LAKES AND PONDS. LAKE CHAMPLAIN. formerly had an abundance, have ceased state of New York, and more than half of to receive the necessary supply of water it within the limits of Vermont. It exduring a considerable portion of the year; tends in a straight line from south to and many mill sites, which were once north, 102 miles along the western bounthought valuable, have, from the same dary, from Whitehall to the 45th degree cause, become entirely useless. One of of latitude, and thence about 24 miles to the principal causes of this diminution of St. Johns in Canada, affording an easy our streams is supposed to be the cutting communication with that province and down of the forests, which formerly threw with New York. This lake is connected off immense quantities of vapor into the with Hudson river, at Albany, by a canal atmosphere, which was again precipitated 64 miles in length; so that the towns lyupon the earth in rain and snow. But it ing on the shores of Lake Champlain is believed that the quantity of water have direct communication by water with which annually passes off in our streams the cities of Troy, Albany, Hudson, and is not so much less than formerly as is New York, and, by means of the great generally imagined. Before the country western canal, with the great western was cleared, the whole surface of the lakes. The length of this lake from ground was deeply covered with leaves, south to north, measured in a straight line limbs, and logs, and the channels of all from one extremity to the other, and supthe smaller streams were much obstruct- posing it to terminate northerly at St. ed by the same. The consequence was, Johns, is 126 miles. Its width varies from that, when the snows dissolved in the one fourth of a mile to 13 miles, and the spring, or the rains fell in the summer, mean widthis about4A miles. This would the waters were retained among the give an area of 567 square miles, two leaves, or retarded by the other obstruc- thirds of which lie within the limits of tions, so as to pass off slowly, and the Vermont. The waters, which this lake streams were kept up, nearly uniform as receives from Vermont, are drained, by to size, during the whole year. But since rivers and other streams, from 4088 miles the country has become settled, and the of its territory. Its depth is generally obstructions, which retarded the water, sufficient for the navigation of the largest removed by freshets, when the snows vessels. It received iti present name melt or the rains fall, the waters run off from Samuel Champlain, a French noblefrom the surface of the ground quickly, man, who discovered it in the spring of the streams are raised suddenly, run rap- 1609, and who died at Quebec in 1635, idly, and soon subside. In consequence and was not drowned in its waters, as has of the water being thus carried off more been often said.* One of the names givrapidly, the streams would be smaller en to this lake by the aborigines is said to than formerly during a considerable part have been Caniaderi- Guarunte, signifying of the year, even though the quantity of the mouth or door of the country.t If so, water be the same. It is a well known it was very appropriate, as it forms the fact that the freshets in Vermont are gate-way between the country on the St. more sudden and violent than when the Lawrence and that on the Hudson. The country was new. name of this lake in the Abena'qui tongue The waters of the lakes, ponds and was Petawd-bouque, signifying alternate streams are universally soft, miscible with land and water, in allusion to the numersoap, and in general free from foreign ous islands and projecting points of land substances. And the same may be said along the lake. Previous to the settleof most of the springs, particularly on the ment of the country by Europeans, this Green Mountains, and in that portion of lake had long been the thorough-fare bethe state lying east of these mountains. tween hostile and powerful Indian tribes, The waters of most of the springs and and its shores the scene of many a mortal wells in the western part of the state conflict. And after the settlement, it are rendered hard and unsuitable for continued the same in reference to the washing by the lime they hold in solu- French and English colonies, and subsetion, and tthere are many springs which quently in reference to the English in are highly impregnated with Epsom salts, Canada and the United States. In conand others containing iron, sulphuretted sequence of this peculiarity of its locahydrogen, &c. These mineral springs tion, the name of Lake Champlain stands will be described in another place. connected with some of the most interestLakes and Ponds. Small lakes and ing events in the annals of our country; ponds are found in all parts of Vermont, and the transactions associated with the but there are no large bodies of water names of Ticonderoga, and Crown Point, which lie wholly within the state. Lake Champlain lies between this state and the * See Part HI, p. 2. tSpafford'sGaz.ofN.Y., p. 98. (3 NATURAL HISTORY OF VERMONT. PAaT L MEMPHREMAGOG LAKE. BAYS, SWAMPS, ISLANDS, SOIL. and Plattsburgh, and many other places, hall. Besides these there are several united with the variety and beauty of the smaller bays lying along the east shore of scenery, the neatness and accommodation Lake Champlain, and a considerable bay of the steamboats, and the unrivalled ex- at the south end of Lake Memphremagog, cellency of their commanders, render a called South bay. Most of these bays tour through this lake one of the most in- will be more particularly described under teresting and agreeable to the enlightened their names in part third, and also some traveller. A historical account of the of the most important bays lying along most important transactions upon Lake the west shore of Lake Champlain, and Champlain, together with some account belonging to New York. of the navigation of the lake, and partic- Swamps.-These are hardly of suffiularly of the steamboats which have been cient importance to deserve a separate nobuilt upon it, will be found in part second, tice. Though considerably numerous, and a much more minute description of they are, in general, of small extent, and, the lake under its name in part third. in many cases, have been, or may be Memphremagog lake is situated on the drained and converted into excellent north line of the state, and about midway lands. They are most common in the between lake Champlain and Connecticut northern and northeastern parts of the river. It extends from south to north, state. In the county of Essex are several and is nearly parallel with lake Cham- unsettled townships, which are said to be plain. It is 30 miles long, and the aver- made up of hills and mountains with age width about two miles. One third swamps lying between them, which renpart of this lake lies in Vermont; the oth- der them to a great extent incapable of er two thirds in Canada. The name of settlement. There isa considerable tract this lake in the Abenaqui tongue was of swampy land at the south end of MemMem-plow-bouque, signifying a large ex- phremagog lake, and another in Highgato panse of water. This, together with nu- about the mouth of Missisco river. When mnerous small lakes and ponds, which lie the country was new, there were many wholly within the state, will be described stagnant coves along the margin and in part third, either under their names, or among the islands of Lake Champlain, in the account of the towns in which they which, during the hotter parts of the sumare situated. There is abundant evidence mer, generated intermittent and bilious that most of our lakes and ponds were fevers. But, since the clearing of the formerly much more extensive than they country, these have been, to a consideraare at present, and that they have been ble extent, filled up, and, with the causes diminished, both by the deposit of earthy which produced them, those disorders matter brought in by the streams, and by have nearly disappeared. the deepening of the channels at their Islands. —The principal islands beoutlets; and there is also sufficient proof longing to Vermont, are South Hero, of the former existence of many ponds in North Hero, and La Motte. South Hero, this state, which have long since become called also Grand Island, is 13 miles long, dry land by the operation of the same and Is divided into two townships, by the causes. Several of these will be pointed name of South Hero and Grand Isle. out in the descriptions of the rivers in North Hero is about 11 miles long, but part third, particularly in the description very narrow, and constitutes a township of Winooski river, Barton river, &c. bearing the same name as the island. Bays.-The shores of Lake Cham- Isle la Motte lies westward of North plain are indented by numerous bays, Hero, and constitutes a township by the most of which are small and of little con- same name. A more particular account sequence. Missisco bay is the largest of of these islands, and also a description of these, and belongs principally to Vermont, Juniper island and several others lying lying between the townships of Alburgh in Lake Champlain, will be found under and Highgate, and extending some dis- their names in part third. tance iAto Canada. The other bays of Soil and Prodluctions.-The soil of most consequence, lying along the east Vermont is generally a rich loam, but vashore of the lake and belonging to Ver- ries considerably according to the nature mont, are M'Quam bay in Swanton, Be- and compositions of the rocks in the diflamaqueen bay lying between St. Albans ferent parts of the state. Bordering our and Georgia, Mallets bay in Colchester, lakes, ponds, and rivers, are considerable Burlington bay between Appletree point tracts of rich and beautiful intervale* and Red Rocks point, Shelburne bay between Red Rocks point and Pottier's * Intervale. This word has not yet found A place oint, Button bay in Ferrisburgmh, and in our dictionaries, and there has been much carping ) — J i I --------- about it by bDr. Dwight, Mr. Kendall, and other East bay between Westhaven and White- travellers and critics. But we use it, notwithstand CHAP. L DESCRIPTIVE GEOGRAPHY, 7 SOIL AND PRODUCTIONS. MEDICINAL SPRINGS. lands, which consist of a dark, deep and the farmer who is saving and industrious fertile alluvial deposit. These intervales seldom fails of having his barn filled with are level tracts lying but little higher than fodder for his horses, cattle and sheep, the ordinary height of the water in the his granary with corn, wheat, rye, oats, streams, and are in most cases subject to peas and beans, and his cellar with potabeing flooded, when the water is very toes, apples, and other esculent vegetahigh. They were, while in a state of na- bles. A sufficient quantity of grain for ture, covered with a heavy growth of for- the supply of the inhabitants might easily est trees, such as oak, butternut, elm, be raised in all parts of the state, yet the buttonwood, walnut, ash, and some other greater part of the lands are better adaptkinds. Back of these flats were frequent- ed for grazing than for tillage. The hills ly others, elevated a few feet higher, and and mountains, which are not arable on covered with white pine. Still further account of their steepness, or rocks, afford back, the land rises, in most cases very the best of pasturage for cattle and sheep. gradually, into hills and upland plains, Of the fruits, nuts, berries, &c., which and the soil becomes harder and more grow in Vermont, both wild and cultivagravelly, but very little diminished in ted, a more particular account will be richness and fertility. The timber upon given in a subsequent chapter on the botathese lands, which constitute the greater ny of the state. part of the state, was principally sugar JMedicinal Springs.-There are in Vermaple, beech and birch, interspersed with mont springs which are more or less imbass, ash, elm, butternut, cherry, horn- pregnated with mineral, or gaseous subbeam, spruce and hemlock. And still fur- stances, but none which have yet acther back the lands rise into mountains, quired a very general or permanent celebwhich are in general timbered with ever- rity for their curative properties. Along greens, such as spruce, hemlock and fir. the shore of Lake Champlain, in the The loftiest mountains are generally rocky counties of A ddison and Rutland, the waand the summits of some few of them ters generally are impregnated with Epconsist of naked rock, with no other traces som salts, (sulphate of magnesia). Some of vegetation than a few stinted shrubs of the springs are so highly charged with and mosses; but they are, in general, these salts, in the dryer parts of the year, thickly covered with timber to their very that a pail full of the water will produce tops. Along the western part of the a pound of the salts. They have been state, and bordering upon Lake Cham- manufactured, for medicinal purposes, in plain, are extensive tracts of light sandy some quantities, and, did the price of the soil, which were originally covered with article make it an object, they might be white, pitch and Norway pine, and in the made here to almost any extent. northern part of the state, swamps are The medicinal properties of most of the numerous, which were well stored with waters in this state, which have acquired tamarack and white cedar. A more full any notoriety, are derived from gaseous account of the native vegetables found in and not from mineral substances. In difthis state will be given in a subsequent ferent towns in the northeastern part of chapter. Since the country has been the state, are springs of cold, soft and cleared, the soil has, in general, been clear water, which are strongly impregfound sufficiently free from stone to ad- nated with sulphuretted hydrogen gas,and mlit of easy cultivation, and to be very said to resemble the Harrow.Gate waters productive in corn, grain and grass. With- in Ensgland, and those of Ballcastle and out manuring the intervales usually pro- Castlemain in Ireland. These waters are duce large crops, and are easily cultiva- found to be efficacious in scrofulous and ted, but these crops are liable, occasion- many other cutaneous complaints, and the ally, to be destroyed by floods-the same springs at Newbury, Tunbridge, Hardagency which produces the fertility of the wick, &c., have been much resorted to by soil on which they grow. All parts are, valetudinarians in their vicinity. however, sufficiently fertile amply to re- Of medicinal springs on the west side ward the labors of the husbandman, and of the Green Mountains, those of Clarendon and Alburgh have acquired the greating,.because it will express our meaning more br est notorieflty. It is now about ye and intelligibly to the greater part of our readers, est notoriety. It s now about 16 years than any other we could employ. It may be derived since the springs at Clarendon began to from inter-within, and vallis-a vale, or valley; be known beyond their immediate neighand in its specific signification, it denotes those allu- borhood. Since that time their reputavial flats, lying along the margins of streams, which have been, or occasionally are overflowed in conse- tion has been annually extending, and the quence of the rising of the water. For the use of the number of visiters increasing, till they word in this sense, we have the authority of Dr. ave at lengt become a place ofconsiderBelknap and Di. Williams, the historians of New have at length become a place ofconsiderHampshire and Vermont, and other good writers. able resort for the afflicted fromn various 8 NATURAL HISTORY OF VERMONT. ~AaP I. CLARENDON SPRINGS. CLARENDON AND PLYMOUTH CAVES. parts of the country. They are situated in a of the year, and water stands in the lowpicturesque and beautiful region, 7 miles est parts of it at all seasons.* southwest from Rutland, and have, in The Plymouth caves are situated at the their immediate vicinity, good accommo- base of a considerable mountain, on the dations for 500 visiters. The waters are southwest side of Black river, and about found to be highly efficacious in affections 50 rods from that stream. They are exof the liver, dispepsia, urinary and all cu- cavations among the lime rock; which taneous complaints, rheumatism, invete- have evidently been made by running rate sore eyes, and many others, and they water. The principal cave was discovpromise fair to go on increasing in noto- ered about the first of July, 1818, and on riety and usefulness. These waters differ the 10th of that month was thoroughly in their composition from any heretofore explored by the Author, who furnished known, but resemble most nearly the the first description of it, which was German Spa water. For their curative published shortly after in the Vermont properties they are believed to be indebted Journal at Windsor. The passage into wholly to the gases they contain. They this cavern is nearly perpendicular, have been analyzed by Mr. Augustus A. about the size of a common well, and Hayes, of Roxbury, Mass., with the fol- 10 feet in depth. This leads into the first lowing results. One gallon, or 235 cubic room which is of an oval form, 30 feet inches of the water contained, long, 20 wide, and its greatest height Carbonic acid gas 46.16 cubic inch. about 15 feet. It appears as if partly filled Nitrogen gas 9.63 " " up with loose stones, which had been Carbonate of Lime 3.02 grains. thrown in at the mouth of the cave. Murate of Lime ) From this to the second room is a broad Sulphate of Soda >2.74 grs. sloping passage. This room is a little Sulphate of Magnesia more than half as large as the first. The One hundred cubic inches of the gas bottom of it is the lowest part of the cave, which was evolved from the water, con- being about 25 feet below the surface of sisted of the ground, and is composed principally Carbonic acid gas 0.05 cubic inches. of loose sand, while the bottoms of all the Oxygen gas 1.50 r other rooms are chiefly rocks and stones. Nitrogen gas 98.45 The passage into the third room is 4 feet wide and 5 high, and the room is 14 feet The Alburgh springs do not differ ma- long, 8 wide, and 7 high. The fourth terially from the springs at Newbury, room is 30 feet long, 12 wide, and 18 high, Tunbridge, and other places in the north- and the rocks, which form the sides, ineastern part of the state, owing their med- cline towards each other and meet at the icinal properties principally to the sul- top like the ridge of a house. The fifth phuretted hydrogen gas, which they con- room, very much resembling an oven in tain. shape, is 10 feet long, 7 wide, and 4 high, Caves. There are no caves in Vermont and the passage into it from the third which will bear comparison with some of room is barely sufficient to admit a person the caverns found in other parts of the to crawl in. At the top of this room is a world, and yet we have several, which conical hole, 10 inches across at the base are deserving the attention of the curi- and extending 2 feet into the rock. From ous. Those at Clarendon, Plymouth and the north side of the second room are two Danby are the most interesting. The openings leading to the sixth and seventh, Clarendon cave is situated on the south- which are connected together, and each easterly side of a mountain in the wester- about 15 feet long, 7 wide, and 5 high. ly part of that town. The descent into it From the seventh room is a narrow pasis through a passage 21- feet in diameter sage which extends northerly 15 or 16 and 31 feet in length, and which makes feet into the rocks, and there appears to an angle of 35 or 40~ with the horizon. terminate. When discovered, the roof It then opens into a room 2() feet long, and sides of this cavern were beautifully 129 wide, and 18 or 20 feet high. The ornamented with stalactites, and the botfloor, sides and roof of this room are all of tom with corresponding stalagmites, but solid rock, but very rough and fineven. most of these have been rudely broken off From the north part of this room is a pas- and carried away by the numerous visitsage about 3 feet in diameter and 24 feet ers. The temperature, both in winter in length, but very rough and irregular, and summer, varies little from 44~~, which which leads to another room 20 feet wide, is about the mean temperature of the cli30 feet long and 18 feet high. This room, mate of Vermont in that latitude. A few being situated much lower than the first, is usually filled with Eater in the spring * Williams' History of Vermont, vol. 1, p. 29. CHAP. 1. DESCRIPTIVE GEOGRAPHY. 9 CLIMATE AND TEMPERIATURE. METEOROLOGICAL JOURNALS. rods to the westward of this cavern there places in this state, was as follows: Montis said to be another which is about two pelier -400, White River — 40, Bradford thirds as large. -38~, Newbury -360, Norwich -36~, Windsor -34~, Hydepark -360, Rutland -30(), and Burlington — 26Q; and the SECTION III. temperature varied but little from the' Climate and iMeteorology. above at those places on the 18th of December. For some time after the first Temperature.-Though situated in the settlement of Vermont the thermometer middle of the north temperate zone, the was hardly known in this part of the climate of Vermont is subject to very country; and since that instrument has considerable extremes both of heat and become common, very few meteorological cold, and the changes of temperature are journals have been kept, and those few often very sudden. The usual annual have not, in general,been kept with suffirange of the thermlometer, in the shade, is cient care to render them of much value, from about 9320 above to 220 below zero nor have many of them been preserved in on Farenheit's scale, though it is some- a condition to be accessible to those who times known to rise as high as 100~, and may wish to consult them. And hence at other times to sink as low as 360, and we possess few accurate data, either for even to 390 or 400 below zero. But so determining the mean annual temperagreat a degree of cold as that last men- ture of the different sections of the state, tioned, which is the freezing point of' or for settling the mooted question with mercury, has not, to our knowledge, boen regard to a change of climate correspondexperienced but twice since the means of ing to the clearing and cultivating of the measuring temperature have been in use country. The results of the principal ohin the state, and these were both in the servations, to which we have access, and year 1835; the first on the 4th of January, which have been made in this state, to and the second on the Inorning of the ascertain the temperature' of tile months 18th of December. The temperature of and the mean annual temperature, are the 4th of January, as noted at several contained in the following tables: Rutland. Burlington. Windsor.l Burlington. Williams.. Sandlers. Fowler Thompson. MONS!)~\ 1 808. 180-7 |lH18t21 13.1833. 1838. 139. 18401 January, 1.0u o.440 422.Oo 25.0 19.7 22.8 26.1 18.6 12.2 25.3 February., 18.5 1.9 265 31.1 19.3 15.3 12.3 24.2 28.4 19.6 March, 32.0 28.5 30).3 32.4 30.8 28.2 32.6 36.6 31.4 25.3 April, 41.0 39.5 38.1 39.21 39.4 46.1 35.8 46.3 47.0 39.1' May, 50.0 56.3 57.1 57.6 52.4 57.0 51.7 53.31 57.2 52.8 June, 64.0 66.6 66.4 6!).7 61.3 59.6 68.1 60.7 65.6 67.1 July, 67.5 68.2 68.5 70.1 68.5 66.2 71.8 71.51 71.6 68.9 August, 67.5 67.6 64.3 70.2 68.3 63.3 67.5 68.3 72.5 70.5 September 57.0 57.1 62.1 60.;3 58.7 57.2 60.5 60.6 58.3 61.9 October, 41.0 45.2 49.5 46.7 47.7 44.9 46.8 50.8 48 0 45.0 November, 37.0 33.5 36.2 38.9 35.6 34.5 31.3 34.0 35.6 35.3 December, 30.0 24.7 24.6 29.3 231.6 24.7 19.1 26.2 21.1 26.4 43.6 43.4 4. 0 47.6 4 43.8 43.3 43.6 45.5 45.7 44.8 Meteorological observations at W1illiamstown by Hon. Elijah Paine. MONTHS. 1829 1830 1831 1832 183311834 1835 1836 1837 183818391 1840 _1841 January,.4 10.9 1 7.1 19.3 12.5 17.9 173 97 23.9 15.3 9.0 21.6 February, 10.9 14.3 14.6 1-4.6 13.5 26.5 12.6 1(05 16.7 9.9 20.8 23.7 1 5.8 March, 23.5 26.4 26.4 25.4 23.5 27.2 I25.1 22.9 23.6130.9 25 8 26.0 24.1 April, 36.6 44.6 39.8 41.2 41.7 136.1 34.5 36.5 131.2 41.21 40.7 34 7 May, 54.8 49.6 53.2 54.7 48.9 4840 51.6 45. 148.5 48.7 51.7 47.7 June, 58.7 5.9 64.8 59.3 5.4 57.4 59.4 58.8 60.6 163.0 54.9 58.5 63.1 July, 60.2 64.1 64.4 63.3 162.3 68.2 64.6 165.4 61.2 166.2 65.2 64.8 62.6 August, 60.7 60.7 63.6 63.5 59.5 60.5 160.9 157.0) 59.8 61.6 161.4 64.6 63.9 September, 47.9 51.4 53.0 53.9 52.7 55.4 150.0 153.3 52.0 54.6 54.2 52.5 57.9 October, 42.6S 44.4 44.6 43.9 41.2 139.7 147.8 34.5 39.0 139.7 45.4 41.9 38.5 November, 2!).7 38.2 30.9:31.7 129.5 28.9 29!).8 28.7 30.6 125.3 i28.1 30.2 29.4 December, 27.3 24.9 7 1 19.7 21.1 16(i.0 13.1 17.8 114.4 14.1 121.4 16.2 21.7 40.7 39.4 39..5 O.2 38.8 37.7 37.5,3:.1 140., 39. 40.0) PT.. 10 NATURAL HISTORY OF VERMONT. PART I. MEAN TEMPER&TURE AT BURLINGTON AND WILLIAMSTOWN. WINDS. With the exception of the first three by the changes of temperature which are columns in the first of the two preceding constantly going on at the surface of the tables, the particulars of which are not earth; the temperature of these may, known,. all the means for the months therefore, be regarded as a pretty fair inhave been deduced from three daily obser- dication of the mean annual temperature vations, taken at sun-rise, 1 o'clock, P. of the climate. The temperature of a M. and 9 in the evening. Now, as the well 40 feet deep, belonging to Mr. Samthree daily observations at Burlington uel Reed, in Burlington, has been obsynchronize for several years with those served and noted during the year 1841 as at Williamstown, the two tables enable follows, the.first number after the day of us to make a very accurate comparison of the month being the depth in feet to the the mean temperature of the two places; surface of the water at the time of the and the comparison shows that the mean observation: Jan. 1, 14-46~, Feb. 12, temperature of Burlington, although sit- 18-44,~, April 14, 16-44~, June 1, 10uated 22' farthest north, is about 50 warm- 44~, July 20, 10-46AQ, and Dec. 8, 20er than that of Williamstown, that of the 4510, giving a mean of 45.1~, or.3~ higher former being 44.6' and the latter 39.4o. than that deduced from the daily obserBut the cause of this difference is obvi- vations. ous in the location of the two places, Bur- IWinds.-For small sections of country lington being situated on the margin of the prevailing winds usually take their lake Champlain, and the place of obser- direction from the position of the mounvation elevated only 250 feet above it, tains and valleys. That is veryfmuch the while Williamstown lies among the Green case in Vermont. Through the valley of Mountains near the geographical centre the Connecticut and of lake Champlain of the state, and, the place of Judge the winds usually blow in a northerly or Paine's observation, elevated 1500 feet southerly direction, while easterly and above the lake.* westerly winds are comparatively of rare The mean annual temperature of Bur- occurrence. In the valley of lake Chamlington, deduced from all of the 12 years plain east winds are exceedingly rare, as observations in the preceding table, is will be seen by the following tables.* 44.1~, and from the seven years observea- Along our smaller rivers, particularly the tions by the author 44.9Q, but, as the year Winooski and the Lamoille, the prevail1828 was very remarkably warm, that ing winds are from the,northwest. The should, perhaps, be set aside, and the following tables contain the result of' mean of the other six, 44.4~, taken as prob- observations made at Burlington, for ably a fair statement of the mean annual eleven years, and at Rutland for one temperature of Burlington. The mean year. In the journal kept by the author annual temperature of Williamstown, de- at Burlington, and from which the taduced from the whole of Judge Paine's bles on the following page were copied, observations, is 40.3~. three observations of wind and weather Many perennial springs, and deep were entered each day, which synchrowells are found to continue nearly of the nize with the observations of temperasame temperature, both in summer and ture for the same years in the preceding winter, and to be but very little affected table, on the ninth page. The following table contains the results of five years observation at Burlington, by Dr. Saunders, and one year at Rutland, by Dr. Williams. Place. 1 Time. INo.Obs. 1 il N s1El sI 4s3 II W 1 rw fair. clody rain snwfog thun Burlington 1803-81 16821739 111191! 8261 251 431 18 1025r1 676 289 127 19 45 27 Rutland 11789 | 109511531131161761272l182112512558 4521 643 89 411371 15 21 * The author has in his possession a meteorologi- * Although, at Burlington, we seldom have a cal journal kept at Hydepark by Dr. Ariel Huntoon, wind from the east sufficiently strong to turn the for a period of 9 years, of which he had intended to vanes upon our churches, it is not uncommoni, dur — insert an abstract; but, finding the three daily ob- ing the latter part of the night and early in the servations to have been made too near the warmest morning, when the weather is fair, to have a light part of the (lay to furnish the true mean tempera- breeze from the east, which is doubtless occasioned ture of the 24 hours, and consequently unsuitable by the rolling down of the cold air from the mounfor comparison with the other tables, he concluded tains to supply the rarefactiorn over the lake. In not to insert it. In order to render meteorological other words, it is strictly a land breeze, similar to observations of service in determining the relative what occurs between the tropics. That these breezes temperature of places, uniformity in the method of are local and limited is evident from the fact, that. making them seems to be indispensable, and a want at the same time, the general motion of the air is in of this renders a great part of the journals which a different direction, as indicated by the motion of have been kept nearly useless. clouds in higher regions of the atmosphere. 00~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~5 WINDS. WEATHER.. WINDS. WEATHER. Z.2- WINDS. WAHR 1832 ~ N ne ErSI S sW wNW fair. cldy r'n sno 1838 ~ N ne E s s w nw fair cldyr'nsno 1840 N ne E SE S SW WNW fair. eldyr'nsno......~ —-, - -.. _ _, ~.............-.................... Jan 93 16 2 0 2 401 4l l18 49 29 312 Jan 93 31 I 1 0 51 1 7 1 43 39 6 5 Jan 98 35 3 0 6 3010 8 1 52 33 2 6 Feb 87 35 0 1 0 37 24 8 42 24 3[18Feb 84 60 3 0 3 14 0 4 0 56 24 0 4[Fcb 87 24 0 1 1 54 4 2 1 47 36 4 0 Mar 93 37 1 0 2 44 13 5 59 23 2 9[Mar 93 54 0 2 232 00 21 56 33 1 3 Mar 93 26 31 7 38 5 2 11 59 20 9 5] Apr 90 40 1 1 7 24 6 2 9 54 25] 8 3 Apr 90 42 0 0 0 31 0[15 2 59 27 4 0 Apr 90 24 0 2 9 42 4 2 7 63 15/11 I May 93 40 1 0 4 31 0 5 12 54 2019 0 May 93 5a 3 0 0 3 36 0 2 0 66 20 7 0 May 93 30 4 3i13 33 0 5 5 72 13 8 0/= J ne 90 42 1 0 1 38 0 4 4 62 20 8 0 Jne 90 33 2 11 51 0 2 0 63 20 70 oJ ne 90/24 1 2 5 48 1 6 3 64 21 5 0] 4July 93 30 4 4 0 471 2 5 59 23a11 O July 93 32 6/01 /46 1 3/3 7341 46 olJuly 93/171 1 3 3 54 2 8 51791 13 0 Aug 93 21 0 0 0 64 10 7 6S 201 5' 0[Aug 93 33 31 6 37 1 10 2 75 13 50 oAug 93 91 5 5 52 213 6 69 18 6 o Sept 90 14 0 0 0 52 312 9 70 15,15 0 Sept 9 45 0 3 2 72 130 Sept 9019 7 0 537l16 15'a9 20illOt Oct 93 22 2 2 532 2 212 53 30olO1 oOct 93,39100 o o44036 50 36 0ct 93o2445 4o7o3732 3211 49439 4 1 a Nov 90 22 3 0 0 38 3110 13 36 41 7 6 Nov 90 36 2 0 2 46 0 2 2 50 31 6 3 Nov 90 19 10 9 3 27 3 9 10 36 49 2 3 I I'd~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ /Dec/ 93[ 451 3 0 3 32 3 2 5 34 50' 0 9 Dec 93 24 4 0 4 55 1 4 1 68 23 0 2 Dec 93 27 8 5 6 27 2 9 9 48 32 310: Total 1098 364,16 621500 26 571107 640632981157 Total 1095!482124 51251478 6155120 731/295:52117 Total 10981278!421361701479]37172 84 697 3076826 - 1833 Obs. N ne E sE S sw NW fair. cldyr'n s 1839 Obs. N ne E SE S SW w nw fair. cldyirnsn 1841 Obs. N ne E SE S SW W N W fair. cidy r'nsno: Jan 93 361 2~ 0 0 43 3 2 7 45 37: 3 8 Jan 93 41 2 0 4 42 0 2 2 45 401 5 3 Jan 93'21 2 1 7 42 512 3 52 25 610 Feb 84'41 0? 1 1 26 0 3 12 51 19: 0 14 Feb 84 21 2 0 1 57 0 1 2 42 37 3 2 Feb 84 18 I 0 4 34 313 11 50 28 0 6 /= Mar 93 34 01 0o 1 471 4 6 65 22~ 3 3lMar 93 40 o/ 3 40 0 4 3 66 232, 2 Mar 93 4.5 6 42 21 3 5 7 64 19 3 7:= Apr 90 43 0o 2 2 39 0 0 4 60 23 7 0 Apr 90 50 0 0 0 36 0 3 1 65 I6 6 3 Apr 90 33 1 1 2 28 610 9 63 9 810 i May 93 34 1 1 8 40 1 5 3 63 19 11 0 May 93 39 3 1 0 47 1 2 0 69 16 8 0 May 93 20 2 0 5 33 5 4 24 65 1016 2/ J/ne 90 27 0 2 3 38 2 10 8 62 20 8 01J ne 90 47 0 0 7 21 4 7 4 60 19.11 0 Jn/e 9 0 20 4 3 7 40 2 6 8 55 28 7 08 July 93 29 11 0 0 58 5 0 65 25 3 OlJuly 93 131 5 4 65 I 11 3 71 14 8 0 July 93 280 o1 3 36 3/10 12 77 12 4 0 Aug 93 3811 102 501 1 0 55 2810 O gl2 5 3 8Aug 93 1 9334 31 343 6 1 8105 0 Sept 90 45 01 0 0 41 0 2 2 66 20 4 0[Sept 90 8 0 1 9 54 5111 2 64 21 5 0|Sept 90 33 g( 0 7 40 04 4 60 23 7 0/ Oct 93 47 0 o 0 40 0 4 2 58 26 90 Oct 93 2 2 o 32 49 014 2 73 17 30 0oct 93 38 21 /0 343 3a312 44 42 6 1 Nov 90 35' 0 0 1 46 0 5 3 42 41 7 0 Nov 90 18 9 2 7 31 6 14 3 39 4.41 4 3 Nov 90 28 4 0 2 1.9 0o15 22 30 45 9 6 Dec 93 34,18 0 7 18 3 5 s 28 61 0 4 Dec 93 40 1[0 1, 4 23 3 012 51 32i 6 4 Dec 93 251 2 1 1 40 5 51 14 40 37 6o10 Total1o095!443 2-3 1.o25486I1 1461 5511660o341!65!29 Total Io1095361 38 1347;50312307 43 1729 285 64'17 Total11095343129 1343/410 37!93 107 6782881771521 12 NATURAL HISTORY OF VERMONT. PART I. ANNUAL QUANTITY OF RAIN. ANNUAL FALL OF SNOrW. Rain.-The quantity of water, which speak with much confidence on this point. falls in rain and snow in any one year, Tile quantity of water, however, which does not probably differ very considerably falls at the same places in different years, in the different sections of the state, but varies very considerably, as will appear observations are too few to enable us to from the following table: RUTLA ND.IV [iN DSO(R. BURLINGTON. MONTHS. Williamls. Fo wier I T/hon7SOs. 1789. 1 (. 1828.J 1832. 18:33. 1838. 1839. 1840. 1841. _. Inches. IncIIes. I Inches. Inces. Inches Inches. IncIles. Incles. Inchels. January, 3.50 2.90 1.30 3.56 1.26 2.52 0.85 1.26 3.49 C1 February, 2.78 2.44 2.10 3.22 2.63 1.32 1.20 2.19 0.80 o March, 3.10 0.48 1.35 2.31 1.48 1.10 1.43 3.05 3.23 April, 3.01 2.78 2.75 1.96 1.28 1.34 1.60 4.69 3.54 I May, 4.72 2.06 2.45 5.71 9.85 4.51 2.43 2.46 2.28 June, 3.91 2.73 3.70 3.41 4.28 5.37 3.70 2.84 5.16 eI July, 2.31 4.34 5.95 3.52 7.54 3.25 6.26 4.18 2.87; August, 2.11 0.95 4.30 4.76 7.34 2.41 1.91 3.51 1.40 September, 2.48 4.57 9.85 1.81 4.17 1.33 2.91 4.71 3.62 Y October,' 5.66 1.40 1.65 4.05 6.01 2.98 0.45 3.76 0.83 November, 4.10 2.17 6.25 3.01 1.91 3.78 2 57 2.22 2.47 d December, 3.49 2 36 1.65 2.27 1.59 0.92 2.68 2.41 3.02 Total, 841.17 29.l 43.30 39.59 49.24 30.83 1 27.99 37.28 32.71 1 The depth of water, which falls during Snow.-For more than three months of a rain storm or thunder shower, is much the year the ground is usually covered less than people generally suppose. A with snow, but the depth of the snow, as fall of 4 or 5 inches during a severe thun- well as the time of its lying upon the der shower would not be thought at all ground, vary much in the different parts extravagant by persons who have paid no of the state. Upon the mountains and attention to the accurate measurement of high lands, snows fall earlier and deeper, the quantity which fell. But during the and lie later in the Spring than upon the seven years observations at Burlington low lands and valleys, and it is believed contained in the above table, the depth of that they fell much deeper in all parts of water which fell in one shower has nev- the state, before the country was much er exceeded two inches, and the whole cleared, than they have for many years amount in 24 hours has, in only one in- past. As little snow falls at Burlington, stance, exceeded three inches, and that probably, as at any place in the state. was on the 13th of May, 1833, when the The following table exhibits the amount fall of water was 3.54 inches. at this place for the last five winters: Fall of Snow at Burlington in the'winters of 1837- 8. Inc. 1838-'9. Inc. 1839-'40. Inc. 1840-'1. Inc. 1841-'2. Inc.! Nov. 9, 2 Oct. 29 1 Nov. 6, 2 Oct. 26, 2 Oct. 8, 2 " 26, 5 Nov. 7, 3 l" 9,1 1 Nov. 22, 7,, 26, 3' Dec. 10, 3 " 19, 2 Dec. 11, 3 " 26,27, 3a " 29, 3 1.1, 1 " 28, 2 " 16, 9 Dec. 7, 6 Dec. 2, 1 " 18, 3 Dec. 7, A " 177 1 " 22, 3 "4 14 1 " 28" 17, 1 / " 1,I " 28, 527 8 L, 18 15 Jan. 15, 1 " 18, 4 /" 29,/ 4 Jan. 2, 10 Jan. 5, 2 1" 19, 2 " 23, 6 Jan. 5, 4 " 6, 1.1, 5 9, 2 2" 8, 12 " 29, 1 " 15, 1/ "22,e25, 8 " 27, 3 Feb. 11, 5 Jan. 4, 1'" 23, 6 " 30, 2 Feb. 17, 15'l 13, 3 L" 5, 1 IFeb. 26, 1 Feb. 2, 2A " 22, 1 " 17, 8 " 28, 1 March 7, 1 " 6, 10, 4& " 26, 4 " 22, 1 Feb. 2, 1 " 10, 2 " 17,27, 7 March 7, 5 March, 6, 6 [" 8, 2 ]" 24, 7 March 7, 5 " 15 1 /" 21, 1 c" 27, 4 " 9, 4 " 26, 5 " 28, 2 March 3, 1 " 29, 7 " 30, 3 /" 19, 5 Apr. 6,13, 2 April, 2, 1 April 13, 3 " 22, 5 60 41 48 92_I 64 I- o[ t-; —I~~~ CHAP. 1. DESCRIPTIVE GEOGRAPHY. 13 SLEIGHING. SEASONS. APPEARANCES OF BIRDS AND BLOSSOMS. In 1838-'9, sleighs run from December or hail. The crops oftener suffer from an 23, to January 8, but there was no good excess, than from a deficiency,of moisture, sleighing during the winter. In 1839-'40 though seldom from either. sleighing was excellent from December Seasons.-During the winter the ground ]6, to February 5, fifty one days. In 1840- is usually covered with snow, seldom ex-'41, sleighs run from November 22, to ceeding one.or two feet deep on the low November 29, and from December 7, to lands, but often attaining the depth of December 12, but the sleighing was not three or four feet on the high lands and good. From December 27, the sleighing mountains. The weather is cold, and, in was good till the 8th of January, after general, pretty uniformly so, with occawhich there was no good sleighing, al- sional snows and driving winds, till the though sleighs continued to run till the beginning of March, when with much 20th of March. In 1841-'2, sleighing to]- boisterous weather there begin to appear erable from December 18, to January 20, some slight indications of spring. About after that no good sleighing though sleighs the 20th of that month the snows begin run at several periods for a few days at a to disappear, and early in April the ground time. is usually bare. But the snows fall some The deepest snows, which fall in Ver- weeks earlier and lie much later upon the mont, are usually accompanied by a north mountains than upon the low lands. The or northeasterly wind, but there is some- weather and state of the ground is usually times a considerable fall of snow with a such as to admit of sowing wheat, rye, northwesterly, or southeasterly wind. A oats,- barley and peas, the latter part of long continuance of south wind usually April. Indian corn is commonly planted brings rain, both in winter and summer. about the 20th of May, flowers about the Although snows are frequent in winter 20th of July, and is ripe in October. Poand rains in summer, storms are not of tatoes are planted any timie between the long continuance, seldom exceeding 24 1st of May and the 10th of June. Frosts hours. Storms from the east, which are usually cease about the 10th of May and common on the sea board, do not often commence again the latter part of Sept., reach the eastern part of this state, and on but in some years slight frosts have been the west side of the Green Mountains observed, at particular places, in all the they are wholly unknown, or rather, they summer months, while in others, the tencome to that portion of the country from derest vegetation has continued green and a northeastern, or southeastern direction. flourishing till November. The observaThunder showers are common in the tions contained in the following table will months of June, July and August, but afford the means of comparing the springs seldom at other seasons. They usually of a few years past. They are gathered come from the west, or southwest, but are from the Meteorological journal kept by not often violent or destructive, and very the author at Burlington: little damage is ever done by hurricanes Robins Son, Barn Currants Red Plum Plumsand Crab Common seen. Sparrows Swallows Blossom. Blossom. Cherries Apple Apple iYear. seen. seen. Blossom. Blossom. Blossom. 182r' April28 May 9 My 12 May 16 182i' i; 23 s" 9 May 12 16 " 22 1832 Mar. 25NMar. 28 it 26 " 12 14 "' 201Mav 24 June 3 1].833 ", 23 "' 28 " 4' 7,. 12 " 15 May 18 837 " 2(0 " 23 " 30 " 16 " 19 " 28 " 30June 2 18381 " 23 31 May 2 " 19 " 22 " 26 June 1 " 2'1839' 25 " 25 April26 "1 4 " 12' 141May 22 May 26'1840 " 15 " 21 " 21 " 3 " 12 " 17 " 201" 23 841. " 27 " 27 " 2 "' 231 " 25/' 26,, 29 " 31' Vegetation, upon the low lands and ture, and bring fruits and vegetables to along the margin of the lakes and large maturity which do not succeed well upon streams, is, in the spring, usually, a week the high lands. To the above remark, or ten days in advance of that upon the with regard to early frosts, there are sevhigh lands and mountains; but frosts usu- eral exceptions. On the low islands and ally occur, in the fall, earliest upon the shores of lake Charnplain, vegetation is low lands, allowing to each nearly the frequently green and flourishing long after same time of active vegetation. The low the frosts have seared it in other parts of lands, however, enjoy a higher tempera- the state, and, along several of the rivers, 14] NATURAL HISTORY OF VERMONT. PART I. OPENING AND CLOSING OF LAKE CHAMPLAIN. DISAPPEARANCE OF THE ICE. vegetation is protected by the morning It frequently happens that the ice confogs for some time after its growth has tinues upon the lake for some time after been stopped upon the uplands. The the snows are gone in its neighborhood early part of the autumn is usually pleas- and the spring considerably advanced. ant and agreeable and the cold advances In such seasons the ice often disappears gradually, but as it proceeds the changes very suddenly, instances having been become more considerable and frequent, observed of the lake being entirely covand the great contrast between the tem- ered with ice on one day and the next day perature of the day and night at this sea- no ice was to be seen, it all having disson render much precaution necessary in appeared in a single night. People in the order to guard against its injurious effects neighborhood, being unable to account for upon health. The ground does not usu- its vanishing thus suddenly in any other ally become much frozen till some time way, have very generally supposed it to in November, and about the 25th of that sink. This opinion is advanced in the month the ponds and streams begin to be account of this lake contained in Spafcovered with ice, and the narrow parts of ford's Gazetteer of New York, and the lake Champlain become so much frozen anomaly is very gravely attempted to be as to prevent the navigation fromnt White- accounted for on philosophical principles. hall to St. Johns, and the line boats go in- But the true explanation of this phenomto winter quarters, but the broad portions enon does not require the absurdity of the of the lake continue open till near the first sinking of a lighter body in a heavier. It of February, and the ferry boats from Bur- is a simple result of the law by which lington usually cross till the first of Jan- heat is propagated in fluids. That bodies uary. The following table contains the are expanded, or contracted, according to times of the closing and the opening of the increase or diminution of the heat they the broad lake opposite to Burlington, contain, is a very general law of nature. and when the steamboats commenced and Fresh water observes this law, when its stopped their regular trips through the temperature is above 40~, but below 40~ lake from Whitehall to St. Johns, for sev- the law is reversed, and it expands with eral years past: the reduction of temperature. When winter sets in, the waters of the lake are much warmer than the incumLake Lake Lineboats Line bent atmosphere. The surface, therefore, Champl'n Champl'n comenc'd Boats. Year. closed. opened. running. stopped. of the water communicates its heat to the -... _.. -_. __ atmosphere, and, becoming heavier in 1816 Feb. 9 consequence, sinks, admitting the warmer 1817 Jan. 29 Apr. 16 water from below to the surface. Now 1818 Feb. 2 Apr. 15 since heat is propagated in fluids almosten1819 Mar. 4 Apr. 17 Apr. 25 tirely by the motion of the fluids, this ciro1820 ( Feb.3 Feb. culationwill go on,if the cold continues,till ~ Mr. 8 Mar. 12 all the water from the surface downward 1821 Jan. 15 Apr. 21 to the bottom is cooled down to the tem1822 Jan. 24 Mar. 30 perature of 400~. It will then cease. The 1823 Feb. 7 Apr. 5 Apr. 15 colder water now being lighter than that 1824 Jan. 22 Feb. 11 below, will remain at the surface and soon 1825 Feb. 9 be brought down to the freezing point and 1826 Feb. 1 Mar. 24 congealed into ice. This accounts for the 1827 Jan. 21 Mar. 31 ice taking soonest where the water is most 1828 not clos'd shallow, and also for the closing of the 1829 Jan. 31 Apr. Apr. 6 broad parts of the lake earliest in those 1.830 winters in which there is most high wind, 1831 Apr. 11 the process of cooling being facilitated 1832 Feb. 6 Apr. 17 Apr. 23 thereby. 1833 Feb. 2 Apr. 6 Apr. 8 After the ice is formed over the lake, 1834 Feb. 13 Feb. 20 Apr. 4 Dec. 5 and during the coldest weather, the great 1835 t JanlO Jan. 23 mass of water, after getting a few inches ~ Feb 7 Apr. 12 Apr. 21 Nov. 29 below the ice, is of a temperature 80 above 1836 Jan. 27 Apr. 21 Apr. 25 Nov. 29 the freezing point. While the cold is se1837 Jan. 15 Apr. 26 Apr. 29 Dec. 10 vere, the ice will continue to increase in 1838 Feb. 2 Apr. 13 Apr. 19 Nov. 26 thickness, but the mass of water below 1839 Jan. 25 1Apr. 6 Apr. 11 Nov. 28 the ice will be unaffected by the tempera1840 Jan. 25 Feb. 20 Apr. 11 ture of the atmosphere above. Now the 1841 Feb. 18 Apr. 19 Apr. 28 Dec. 1 mean annual temperature of the climate 1842 notclos'd Apr. 13 in the neighborhood of lake Champlain CHAP. 1. DESCRIPTIVE GEOGRAPHY. 15 FORMATION OF ANCHOR-ICE. SMOKY ATMOSPHERE. DARK DAYS. does not vary much from 450, and this is scent, are successively brought in contact about the uniform temperature of the with the stones at the bottom, which, earth at some distance below the surface. themselves, soon become ice-cold, after While then the mass of the waters of the which they serve as nuclei upon which lake is at 400, and ice is forming at the -the waters are crystilized and retained by top, the earth, beneath the water, is at the attraction, forming anchor ice. temperature of 45~, or 50 warmer than the Smoky.Stmosphere.-From the earliest water. Heat will, therefore, be constantly settlement of this country there have been imparted to the water from beneath, when observed a number of days, both in spring the temperature of the water is less than and autumn, on which the atmosphere 45~. The only effect of this communica- was heavily loaded with smoke. The tion of heat to the water from beneath, smoke has generally been supposed to reduring the earlier and colder parts of the suit wholly from extensive burnings in winter, is to retard the cooling of the lake some unknown part of the country. There and the formation of ice upon its surface. is no doubt but that much of the smoke But after the cold abates in the end of often is produced in this way, but it has winter and beginning of spring, so that appeared to us, that, since smoke is not a the lower parts of the ice are not affected product, but a defect, of combustion, it by the frosts from above, the heat, which may be possible for it to be produced even is communicated from below, acts upon where there is no fire. We have been the under surface of the ice, and, in con- led to this conclusion by observing that junction with the sun's rays, which pass the amount of smoke has not always been through the transparent surface and are greatest in those years in which burnings intercepted by the more opaque parts were known to be most extensive; and below,* dissolves the softer portions, by observing, moreover, that the atmosrendering it porous and loose like wet phere was usually most loaded with smoke snow, while the upper surface of the ice, in those autumns and springs which suchardened by occasional frosts, continues ceeded warm and productive summers. comparatively more compact and firm. In These circumstances have led us to the this state of things, it often happens that, opinion that the atmosphere may, by its by a strong wind, a rent is made in the solvent power, raise and support the miice. The waters of the lake are immedi- nute particles of decaying leaves and ately-put in motion, the rotten ice falls in- plants, with no greater heat than is neto small fragments, and, being violently cessary to produce rapid decompositioh. agitated, in conjunction with the warmer When, by the united action of the heat water beneath, it all dissolves and van- and moisture of autumn and spring, the ishes in the course of a few hours. leaves are separated into minute particles, There is one phenomenon, which is of we suppose these particles may be taken common occurrennce in many of our up by the atmosphere, before they are enstreams, during the coldest part of win- tirely separated into their original eleter, and which may not at first appear ments, or permitted to form new comreconcilable with what has been said pounds. This process goes on insensibly, above, and that is, the formation of ice until, by some atmospheric change, a conupon the stones at the bottom of the densation takes place, which renders the streams, usually called anchor ice. An- effluvia visible, with all the appearance chor ice is formed at falls and places and properties of smoke. where the current is so rapid that ice is Dark Days.-It sometimes happens not formed upon the surface. In the case that the atmosphere is so completely fillof running water, and particularly where ed with smoke as to occasion, especially the water is not deep and the current when accompanied by clouds, a darkness, rapid, over a rough bottom, the tempera- in the day-time, approaching to that of ture of the whole mass is probably reduced night. The most remarkable occurrennearly or quite to the freezing point be- ces of this kind, within our own recollecfore any ice is formed; and then, where tion, were in the fall of 1819, and in the the current is so rapid that the ice cannot spring of 1820. At both of these seasons, form at the surface, the ice-cold waters the darkness was so great, for a while of the surface, in their tumultuous de- near the middle of the day, that a book of i ordinary print could not be read by the * A remarkable phenomenon attending this dis- sun's light. The darkness in both cases integration of the ice by the influence of the sun's was occasioned principally by smoe, and rays, and one WVhich we think worthy of investiga- was occasioned principally by smoke, and tion, is its separation into parallel icicles, or can- without any known extensive burnings; dies, as they are sometimes called, extending per- but the summer of 1819, is known to have pendicularly from the upper to the lower surface of been remarkable for the abundant growth the ice, giving the mass, particularly the lower portions, somewhat the appearance of a honey comb. of vegetation. But the most remarkable 16 NATURAL HISTORY OF VERMONT. PART. L DARK DAY. INDIAN SUMMER. METEORS. darkness of this nature, which has occur- preceding articles, this is precisely what red since the settlement of this country, we should expect. When our ancestors was on the memorable 19th of May, arrived in this country, the whole conti1780, emphatically denominated the dark nent was covered with one uninterrupted, day. The darkness at that time is known luxuriant mantle of vegetation, and the to have covered all the northern parts of amount of leaves and other vegetable prothe United States and Canada, and to ductions, which were then exposed to have reached from lake Huron eastward spontaneous dissolution upon the surface over a considerable portion of the Atlan- of the ground, would be much greater tic ocean. It was occasioned chiefly by a than after the forests were cut down and dense smoke, which evidently had a pro- the lands cultivated. Every portion of gressive motion from southwest to noth- the country being equally shielded by the east. In some places it wasattended with forest, the heat, though less intense, on clouds and in some few with rain. The account of the immense evaporation and darkness was not of the same intensity in other concurring causes, would be more all places, but was so great through near- uniformly distributed, and the changes ly the whole of this extensive region as to of wind and weather would be less frecause an entire suspension of business quent than after portions of the forests during the greater part of the day, where had been removed, and the atmosphere, the country was settled, and in many pla- over those portions, subjected to sudden ces it was such as to render candles as expansions from the influence of the stll necessary as at midnight. Several hypoth- upon the exposed surface of the ground. eses have been advanced to account for It is very generally believed, that our this remarkable darkness, such as an erup- winds are more variable, our weather tion of a volcano in the interior of the more subject to sudden changes, our ancontinent, the burning of prairies, &c., nual amount of snow less and our mean but by the one advanced in the preceding annual temperature higher than when article, it receives an easy explication. the settlement of the country was comThe regions at the southwest are known menced. And causes, which would proto be extremely productive, and to have duce these changes, would, we believe, been, at that period, deeply covered with be sufficient to destroy, in a great measforestsand plants,whose leaves andperish- ure, the peculiar features of our Indian able parts would be sufficient, during their Summers. The variableness of the winds, decay, to fill the atmosphere to almost any occasioned by cutting down large porextent; and nothing more would be neces- tions of the forests, would of itself be sary for the production of the phenome- sufficient to scatter and precipitate those non, than a change of atmospheric press- brooding oceans of smoke, and prevent ure, which should produce a sudden con- the long continuance of those seasons of densation, and a southwesterly wind. dark and solemn stillness, which were, in Indian Summer.-It has been said, ages that are past, the unerring harbinthough we do not vouch for its truth, that gers of long and dreary winters and deluit was a maxim with the aborigines of this ges of snow. country, which had been handed down Meteors and Earthquakes.-Upon these from time immemorial, that there would subjectsVermont affords nothing peculiar. be 30 smoky days both in the spring and The common phenomenon of shooting autumn of each year; and their reliance stars is witnessed here as in other parts of upon the occurrence of that number in the country, and those uncommon disautumn was such that they had no fears plays which have several times occurred of winter setting in till the number was about the 13th of November, have been completed. This phenomenon occurred observed from various parts of the state. between the middle of October and the In addition to these, several of those rare middle of December, but principally in meteors, from which meteorolites or meNovember; and itbeing usually attended teoric stones are thrown, have been noby an almost perfect calm, and a high ticed, but the records of them are few and temperature during the day, our ances- meagre. These meteors make their aptors, perhaps in allusion to the above pearance so unexpectedly and suddenly, maxim, gave it the name of Indian Sum- and continue visible for so short a period mer. But it appears that from the com- of time, that it is hardly possible to make mencement of the settlement of the coun- observations sufficiently accurate to furtry, the Indian Summers have gradually nish data for calculating their velocity, become more and more irregular and less distance or magnitude.'That most restrikingly marked in their character, un- markable meteor which passed over New til they have almost ceased to be noticed. England in a southerly direction in the Now upon the hypothesis advanced in thei mornirg of the 14Ath of' December, 1807, CrtrP. 1, DESCRIPTIVE GEOGRAPHY. 17 REMARKABLE METEORS. ~ REMARKABLE METEORS. and from which fell large quantities of from the rest of New England, and from meteoric stones in Weston, Connecticut, New York and Canada, about 10 o'clock was seen fromRutland in this state,and the in the evening of the 9th of March, 1822. observation there made formed one of the From observations made at Burlington elements in Dr. Bowditch's calculations and Windsor, Prof. Dean computed its of its velocity, distance and size. A me- course to be S. 350 W., its distance from teor of the same kind passed over New Burlington 59 miles and from Windsor 83 England and New York in a southwest- miles, and its height above the earth about erly direction a little before 10 o'clock in 37 miles when it first appeared, and when the evening of the 23d of February, 1819, it disappeared its distance from Burlingand was seen from many parts of Ver- ton was 144 miles and its distance from mont. We had the pleasure of witness- Windsor 133 miles and its height 29 miles. ing it at Bridgewater in this state. The According to these computations, at the meteor there made its appearance about first appearance of the meteor, it was ver100 south of the zenith, and, descending tical over the unsettled parts of Essex rapidly towards the southwest, it disap- county in the state of New York, and at peared when about 250 above the horizon. its disappearance, it was over the western Indeed, its velocity was such over Wind- part of Schoharie county in the same sor and Rutland counties as to give to all, state. who observed it, though at the distance of Several other meteors of this kind have 10, 20 and even 30 miles from each other, been observed, the most remarkable of along the line of its course, the impres- which was seen from the northern part of sionthat its fall was nearly perpendicular; the state and from nearly the whole of and each observer supposed that it fell Lower Canada, about 4 o'clock in the within a few hundred yards of himself. morning of the 28th of May, 1834. It beNow as this meteor was probably moving ing a time when people generally were in nearly parallel to the horizon, the decep- bed and asleep, comparatively few had the tion must have arisen from the rapid dim- opportunity of seeing it. Many, however, inution of the visible angle between the were awakened by its light, and still more meteor and the horizon, occasioned by the by its report. Residing then at Hatley in great horizontal velocity of the meteor in Canada, which is 15 miles north of the its departure from the zenith of the ob- north line of Vermont at Derby, we were server. These facts should teach us to suddenly awakened by a noise resembling guard against the illusions of our own that of a large number of heavy carriages senses and to admit with caution the tes- driven furiously over a rough road or timony of others respecting phenomena pavement, and by a shaking of the house, of this nature. which caused a rattling of every door and According tothe best of our judgment, window. ~ Supposing it to he an earththe meteor was visible three or four sec- quake, we sprung out of bed and reached onds, in which time it passed through an the door two seconds at least before the arc of near 50~ of the heavens. Its ap. sound ceased. The atmosphere wascalm parent diameter was about 20', or two and the sky was perfectly clear, with the thirds that of the moon, and the color of exception of a narrow train of cloud or its light was very white and dazzling, like smoke,extending from southwest to norththat of iron in a furnace in a state of fu- east, and at considerable distance to the sion. It left a long train of light behind northward of the zenith. It was nearly it, and just at the time of disappearance a motionless, and was apparently at a vastly violent scintillation was observed, and the greater height than clouds usually lie. fragments detached continued luminous Indeed there was something so peculiar at considerable distance from the main in its appearance as to nake it the subbody of the meteor, but no meteoralites ject of remark and careful observation till are known to have fallen. Five or six after sunrise, when it gradually vanished, minutes after the disappearance of the although at this time we had no reason to meteor, a very distinct report was heard suspect its connexion with the noise and accompanied by a jarring of the earth, like shaking of the earth, which had awakenthe report of a cannon at the distance of ed us. We,.however, soon learned that five or six miles. Now, assuming the a remarkable meteor had been seen, and correctness of the above data, and that that its course lay along the very line octhe report was given at the time of the cupied by the remarkable cloud above scintillation, the distance of the meteor mentioned. From an intelligent young was then between 70 and 80 miles, and man, who was fishing at the time on Masits diameter about one third of a mile. suippi lake in Hatley, and who had a full Another, and still more remarkable me- view of the meteor during the whole time teor, was seen from this state as well as it was visible, we learned that it made its PT. I. 3 18 NATURAL HISTORY OF VERMONT. PART 1. NEW ENGLAND EARTHQUAKES. AURORA BOREALIS. appearance at a point a little north of horizon towards a point not far from the west at an elevation of about 35o, passed zenith; but at times it assumes forms as the meridian at a considerable distance various and fantastic as can well be irnorth of the zenith and disappeared in the agined, and exhibits all the colors of the northeast with an altitude of about 250. rainbow. It is not uncommon that it takes He thought its apparent magnitude to. be the form of concentric arches spanning the 8 or 10 times that of the moon, and that heavens from west to east, usually at the' it was visible about 10 seconds. It was north, but sometimes passing through the of a fiery red color, brightest when it first zenith, or even at considerable distance appeared;and gradually decreased in brill- to the south of it. At times the meteor is iancy, all the time throwing off sparks, apparently motionless, but it is nQt anuntill it disappeared. About 4 minutes af- common thing for it to exhibit a violent ter the vanishing of the meteor, a rumb- undulating motion like the whipping of a ling or rattling sound, which sensibly flag in a brisk wind. But it is sovariable agitated the surface of the lake, corm- in itsappearance, that it is vain toattempt menced in the point where the meteor its description. We will, however, menwas first seen, and following the course tion a few of the remarkable occurrences of the meteor died away at the point where of this meteor which have fallen under the meteor vanished. This meteor was our own observation, and some of the atvertical on a north and south line,about 50 tending circumstances. miles to the northward of Derby in this On the 12th of October, 1819, at about state, or nearly over Shipton in Canada, 7 o'clock in the evening, the Aurora Boand its altitude must have been at least realis assumed the form of three luminous 30 miles, and still the agitation it pro- resplendant arches, completely spanning duced in the atmosphere was such as to the heavens from west to east. The lowbreak considerable quantities of glass in est arch was in the north a little below the windows at Shipton, Melbourne and the pole star, the second about midway some other places. The course of this between the pole star and the zenith, and meteor was mostly over an unsettled the third 10~ or 15o to the southward of country. The most remarkable circum- the zenith. These belts gradually spread stances attending this meteor were the out till they became blended with each train of smoke which it left behind, and other, and the whole concave heavens was the long continued noise and shaking of lit up with a soft and beautiful glow of the earth. white light. It would then concentrate Since the settlement of New England, to particular points whose brightness there have been recorded a considerable would equal that of an ordinary par, number of earthquakes, and several have helion, and around them would be exhibbeen noticed in Vermont. The sound ited the prismatic colors melting into each accompanying these is usually described other in all their mellow loveliness. The as having a progressive motion; and that, motions of the meteor were rapid, undu. and the shaking of the earth have been latory and from north to south varying a supposed to be produced by the rushing of little towards the zenith. The sky was steam through the cavities in the interior clear and of a deep blue color where it of the earth, but the effect known to have was not overspread by the meteor. It was been produced by the meteor last de- succeeded in the morning of the 13th by scribed, furnishes strong reasons for sus- a slight fall of snow with a northwest pecting that the cause of many, and per- wind. The aurora exhibited itself in a haps of all the earthquakes which have manner very similar to the above in the occurred in New England, has been in evening of the 3d of April, 1820, and sev. the atmosphere above instead of the earth eral times since. beneath. Had this meteor passed with- But the most remarkable exhibition of out being seen, the sound and shaking of this meteor, which has fallen under our the earth, which it produced, would have own observation,was in the evening of the been regarded as a real earthquake, and 25th of January, 1837. It first attractits origin in the atmosphere would not ed our attention at about half past 6 have been suspected.. o'clock in the evening. It then consisted Ilurora Borealis.-This meteor has been of an arch of faint red light extending very common in Vermont, ever since the from the northwest and terminating nearly first settlement of the state; but in some in the east, and crossing the meridian 15 years it is of more frequent occurrence, or 20~ north of the zenith. This arch and exhibits itself in a more interesting soon assumed a bright red hue and gradand wonderful manner than in others. Its ually moved towards the south. To the mostcommon appearance is thatofstreams northward of it, the sky was nearly black, of white light shooting up from near the in which but few stars could be seen. Next Chap. 1. DESCRIPTIVE GEOGRAPHY. 19 AURORA BOREALIS. MAGNETIC VARIATION. to the red belt was a belt of white light, This meteor,when very brilliant, is usually and beyond. this in that direction, the sky regarded as an indication of an approachwas much darker than usual, but no clouds ing storm, but, like other signs, it often were any where to be seen. The red belt, fails. It is most common in the months increasing in width and brightness, ad- of March, September and October, but it vanced towards the south and was in the is not unusual in the other months. zenith of Burlington about 7 o'clock. The.Magnetic Variation.-Very few obserlight was then equal to the full moon, and vations have hitherto been made in Verthe snow and every other object from mont for the purpose of determining the which it was reflected, was deeply tinged variation of the magnetic needle, and with a red or bloody hue. Between the these few have generally been made with red and white belts, were frequently ex- a common surveyor's compass, and, probhibited streams of beautiful yellow light, ably, in most cases, without a very corand to the northward of the red light rect determination of the true meridian; were frequently seen delicate streams of and hence they cannot lay claim to very blue and white curiously alternating and minute accuracy. But since such obserblending with each other. The most vations may serve to present a general prominent and remarkable belt was of a view of the amount and change of variablood-red color, and was continually va- tion, since the settlement of the state, we rying in width and intensity. At eight have embodied those to which we have o'clock, the meteor, though still brilliant, had access, in the following table. had lost most of its unusual properties. JMagnetic Variation in Vermont. Place of Observation. Date. Vari. west. Latitude. Lon.w.G'fi Authorities. Burlington, 1793 70 38' 440 28' 73" Dr. S. Williams. "6 1818 7 30 "c J. Johnson, Esq. 1822 7 42 " " e; 1830 8 10 " " 1831 8 15 " "c 1 1832 8 25 41' "2 1834 8 50. "6 1837 8 45 " "4 Prof. Benedict. 1840 9 42 C cc J. Johnson, Esq. Rutland, 1789 7 3 43 37 72 Dr. S. Williams. "C 1810 6 4' "4 cc 1811 6 1 C':" cc Ryegate, 1801 7 0 44 10 72 Gen. J. Whitelaw, Holland, 1785 7 40 45 0 71 " 4 St. Johnsbury, 1837 9 16 44 26 71 Prof. A. C. Twining. Barton, 1837 10 51 44 44 cc Montpelier, 1829 12 25 44 17 72 Exec. Documents. Pownal, 1786 5 52 42 46 72 Dr. S. Williams. Canaan, 1806 9 00 45 0 71. ( From repeated observations and from lMagnetic Variation at Burlington. a careful examination of the lines of the Year Var.w Year. Var.w Year. Var.w Year. Var.w original surveys, John J ohnson,Esq.was - of the opinion that in 1785, the westerly 1785 7012' 1800 6027' 1815 7~12' 1830 8o42' variation at Burlington was about 7o 1786 7 9 1801 6 24 1816 7 18 1831 8 48 12' and that it diminished till the year 1787 7 61802 6 21 1817 7 24 1832 8 54 1805 when it was about 6~ 12". From 1788 7 31803 6 181181 7 301833 9 0 1805 the variation has been increasing 1789 7 0 1804 6 151819 7 36 1834 9 6 nptothepresenttime, 1842; andisnow 1790 6 571805 6 12 1820 7 42 1835 9 12 9~ 54. This would give a mean annual 1791 6 54 1806 6 18 1821 7 48 1836 9 18 change of variationof6' since 1805, and 1792 6 51 1807 6 24 1822 7 54 1837 9 24 of 3' previous to that time. And al- 1793 6 481808 6 30 1823 8 0 1838 9 30 though he thought the change of varia- 1794 6 451.809 6 36 1824 8 6 1839 9 36 tion may not have been perfectly uni- 1795 6 421810 6 42 1825 8 12 1840 9 42 form, yet he was of opinion that a table 1796 6 391811 6 4811826 8 18 1841 9 48 constructed with the above variation 1797 6 361812 6 5411827 8 24 1842 9 54 would not differ materially from the 1798 63418137 0 1828 830 1843 10 0 truth. The following is such a table. 1799 6 30 1814 7 611829 83611844 10 6 20 NATURAL HISTORY OF VERMONT. PART. I REMARKABLE SEASONS. GREAT FRESHET. COMPARISON OF CLIMATES. Remarkable Seasons. —Although the July 15. Thursday,... 940 mean temperature of Vermont has not " 16. Friday,.... 92 usually varied much from year to year, " 17. Saturday,... 921 yet seasons have occasionally occurred, " 18. Sunday,... 92 which became, for a time, proverbial on " 19. Monday,... 90 account of their unusual coldness, or heat,' 20. Tuesday,. 91 or on account of an excess or deficiency " 21. Wednesday, 94 of snow or rain. Of the years, which Nor was the heat much diminished in were remarkable on any of these ac- the absence of the sun. In some cases counts in early times, we have no accu- the thermometer stood as high as 800 rate records. But it is universally con- during the whole night, and it sunk but ceded that the year 1816, was the coldest, little below 80' during any part of the and perhaps the dryest during the early time included in the above table. Another part of summer, ever known in Vermont, such succession of hot days and nights although we have no meteorological ob- was perhaps never experienced in the servations for that year, and are therefore state. From the 15th up to Saturday the unable accurately to compare the temper- 24th, the weather was for the most part ature of its seasons with other years. clear and calm. On Saturday afternoon, Snow is said to have fallen and frosts to the rain commenced and continued with have occurred at some places in this State only short intermissions, till Thursday in every month of that year. On the 8th following. During the 5 days from Satof June, snow fell in all parts of the State, urday noon to Thursday noon, the fall of and upon the high lands and mountains, water at Burlington, exceeded 7 inches, to the depth of five or six inches. It was and of this 3.85 inches fell on the 26th in accompanied by a hard frost, and on the the space of about 16 hours, and this. is morning of the 9th, ice was half an inch believed to be one of the greatest falls of thick on shallow, standing water, and water, in that length of time, ever known icicles were to be seen a foot long. The in Vermont. The Winooski, which was weather continued so cold that several most affected of any of our large streams, days elapsed before the snow disappear- was at its greatest height in the afternoon ed. The corn, which was up in many of Tuesday the 27th, and was then from places, and other vegetables, were killed 4 to 20 feet, according to the width of the down to the ground, and, upon the high channel, higher than had ever before been lands, the leaves of the trees, which were observed. Although the county of Chitabout two thirds grown, were also killed tenden, and the northern parts of the and fell off. The summer was not only county of Addison, seemed to bethe secexcessively cold, but very dry. Very tion upon which the storm spent its greatlittle Indian corn came to maturity, and est force, yet its disastrous effects were many families suffered on account of the felt with unusual severity throughout the scarcity of bread stuffs and their oonse- valley of lake Champlain, and in all the quent high prices. northern and central parts of the state, The year, 1828, was nearly as remark- and the destruction of property in bridges, able for warmth as 1816 was for cold. mills, buildings and growing crops was The mean temperature of all the months great, almost beyond computation. But of this year, with the exception of April, its most melancholly effect was the dewas higher than their average mean, and struction of human life. By a change of the temperature of the year 3Q higher than the channel of New Haven river, in the the mean of the annual temperatures town of New Haven, during the night, which have been observed. The broad between the 26th and 27th, several buildparts of lake Champlain were not frozen ings containing families were insulated, over during the winter. and afterwards swept away by the waters. The year 1830 was distinguished on ac- Of 21 persons, who were thus surprized count of the great quantity of water which and washed away, 7 only escaped; the fell in rain and snow, and especially for remaining 14 found a watery grave.' one of the most extensive and destruc- The whole quantity of water which fell tive fteshets ever known in Vermont. at Burlington, in 1830, measured 59.3 in. Up to the 15th of July, the weather was being half as much again as the mean ant exceedingly cold as well as wet. It then nual quantity, and probably exceeding changed, and became suddenly and ex- the amount in any other year since the cessively warm. The following table state was settled. shows the height to which the ther- Comparative view of the Climate.-As mometer rose in the shade, on each day Vermont extends through 2Q 16' of lati. from the 15th of July to the 21st, inclu- tude, there is, as might be expected, a sBive. * See part III. Article, New Haven. CHAP 1. DESCRIPTIVE GEOGRAPHY. 21 CLIMATE OF AMERICA AND EUROPE. CAUSES OF'DIFFERENCE. sensible difference between the tempera- ical observations. A comparison of the ture of the northern and southern parts, journals kept in this country with those and there is a difference still more mark- kept in Europe shows us that the climate ed between the elevated and mountainous of Vermont, which lies in the latitude of parts and the lower country along our the southern part of France, is as cold as lakes and rivers; but observations are too that of Denmark, situated 11 or 120 furlimited to enable us to form any accurate ther north. The following table exhibits comparison between the different sections pretty nearly the mean temperatures aof the state.* Between the climate of this long the coasts of the two continents, with state and that of those portions of other the differences, from the 30th to the 60th states, lying in the same latitude, there is degree of latitude. no material difference, with the excep- Table. tion, perhaps, of the sea-coast of New Hampshire and Maine, whose mean an- Lati- Europe. America. Diffiernual temperature may be a little higher. tude. Mean Temp. Mean Temp. ences. But between Vermont and the countries 300 70.1 66.8_ 3 of Europe, lying in the same latitude, 35 66.5 60.5 6.0 there is a remarkable difference, the tem- 40 63.1 54.2 8.9 perature of the latter being no less than 4 5 56.8 45.0 11.8 11J~ higher than ours; and there is a 50 50.8 37.9 12.9 like contrast, increasing towards the 55 46 0 280 18.0 north, between the whole western coast 60 46 0 28.0 18.0 of Europe and the eastern coast of North 60 40.0.0 America. A contrast so remarkable, as is exhibitThis singular contrast was observed by ed in the preceding table, has been the the earliest navigators, who visited the source of much speculation, but, as it apcoast of North America, and has since pears to us, without throwing much light been confirmed by numerous meteorolog- upon the true cause of the phenomenon. Among the earliest writers who at* As the extremes of heat and cold were not no- tempted to account for it was Father Brested in the preceding meteorological tables, we have collected in the following table the extremes of ani, an Italian Jesuit, who spent most of cold which have been entered at sun-rise upon his life in Canada. He says that "' a cerjournals kept at three different places within the tain mixture of dry and moist makes ice, state since 1829. Degrees in all cases below zero. and that in Canada there is a remarkable and that in Canada there is a remarkable Year. Williamstowcn. Burlington. Hydepark. mixture of water and dry sandy soil; and... _-........._ hence the long duration of cold and great 1829 Feb. 5. 11~ quantities of snow." To this he-adds an1830 Jan. 31, 18 other cause, which is "the neighborhood 1831 Dec. 22. 18 Dec. 14~ 1831 Feb.24) 22 Jan.26, 16 of the northern sea, which is covered 1833 Jan. 19, 26 Jan. 19, 20 Dec.15, 12~ with monstrous heaps of ice, more than 1834 Dec. 15, 18 Jan. 24, 28 8 months of the year." FatherCharlevoix, 1835 Feb. 4, 24 Jan. 4, 36 1836 Feb. 2, 26 Feb. 18, 34 who visited Canada in 1720, and from 1837 Jani 4, 16 )ec. 22, 15 Jan. 26, 34 whose travels the forgoing opinions of 1838 Dec. 13, 15 Jan. 21, 13 Feb. 2, 22 Bresani are taken, says* that, in his opin184039 Jan24, 24 Jan.24, 16 F ion," " no person has explained the cause, 1840 Jan. 16, 17 Jan. 18, 16 1841 Feb. 9, 9 Jan. 4. 10 why this country is so much colder than France in the same latitude." cc Most It wduld appear from various observations and France in the same latitude." "Most circumstances, that during calm weather, when writers," he continues, "attribute it to the sun does not shine, the temperature of vallies the snow lying so long and deep on the and low situations is lower than that of the high ground. But this only makes the difficullands, but in windy weather and when the sun Whence those great quantishines, it is coldest on the high lands. In confir- ty worse. Whence those great quantimation of this statement, in part, we give the fol- ties of snow?" His own opinion is that lowing extract of a letter to the author from the the cold and snow are to be attributed to Hon. Elijah Paine, of Williamstown, (see pages 9 the mountains, woods and lakes. Many andl 10.) " I have found," says lie, " that in extremely cold, still weather, the mercury in the European writers have supposed the great thermometer at Burlington, Montpelier, at North- lakes, which abound in the country, to field, on Dog river, on the low lands at the cause of the coldness of our climeeting-house in this town, at Woodstock, Hanover, N. H., and even at Albanv, N. Y., has some- mate; while others have imagined that times been 14 degrees lower than in mine. Some- there must be a chain of very high mountimes, even in March, I have found the difference tains in the interior of the continent runequally great, when the wind was light and the from s weather very cool for the season. But the reverse ning from southwest to northeast, which is the case in extremely cold, windy weather. I produce the coldness of our north westerhave known my thermometer in such weather 11 ly winds. Doct. Dwight supposes these degrees lower than some of those I have mentioned." * Charlevoix's Travels in America,Vol. 1. p. 136 NATURAL HISTORY OF VELMONT. PAT I. CHAXGE OF CLIMATE. CURRENTS OF THE OCEKAf. winds to be- descending currents from the of June, when the temperature of the air higher regions of the atmosphere; and was 48Jo, that the temperature of the hence their coldness. Doct. Holyoke at. ocean at the depth of 4680 feet, was 26, tributed the coldness of our climate to the or 60 below the freezing point. On the extensive forests of evergreens. Doct. 31st of August, in latitude 69~ where the Williams, the able historian of Vermont, annual temperature is 38', that of the air attributed it to the forest state of the being 59~0, the temperature of the water country, and has endeavoured to prove at the depth of 4038 feet was 320.* At that, eighteen centuries ago, the climate the tropic where the temperature does of Europe was even colder than that of not vary more than 7~ or 8~0 during the America at the present time.* But other year, at the depth of 3600 feet the temwriters have, with equal plausibility, perature of the water was found to be onshown that no considerable change has ly 530, while that of the air was 84~, taken place in the mean temperature of making a difference of 310,and indicating Europe within that period.t The fact, a degree of cold in the lower parts of the moreover, that the western coasts of ocean nearly 250 more intense than is ever America, which are wholly uncultivated, experienced in the atmosphere in that are very much warmer than the eastern latitude,t How else can we account for the coasts of Asia in the same latitude, which coldness of these waters, but by supposare cultivated to considerable extent, ing them to come from higher latitudes in shows that these differences of tempera- the manner we have described? ture do not depend upon cultivation, nor, Of the opposite motion of the warmer indeed, upon any of the causes which waters along the surface of the Atlantic have been mentioned, but upon some more ocean, from the equatorial towards the general cause. And this cause, we be- polar regions, the gulfstream, the currents lieve, is to be sought in the influence of setting along the western coasts of Northe ocean upon the prevailing winds in way, and the vast quantities of tropical high northern latitudes. We regard the productions, lodged upon the costs and ocean as the great equalizer of tempera- islands of the northern ocean, afford ature upon the surface of our globe-as the bundant proof. instrument for distributing the heat of Now this transportation of the colder the equatorial regions towards the poles waters towards the equator and of the and bringing thence cold towards the warmer waters towards the poles, serves, equator, and thus meliorating the climate as already remarked, to mitigate the otherofboth. We look upon it as a truth es- wise intolerable heat of the former, and tablished both by theory and fact that the excessive cold of the latter; and afthere is a general circulation of the wa- fords an obvious manifestation of the wisters of the ocean between the equatorial dom and goodness of providence. And and polar regions-that the warm water it is to the influence of the warm superfifrom the equator is flowing along the sur- cial waters of the ocean, which have face of the ocean towards the poles, while come from tropical regions, upon the the colder water from the poles is ad- winds, or currents of the atmosphere, that vancing along the bottom of the ocean to- we are to look for the cause of the differwards the equator. Such a motion of the ence of temperature in the climate of the waters might be inferred, as the result of eastern coasts of North America and the the unequal distribution of heat through western coasts of Europe, and also in that the oceanic mass, increased by the rota- of the eastern coasts of Asia and the westtion of the earth on its axis. But inde- ern coasts of North America. If we obpendent of this, facts furnish indubitable serve the gulf stream, which is only a proof of its, existence. The temperature concentration by the trade winds of those of the earth, at a distance below the sur- warm waters which are flowing northerface, being a pretty correct index of the ly along the surface of the ocean, we mean temperature of the climate, with- shall perceive it to be very narrow, preout the circulation we have supposed, the senting to the atmosphere only a small temperature of the ocean at consider- surface of its warm water, while near the able depths, ought, particularly in the American coast. But as it proceeds to warmer parts of the year, to be as the northeast its warm waters are spread high, at least, as the mean annual tem- out upon the surface of the ocean and are perature. But on the contrary, observa- thrown directly along or upon the westtion proves it to be much lower. In lati- ern coasts of Europe. Observation also tude 67~, where the mean temperature is shows that the prevailing winds in high 390, Lord Mulgrave found, on the 20th northern latitudes, are from a north west* Williams' History of Vermont, Vol. 1, p. 475. * Count Rumford's Essays, Vol. II. page 304. t Edinburgh Review, Vol. XXX, p. 25. tPhil. Transactions, 1752. CrAP. ~2. QUADRUPEDS OF VERMONT. 23 CLASSIFICATION OF ANIMALS. ORDERS OF *IAMWAIiLI. erly direction, or passing nearly at right ice the greater part of the year; and angles across the great northeasterly cur- hence they are excessively cold In their rent of the ocean, and we believe it to be progress over the Atlantic, they are gradthe influence of these warm waters of the ually warmed by imbibing heat from the ocean upon the westerly and northwester- surface of the ocean, so that w. hen they ly winds,which produces the phenomenon arrive upon the continent of Europe, their in question. On the eastern coasts of temperature is so much elevated as to North America, these winds come from produce the remarkable differen'eebsetmountainous, snowy regions, or from ved between the climates of the coasts of lakes and seas, which are covered with the two continents.* CHAPTER II. QUADRUPEDS OF VERMONT. Preliminary Observations. tion in an abdominal pouch, which inclos. All animals are divided by Baron Cu- es the teats, of which the opossum is a vier, the celebrated French naturalist, example. whose arrangement we shall endeavor V. Rodentia —have large incisory teeth mainly to follow, into four general divis- suitable for gnawing, and grinders with ions, viz. I. Vertebrated animals, or such flat or tuberculated crowns, but no canine as have a spine, or back bone, II. NMolus- teeth, as the rat, beaver, &c. cous animals, or such as have no skele- VI. Edentata-,having no incisory teeth ton, III. Articulated animals, whose trunk in either jaw, and in some genera no teeth is divided into rings, and IV. Radiated at all, of which the sloth and ant eater animals, or zoophytes. The first division are examples. embraces the mammalia, the birds, the rep- VII. Packydermata-having either tiles and the fishes; the second, the shell three or two kinds of teeth, toes variable fishes; the third, the insects, and the in number and furnished with strong fourth, polypi. In this work we shall at- nails or hoofs, and the digestive organs tempt but little beyond an account of our not formed for ruminating, as the horse vertebrated and moluscous animals. elephant and hog. VIII. Ruminantia-having no incisory MAMMALIA. teeth in the upper jaw, cloven hoofed The Mammalia are such animals as feet, and four stomachs fitted for xuminasuckle their young, and are divided by ting, or chewing the cud, as the oxt Cuvier into the following orders: sheep, deer, &c. I. Bimana-having two hands and three IX. Cetacea-Aquatic animals having kinds of teeth. Man is the only species. their bodies shaped like fishes, as the II. Quadrumana-nanimals having four whale, dolphin, &e. hands and three kinds of teeth. Mon- Of these nine orders of animals, only kies and baboons belong to this order. three are found in Vermont, in a wild III. Carnivora-having three kinds of state. These are the Carnivora, the Roteeth and living principally upon animal dentia and the Ruminantia. We have one food, as the dog, cat, &c. order more, the Pachydermata, among IV. MJarsupialia-producing their young our domestic quadrupeds, including the prematurely and bringing them to perfec- horse, ass and hog. * Mr. Daniels in his meteorological essays en- coasts contain little vapor to be condensed, and deavors to account for the higher temperature of consequently do not produce an elevation of temthe western coasts of continents in a different perature. If this were the principal cause of the manner. He supposes the northwesterly winds phenomenon under consideration, the quantity of to arrive loaded with vapor and that the caloric, rain on the western coasts should be greater than liberated by its condensation, raises the general upon the eastern in proportion as the temnperature temperature of the atmosphere on the western is higher, but so far as observations extend the recoast; but, as the winds proceed eastward, they verse of this seems to be true, the quantity of rain become dryer and when they reach the eastern on the eastern coast being greatest. 24 NATURAL HISTORY OF VERMONT. PART I, CATALOGUE OF QUADRUPEDS, CARNIVEROUS ANIMALS. BATS, QUADRUPEDS OF VERMONT. GENUS VESPERTILIO.-LinntaUs. The following is a catalogue of the-na- Generic Characters.-Teeth from 32 to 36,tive quadrupeds of Vermont, arranged innCiSOrS 6, canines 11 grind 4-4, 5 5 to6' the order, in which they are described in Upper incisors in pairs, cylindrical and pointed; the following pages: the anterior grinders simply conical, posterior having short points or prominences. Nose, ORDER,CARNIVORA-CarniVerous Animals. simple, without grooves, or wrinkles; ears, with an auriculuti, lateral and more or less large; Vespertilio subulatus, Say's Bat. tongue smooth, and not protractile; index finger " pruinosus, Hoary Bat. with but one phalanx, the middle with three, the " carolinensis, Carolina Bat. annular and little finger with two; tail comprised " noctivagans, Silver-haired Bat. in the interfemoral membrane; sebaceous glands Sorex Forsteri, Forster's Shrew. under the skin of the face, which vary in different " brevicaudus, Short tail Shrew. species. Scalops canadensis, Shrew Mole. The bats consist of a great number of Condylura macroura, Star-nosed.Mole. species, but they agree very nearly in, Ursus americanus, Black Bear. their general form and habits. They proProcyon lotor, Raccoon. duce and nourish their young in the manGulo luscus, Wolverene. ner of other quadrupeds, but unlike them.Justela vulgaris, Weasel. they are furnished with delicate mem"& erminea, Ermine. branous wings upon which they spend " vison, Mink. much of their time in the air, thus seemc" canadensis, Fisher Martin. ing to form the connecting link between ~" martes, Pine Martin. the quadrupeds and birds. They are nocfephitis americana, Skunk. turnal in their habits, }ying concealed Lutra brasiliensis, American Otter. during the day, but venturing abroad on Canis ulvus, Wolf. the approach of evening, during the early -" ful us, Red Fox. part of which they may be seen flitting aar. decussatus, Cross Fox. lightly and noiselessly through the air in s aar.can entatus, Blacky orSilverFox. quest of food, which consists chiefly of inFSelis canadensis, Lynx. sects. At such times they often enter " rufra, Bay Lynx. the open windows of our dwellings and " concolor, Catamount. sometimes commit depredations upon our Phoca vitulina, Common Seal. larders, being exceedingly fond of fresh meat. Their nocttirnal habits manifest ORDER RODENTIA-Gnawing.Animals. themselves in the domesticated state as Castor fiber, Beaver. well as the wild, and it is with difficulty Fiber zibethicus, Musk Rat. that they are made to mount upon their Alrvicola riparius, Meadow Mouse. wings, or take food during the day., but Alus decumanus, Norway Rat. in the evening they devour food vora" rattus, Black Rat. ciously and fly about the room without " musculus, Common Mouse. reluctance. On the approach of winter Gerbillus canadensis, Jumping Mouse. bats retire to dry caverns and hollow trees Arctomys monaz, Woodchuck. where they suspend themselves by the 8ciurus cinereus, Gray Squirrel. hooked nails of their hind feet, and thus 4 niger, Black Squirrel. remain in a torpid state during the win" hudsonius, Red Squirrel. ter. They void their excrement, which " striatus, Stiped Squirrel. is found in abundance in these retreats, Pteromys volucella, Flying Squirrel. by reversing their position and suspendHystrix dorsata, Hedge Hog. ing themselves by the hooks upon their Lepus americanus, Rabbit. thumbs till their object is accomplished, " virginianus, Hare. when they resume their former position. FORDER RUIMSNA:NTsA-Rum~inatiZg Animals. Bats produce their young in June or July, and have from one to three at a time. Cervus alces, Moose. The teats of the female are situated on 44 canadensis, Elk. the chest and to these, as we are assured,' virginianus, Common Deer. by Dr. Godman, (Nat. His. I. 56.), the young attach themselves so firmly as to be carried about by the mother in her ORDER CARN1VORA. flight, till they have attained a consideraThe animals of this order have three ble size. The four following species are kinds of teeth, a simple, membranaceous all that have hitherto been distinguished stomach, and short intestines. They live in Vermont. It is, however, probable principally on flesh, or animal food. that othersmay hereafter be detected. CHAP. 2. QUADRUPEDS OF VERMONT. 25 S&Y'S BAT. HOARY BAT. CAROLINA BAT. and at the central part of the inside, tragus bent, club-shaped and blunt at the tip. Canine teeth large and prominent; incisors in the upper jaw conical with a tubercle near the base, very near the canines, and nearly in a line with them;.snout cartilaginous and moveable; nostrils wide apart. Eyes black and prominent. Fur on the body blackish brown at its base, then pale brownish yellow, then brownish and terminated with clear, Vespertilio subula.tus.-SAY. delicate white, like hoar frost; fur on the DESCRIPTION.-Head short, broad and throat, on and about the ears, and on the flat; nose blunt with a small, flat, naked inside of the wings towards their base, muzzle; eyes small, situated near the fulvous; snout, chin, margin of the ears ears and covered with fur; ears longer and the posterior part of the wing memthan the head, thin ovate, obtuse and brane, blackish; the anterior part of the hairy at the base behind; tragus thin, wings and the base of the fur on the inbroadly subulate below, tapering upwards terfemoral membrane, dark chestnut. and ending in an obtuse tip, at about two Tail, wholly embraced in the interfemoral thirds the height of the ear; color of the membrane, which is thickly covered with back yellowish brown, the belly yellow- fur, except at the very posterior extremiish gray; fur soft and fine, and blackish ty. Length of the specimen before me, towards the roots; head covered with from the snout to the extremity of the fur, excepting about the nostrils; color tail, 5J inches; spread of the wings, when blackish about the mouth; whiskers few, fully extended, 16~ inches. short and stiff; membrane between the HISTORY.-This bat was also first dehind legs broad, thinly covered with scribed by Say in Long's expedition and fur next the body, and tapering to a point has since been minutely described by near the extremity of the tail, which it Richardson,* Coopert and others. It has envelopes; toes of the hind feet long; been found in most parts of the United hooked thumb including the nail i of an States and was obtained by Dr. Richardson inch. Length of the specimen before as far north as]at. 540~. It is not common me, from the nose to the insertion of the in Vermont, but is occasionally met with. tail, 2 inches; tail 1 inches; spread of The onlyVermont specimen, which I have the wings, 10 inches. examined, and that from which the preHISTORY.-This Batseemsto be distrib- ceding description was drawn, was sent uted very generally through the conti- me alive by my friend, David Reed, Esq., nent. It was first described scientifically of Colhester. It was taken at his place by Mr. Say, in the notes to the account of in Colchester the latter part of October, Long's expedition, from a specimen ob- 1841, and was kept alive for some time in tained at the foot of the Rocky Moun- a large willow basket with a flat cover of tains. It was afterwards minutely descri- the same material. On opening the basbed by Dr. Richardson from specimens ob- ket, he was almost invariably found sustained on the upper branches of the Sas- pended by his hind claws from the central katchewan and Peace rivers.* Speci- part of the cover. When the basket was mens have since been obtained from Lab- open, he manifested little fear, or disposirador, Georgia, Ohio, New Hampshire tion to fly, or get away, during the day and Columbia river. It is one of the small- time, but in the evening would readily est, and, I think, the most common Bat mount on the wing and fly about the found in Vermont, especially in the cen- room, and on lighting always suspended tral mountainous parts, where it enters himself by his hind claws with his head -the houses in the evening and is easily downward. He ate fearlessly and voracaptured. The specimen, from which my ciously of fresh meat when offered to him, description was drawn was taken in Wa- but could not be made to eat the common terbury. house fly. THE HOARY BAT. CAROLINA BAT. Vespertilio pruinosus.-SAY. Vespertilio carolinensis.-GxomFFRoY. DEscRIPTION.- Earsbroad, shorter than DSCRIPTION.-Ears rather large and the head, broadly emarginate behind,hairy naked except on the back side near the on the outside more than half the length, *Fauna Bureal Americana [.p. 1. * Fauna Boreali Americana, part I. p. 4. t Annals N. Y. Lyceum of Nat. Hisi. Vol. IV. 54. PT. I. 4 I NATURAL HISTORY OF VERMONT. PART-. SILVER-HAIRED BAT. FORSTER S SHREW. head, emarginate on the outer posterior description of this Bat*, who says that "it edge, tragus shorter and less pointed than was first described in 1831. by Major Le in Say's Bat. Head long and narrow; Conte and Dr. Harlan, and that it may be canine teeth very prominent; snout, in- easily recognized by its dark black-brown terfemoral and wing membranes black fur tipped with white on.the back." It and entirely naked; a few scattering was named V. noctivagans by Le Conte hairs on the feet. Fur on the head and back and V. qudiboni, by Harlan, and the forlong and color uniform bright ferrugin- mer of these names is retained, because ous; beneath yellowish brown; last joint Le Conte's account was first published. of the tail not enveloped in the membrane. / Bones supporting the membrane very ap- GENUS SOREX.-Linnceus. parent. Length of the Specimen before Generic Characters.-Teeth variable from 26 me, from the snout to the extremity ofthe to 34. The two middle upper incisors hooked tail 4.7 inches, head and body 3 inches, and dentated at their base; the lower ones tail 1.7, fore arm 1.8, tibia.7, spread of the slanting and elongated; lateral incisors small, wings 11.5 inches. usually five on each side above, and two below; HISTORY.-Of the history of this bat I grinders, most commonly 4 on each side above, know nothing. It is said to be quite and 3 below. The body is covered with fine, common in the southern states particular- short fur; toes, five on each foot, separate, furly in the Carolinas and Georgia and also nished with hooked nails not proper for digging: on Long Island near New York. The only head and nose elongated, the latter moveable specimen I have seen and that from which ears short and rounded; eyes small but visible. the above description was made, was taken in Burlington, and deposited in the museum of the college of Natural History of the University df Vermont by Mr. John H. Morse, a student of the University. A Vermont specimen of this species is also preserved in the museum of N.at. His. of Middlebury college. FORSTER'S SHREW. Sorex Forsteri.-RICHARDSON. DESCRIPTION.-Color yellowish brown Vespertilio noctivagans.-LE CONTE. or dark olive above, bluish white or cinDESCRIPTION.-Ears dusky black, rath- erous beneath; base of the fur plumbeous er large, naked on the anterior portion, for two thirds its length both above and somewhat ovate and obtuse, with two below; teeth white at the base and at emarginations, on the outer posterior bor- their points, deep chestnut brown; tail der, produced by two plaits; naked with- long, four sided, covered with short hair in, and with the tragus moderate, ovate and terminated in a fine pencil of hairs; and obtuse. Color above, a uniform dark feet small, light flesh-colored and nearly dusky brown, approaching to black. On naked; nails slender and white; whiskers the back the fur is somewhat glossy and half an inch long, light brown. Length tipped with silvery white, forming an of the head and body 2 inches, tail 1.4, interrupted line across the shoulders, head.9,from the eye to the point of the and thence irregularly mixed down the nose.3. centre of the back. Interfemoral rem- HiSTOY.v. —This little animal is occabrane thickly hairy on the upper part be, sionally met with in our pastures and coming thinner downward and naked near fields, having their places of retreat in the border. Tip of the tail projecting stone walls and under old fences and logs. about a line beyond the membrane. Feet The specimen from which the above dehairy. Wing membrane entirely naked. scription was made was taken in BridgeBeneath very similar to the upper parts, water and is now in my possession. This though the light colored tips of the hairs shrew was first described by Dr. Richardare more yellowish. Total length 3.8 in- son who says that it is common throughout ches, tail 1 5, fore-arm 1.8, tibia.8, spread the fir countries, even as far north as the of the wings 11 inches. 67~ oflatitude and that its delicate footHISTORY.-This Bat I have not seen in steps are often seen imprinted bn the Vermont, but I am informed by my friend snow when the temperature is 40 or 50~ Prof Adams that there is a specimen of below zero.* It is also found according it, which was taken in this state, in the to Dr. Bachman on Long Island in the museum of Natural History of' Middlebu- vicinity of New York.t ry College. The above is Mr. Cooper's *Fauna Boreali, vol. I. page 6. *Annals N. Y. Lyceum Nat. His. Vol. IV. p. 9' tJournal Acad. Nat. Sci. of Phil. vol. VI. p. 386i OLP. 2. QUADRUPEDS OF VERMONT. 27'HORT-TAILED SHREW. SHREW MOLETHE SHREW MOLE. Scalops aquaticus.-LINNstus. THE SHORT-TAILED SHREW., q Scalops canadensis.-Desmarcst. Sorer Brevicaudus.-SxY. )DEscRIPTIos.-Color, grayish brown; DrxscRTPTIoN.-Color of the head, body body, plump, cylindrical and tapering and tail dark plumbeous brown above, a from the shoulders backward; nose long, little lighter beneath; lips naked fleshy terminated by a button shaped cartilage:; and flesh-colored; extremity of the snout eyes and ears concealed by the fur; fore brown, notched; teeth tipped with dark feet broad and strong, with the toes united chestnut brown at their points fading in- up to the roots of the nails; nails broad, to white at their base; feet flesh-colored, flat and strong; palms naked, bordered nearly naked and slender; nails slender, by small stiff hairs, above slightly coverwhite on the fore feet, and on the hind ed with grayishlown; hind legs and feet feet chestnut brown at the base and white slender and delicate, with slender, sharp, at the tip. The inner toe on each foot is hooked nails; tail short and covered with shortest, the outer a little longer and the hair. Length of thespecimen before me, other three nearly equal, the third being from the nose to the insertion of the tail, a little the longest. The tail is squarish, 5.3 in. tail I in. head 1.3in. largest in the middle, slightly strangula- HISTORY.-The Shrew Mole inhabits ted at the base and sparsely covered with fields and meadows, but seems to prefer short hairs.; whiskers whitish, sparse, the banks of rivers and other -wster courshalf an inch long, situated between the es. In its habits it resembles the other eye and th! snout and turned backwards. moles. Its large and powerful paws are No external ear, opening large. Total well calculated for digging in the eartli, length of the specimen before me 4-8 and by their aid it is enabled to burrow inches, to the origin of the tail 3-8, tail 1, with surprising quickness. They spend head 1-1, hind foot to the point of the most of their time in the ground, where longest nail.6. they form extensive and connected galHIsTORY.-This species of Shrew bears leries, through which they can range at a very considerable resemblance to the pleasure to considerable distances and in Shrew mole in its general appearance, various directions, without coming to but is much inferior to it in size, and dif- the surface. In excavating these gallefers from it remarkably in the structure of ries, they throw up, in a manner difficult its fore feet. As they seldom venture in- to be explained, little mounds of loose to cleared fields, very little is known of earth, by which their burrows may be detheir habits, but in the woods they are of- tected. These mounds occur at distanten seen and heard rustling among the ces, from one to three feet, and are from leaves and digging little holes into the three to six inches in height, but exhibit ground, probably in quest of food. This externally no appearance of passages inand the preceding species are occasionally to the burrows. The fur of this animal caught and brought in by cats; but they is exceedingly beautiful, being thick, fine, will seldom attempt to eat them on ac- soft and even, with delicate glossy, or silcount, probably,of their disagreeable mus- very reflections. ky odor. In addition to the foregoing we certainly have one other species, and pro- GENUS CONDYLURA.-Jlliger. bably more, but they require further examination. Generic Characters. —Teeth, 40 —Incisors A canines 4-4 grinders 4_- In the upper GsNus SCALOPS.- Cuavier. 5 5 X 3 3 jaw are two large, triangular incisors, two very Generic Characters.-Teeth 36 to 44-Incisors side a a small ones, andon.each side a large, strong caX canines 6.A or 6 6, grinders 3.3 OT 44. ne.nt canines rinders 33 nine. In the lower jaw the four incisors slant crowns of the grinders furnished with sharp tu- forward, and the canine on each side is small anrid bercles; nose long and pointed; eyes very small; pointed. Body cylindrical, clumsy, and covered no external ears; fore feet very broad and strong, with short thick fur, which is perpendicular to the with long flattened nails fit for excavating the skin; nose elongated and sometimes furnished earth; hind feet small and thin, with slender, with a membranous crest disposed in the fot m of a arched nails; tail short; body thickly covered star around the nostrils; feet five-toed; fore feet with fine, soft fur, which is perpendicular to the broad and strong, fitted for digging; hind feet Akuin; feet five toed. slender; eyes very small; no external ear. 248 NATURAL HISTORY 01 VERMONT. PART I. STAR-NOSED MOLE. THE BLACK BEAR. cases, from a white viscous fluid contained in a sack near the vent. GENUS URSUS.-Linne'us. Generic Characters -Teeth, 32 to 44,-incis.. ors 6, canines 1_-, grinders 44 to 7-. Three of the grinders on each side in each jaw, are large, with square -tuberculous crowns; the THE STAR-NOSED MOLE. other are small, most of which appear late and Condylura imacroura.-HARL&AN are shed early. Body thick, covered with strong hair; ears long and slightly pointed; toes, five, DESCRIPTION. —C olo r dark brown ap- furnished with strong, curved claws, calculated proaching to black; body cylindrical; nose for climbing or burrowing; tail, short. long, tapering and surrounded at the extremity by a fringed membrane, having twenty points; tail nearly as long as the body, strangulated at the base and then becoming suddenly enlarged as if swollen and thence tapering to a point. The tail is scaly and sparsely covered with stiff hairs. The fore legs very short; the paws large and naked, excepting the edges, which are fringed with stiff hairs; nails long and flat with cutting edges. THE BLACK BEAR. The hind feet are naked, long and narrow, and the nails, long, slender and sharp Ursus americanus.-PALLAS. resembling birds claws; eyes concealed DEscRIPTIlOR.-Color shining black; and very small; no external ear, 4 pec- hair long and not curled; nose fawn coltoral mammae; length from the nose to ored, projecting, brightest about the anthe insertion of the tail 4.7 inches, tail 2.8 gle of the mouth, and terminated by a inches, hand.7 inches, longest nail.3 inch- naked black snout; forehead slightly arches, hind foot 1. ed; ears oval, rounded at the tip and far HISTORY.-This animal being rare, its apart; palms and soles of the feet short habits are not well understood. They ap- in comparison with the brown bear; pear, however, from what is known of claws black and strong with the hairs of them, to be similar.to those of the other the feet projecting over them; tail short. moles. They are usually found about HISTORY.-The specimen from which old buildings,fences and stone-walls, and our description is drawn was killed in they occasionally find their way into Williston in 1838, and presented to the cellars of dwelling houses. I have two College of Natural History of the Universpecimens of this animal, both of which sity of Vermont. It measures 6 feet from were before me, while making out the the nose to the tail; tail 2 inches; height foregoing description. The color of one of the ears 4 inches; height to the top of is a little darker than the other, but they the shoulders 3 feet; rump 2 feet 4 inscarcely differ in any;other respects. ches. This Bear, which is found throughThey were both caught in Burlington, out all the woody parts of North America, one in 1830, in the cellar of the Rev. G. was formerly very common in Vermont, G. Ingersoll, and the other in 1840, on and continues so plentiful at the present the surface of the ground in a door-yard. day, that our Legislature continue in Their fore feet are so closely attached to force a law allowing a bounty of $5 each, their bodies, that they serve but little pur- for its destruction. It appears from our pose except for digging, and their prog- Treasurer's reports for several years past ress upon the surface of the ground, is ex- that the number of bears for which the tremely slow, labored and awkward. Like bounty has been paid has varied from 40 the shrew moles, they probably reside to 50 annually. The black bear, under most of the time in the ground and ven- ordinary circumstances, is neither very ture abroad only in the night. On ac- carniverous nor very ferocious. Its facount of their clumsiness they are fre- vorite food consists of vegetables, such as quently drowned in cisterns and tubs of Indian corn, nuts, berries and roots. But water and are sometimes brought in by when these fail, it is compelled by necescats; but cats are not fond of eating them sity rather than choice to resort to anion account of the musky odor which mal food. In such cases, impelled by they have in common with the shrew and hunger, it will sometimes attack and deshrew mole. It proceeds, as in the other stroy young cattle, sheep and hogs, but CRAP. 2. QUADRUPEDS OF VERMONT. 29 THE RACCOON. THE WOLVERENE. will seldom, if ever, attack a person ex- alternately ringed with black and. dirty cept in defence of its cubs, or when pro- white; belly lighter; tail bushy, like that voked, or wounded. The early settlers of the fox, but more tapering, surrounded of this State suffered most from them in by alternate rings of dark and yellowish consequence of their ravages upon their white, about six of each; head roundish fields of Indian corn. They entered the with the snout projecting beyond the upfields in the night when the corn was in perjaw and terminating in a smooth black the milk and broke down and devoured membrane through which the nostrils the ears with great greediness; and it open; face whitish in front, with ablack was a common business for the settlers to patch surrounding the eye and descendwatch for them with guns and shoot them ing to the lower jaw, and a black line dewhile committingtheir depredations; and scending from the forehead between the in this way large numbers were annually eyes; pupils of the eyes round; the ears killed. During the fall, when their fdod oval, rounded at the tip and the edges of is abundant, bears usually become very a dirty white color; legs short; whiskers fat, and, as the winter sets in, they retire strong. Usual length of the head and to some natural den among the rocks, or body 22 inches, tail 9 inches; height 12 uprooted trees, or into some hollow tree, inches. where they remain in a torpid state and HISToRY. —Raccoons were very plenty without food until the return of warm in all parts of Vermont, when the counweather in the spring. The female pro- try was new, and they exist in the mounduces her young during her hibernation tainonls and woody parts in considerable and has from one to five at a litter, but the numnhers at the present time. In the genmore common number is two. Their pe- eral aspect of this animal there is some riod of gestation is about 15 or 16 weeks, resemblance of the fox, but in its moveand during this time the females conceal ments it is more like the bear. It also themselves so effectually that we have no like the bear subsists both upon animal record of any being killed while pregnant and vegetable food and its destructive prothough they are often discovered while pensity is well known. It sleeps during the cubs are very small. When the bears the day in its nest in some hollow tree or first leave their winter quarters, they are among the rocks, and prowls for its prey said to be about as fat as when they retir- during the night; and is said to destroy ed in the fall, but with exercisethey short- many more animals than it consumes, ly lose their fat so as to appear in a few merely sucking their blood or eating their days much emaciated. When the bear is brain. It sometimes makes great havoc in high order he is valued for his flesh, in the farmer's poultry-yard, and being an his grease, and his skin. He is, with the excellent climber scarcely any roost can exception of the moose, the largest native be placed beyond his reach. But it probaquadruped found in Vermont, and has bly does most mischief in the fields of Inbeen frequently killed weighing from 400 dian corn, of which it is extremely fond, to 500 pounds. Their skins are worth while the corn is soft, or "s in the milk." from $2, to $4, or $5 according to their Here it breaks down and destroys much size and quality. more than it eats. The Raccoon is said to be fond of dipping its food in water beGENUS PROCYON.-Storr. fore it eats it, and hence, Linntous gave it Generic Characters.-'lTeeth 40,-Incisors the specific name of lotor, which signifies & canines 1.1 grinders 0 6 The thtee first washer. The price of the skin is variable, X 1 11. 66 from 17 to 37i cents. The largest of grinders on each side in each jaw, are pointed, these animals in Vermont, weigh about the others are tuberculated. Body low set; nose 32 pounds, according to Dr. Williams, pointed; external ears small, oval; tail long and;pointed; feet five toed; nails sharp; mammas six. who says that its flesh is eaten and considered very excellent food. GENUs GULo.- Cuvier. Generic Characters.-Teeth 36 to 38-Incisors A canines,.L_._, grinders 4_4 or 5-5.' 1 1 6 6 6 6 The three first grinders in the upper jaw, and four first in the lower are small, succeeded by THE RACCOON. a large carniverous or cutting tooth, and small tuberculous teeth further back. Body low; head Proc yon lOtOr.-CUVIER. moderately elongated; ears short and round; tail DESCRIPTrION.-General color blackish short; feet with five toes armed with crooked gray which results from the hairs being nails. $03 NATURALwHISTORY OF VERMONT. PART L THE WOLVERENE. THE WEASEL. THE WOLVERENE. with sharp. crooked claws, and glands producing a strong, fetid secretion. Gulo luscus. —SAB INE. DESCRIPTION.-Head broad and rounded; jaws like the dog; ears low, rounded and much hidden by the fur: back arched; tail low and bushy; legs thick and short and the whole aspect of the animal indicates more strength than activity. Color dark brown, passing into almost black on the back in winter with a pale reddish brown band passing from each shoulder along the flanks and meeting on the rump. Fur similar to that of THE WEASEL. the bear, but not so long nor valuable. Mustela vulgaris.-LIsNNeNs. The tail is thickly covered with long black hair. Some white marking on the Putorits vulgarism-Cuvier. throat and between the fore legs; legs DESCRIPTION.-Color above, in summer brownish black; claws strong and sharp. dull yellowish brown deepening into hair Length 2 feet 6 inches; tail (vertebrae) brown on the upper part of the head and 7 inches; tail with the fur 10 inches. nose, and yellowish white beneath, the HISTORY-This animal was occasional- brown extending in a rounded spot into ly found when the country was new, in all the white behind the angle of the mouth; parts of the state, butwas never very plen- tail next the body the same color as the tiful. For many years past, however, it has back, but darker as it approaches the exbeen known only in the most woody and tremity, where it is quite black, and the unsettled districts, and in such places it hairs terminate in a point resembling that is now extremey rare, none having been of a camel's hair p9ncil. Color in winter met with to my knowledge for several wholly white, excepting the posterior years. According to Dr. Richardson, half of the tail, which is always black, or from whose work the above description is reddish brown. Forehead flatish; ears abridged, this animal is quite common in slightly pointed; eyes small, black and the fur countries at the north, and is a lively; body long and cylindrical; tail great annoyance to the hunters, robbing short, less than half the length of the their traps of game, or of the bait, which body. Length of the head and body of they do so dexterously as seldom to be the specimen before me 8 inches; tail caught themselves.* The Wolverene is (vertebra) 2 inches. represented as being very fierce and car- HISTORY. —The Weasel, though noniverous in its disposition, and many mar- where greatly multiplied, is frequently vellous stories have been told of its cun- met with in all parts of Vermont. It is ning and artifice and gormandizing pro- generally seen in stone walls, old fences pensities,which are totally unfounded. Its and heaps of bushes. When in sight it food ordinarily consists of mice, moles, seems to be always in motion and its mohares and other small animals, seldom tions are very quick. When in a stone meddling with larger ones, excepting such wall or heap of bushes he will sometimes as have been previously killed or disabled. show himself for an instant in half a dozIt produces once a year from two to four en places in the course of half that numcubs which are covered with adowny fur ber of minutes. The weasel feeds upon of a pale cream color. It is found through- mice, young rats, young birds and birds out all the northern parts of North Amer- eggsand sometimes commits depredations ica, even as far north as the 75th degree upon the eggs and young of our domestic of latitude. fowls. It is not uncommon for it to enter the barns and granaries and cellars of the GENUS MUSTErLA.-LinnoCus. farmers in quest of food, and particularly in pursuit of mice, of which it destroys Generic Charaters.r-Teeth 34 or 38-Incls- large numbers, and on which account it ers 6 canines'1, grinders 4 4 or 5 5. 6 5. 11 5 5, 6' might be regarded as a public benefactor, Second inferior incisors on each side slightly re-were it not for its occasional depredations ceding; canines strong; grinders cutting; the upon the poultry yard. The female proanterior false grinders, conical and compressed; duces her young several times in the true grinders trilobate, the last with a blunt crown. course of the year and has from three to Body long and cylindrical; head small and oval; five at a litter. Blt notwithstanding their ears short and round; legs short; toes 5, armed *Fauna Burent fecundity,1 41 very numever become ~*Fauna Boreali, I. 41. very numerous. UCHAP. 2. QUADRUPEDS OF VERMONT. 31 THE ERMINE. THE MI~X. THE MINK..Tustela viSOn.-LINN. GMEL. Putorius zrison.-Cuvier. THE ERMINE. DESCRIPTION. —The head is depressed Mustela erminea.-LINN. GIaEL. and small; eyes small and far forward; ears low and rounded; neck and body Ptotr'ius erminea. —Cuvier. DESmR I aN.-C r both. ismelong and slender; tail round and thick:DEscRIPTIoN.-Color, both in summer next the body and tapering towards the and winter, nearly the same as that of the tip; legs short; toes connected by short Weasel, excepting that the upper parts hairy webs; claws nearly straight, sharp, of the Ermine are darker in summer and of the Ermine arte darker in summer and white and concealed by the fur. The fur the under parts a clearer white than the is of two sorts, a very dense down mixed same parts of the Weasel. The Ermine with strong hairs; shortest on the head also grows to a larger size than the Wea- and increasing in length backwards; color sel and is likewise more thick set, its of the down brownish gray; that of the forehead and nose more convex; its ears hairs varying in different parts from chocbroader and more rounded, and its tail a- olate brown to brownish black occasionbout twice as long in proportion to the al white spots about the throat; two oval length of the body. Length of the head glands which secrete a very fetid fluid. and body of the specimen before me 8 in- Length of the head and body 20 inches, ches; tail (vertebra) 3.5. The tuft or pen- tail 9 inches. cil at the extremity extends about.7 inch- HSTORY.-The Mink is a common anies beyond the vertebrae both in this and mal in Vermont' Its favorite haunts are the Weasel. along the banks of streams, where it HISTORY.-It has been a matter of dis- dwells in holes near the water, or in the pute whether this and the preceding ani- ruins of old walls, or in heaps of flood mal do or do not belong to the same wood, or in piers and abutments ofbridges. species. Dr. Harlan describes them as It does not venture far from the. streams two,' Dr. Godman, as one.t With these and when pursued betakes himself immeauthorities before him, Dr. Richardson diately to the water. It does not run well says that both these species are, indubita- on land, but swims and dives admirably, bly, inhabitants of the American conti- and can remain a longf time under water. nent, the Ermine extending to the most When irritated it ects fluid, which remote arctic districts and the Weasel as diffuses a very unpleasant odor. Its fine far north, at least, as the Saskatchewan short fur, Otter-like tail, short legs and river.+ Dr. Williams also describes the webbed feet, all denote its aquatic habits. two as distinct species, and says that the Its fur though not highly prized, is more Ermine, which he calls "ccone of the great- valuable than that of the Musk rat. est beauties of nature" sometimes weighs The food of the Mink consists of frogs, 14 ounces, but that the Weasel is smaller.~ fishes, muscles and fish spawn; and also The skin of the Ermine, in its winter pe- rats, mice, young birds and other small lage of pure white, was formerly held in land animals. T'hey sometimes enter the very high estimation, and was much worn poultry yard, where they make great havby the nobility and high functionaries of oc among the fowls, by cutting off their Europe upon their robes and dresses, and heads and sucking their blood. It is not particularly by judges. Thence it became a very timid animal when in the water, the emblem of judicial purity, and the but dives instantly at the flash of a gun, judge who was any way corrupted was which makes it difficult to shoot them. It is said to have soiled his Ermine. The value easily tamed and in that state is very of the skins at present is hardly sufficient fond of being caressed, but, like the cat, to pay for collecting them. The Ermine is easily offended, and, on a sudden proin its summer dress is, in many places, vocation, will sometimes bite its kindest called the Stoat. benefactor. This animal is found throughout the United States and British Ameri* Fauna Americana p. 61. t Nat. His. I. p. 193. t Fauna Borea i. Ip. 45. O H1is. Vt. [. p. 111. ca, but there has been some confusion 32 NATURAL HISTORY OF VERMONT. PART 1. FISHER MARTIN. PINE MARTIN. with regard to its name. The Mink pro- sometimes called the Pekan, or the Pekan duces from three to six at a litter. When JWeasel, or the Fisher Weasel. fully grown their weight is about four pounds. Mink skins are worth from 20 to 40 cents, according to quality. THE PINE MARTIN. Mustela martes.-LINNAUS. THE FISHER MARTIN. DESCRIPTION.-General color, fulvous brown, varying in different individuals, JMustela canadensis.-LINNsUs. and at different seasons, from bright fulDESCRIPTION.-Head, neck, shoulders vous, to brownish black; bright yellow and top of the back, mixed with gray and under the throat; hair of the tail longer, brown; nose, rump, tail and extremities, coarser and darker than that of the body; brownish black; sometimes a white spot the color on all parts darker and more under the throat, and also between the lustrous, and the fur more valuable in fore and hind legs; lower part of the fore winter than in summer; nose and legs, legs, the fore feet and the whole of the at all seasons, dark, and the tip of the ears hind legs, black; tail full, black, lustrous light. The fur of this animal is of two and tapering to a point; fur on the kinds, one coarse and the other fine and head short, but gradually increasing downy. The usual length of the head in length towards the tail; the head has and body, 18 inches; tail, 9. a strong, roundish, compact appearance; HISTORY.-In Vermont the name of Marthe ears are low semicircular and far tin and Sable are indifferently applied to apart, leaving a broad and slightly round- this animal,but the latter incorrectly,as the ed forehead; fore legs short and strong; true sable is not found in this country. In toes on all the feet connected at the base works on natural history it is usually deby a short web which is covered on both nominated the Pine Martin. This animal sides with hair. Length from the nose to was formerly very plentiful in most parts the insertion of the tail, 23 inches; tail, of the state, but it is at present chiefly including the fur, 16 inches. confined to the mountainous and woody HISTORY.-This animal is known in dif- portions. Though small it is much huntferent places under a great variety of ap- ed for its fine and valuable fur, which, pellations, but in Vermont it is usually with the clearing and settling of the councalled the Fisher, or Fisher Martin. This try, has very much reduced their numname is, however, badly chosen, as it is bers. Many are, however, still taken on calculated to deceive those unacquainted the forest-clad mountains along the cenwith the animal, with regard to its na- tral part of the state. They are usually ture and habits. From its name theinex- caught in traps baited with some kind perienced would conclude that it led,an of fresh meat. Their food consists of aquatic mode of life, and that like the ot- mice, hares, partridges, and other birds. ter, it subsisted principally upon fishes They often rob birds nests of their eggs, or But this is by means true; and they, young, and will ascend trees for thatpurwho have had an opportunity to observe pose, or to escape pursuit. When its reits habits, aver that it manifests as much treat is cut off, it will turn upon its assailrepugnance to water as the domestic cat. ant, arch its back, erect its hair and hiss It may, perhaps, sometimes devour fishes, and snarl like a cat. It will sometimes which are thrown upon the shore, but it seize a dog by the nose and bite so hard, usually subsists by preying upon small that, unless the latter is accustomed to the quadrupeds, birds, eggs, frogs, &c. like combat, it suffers the little animal to esthe martin and other kindred species. It cape. It is sometimes tamed and will is said to kill the porcupine, by biting it manifest considerable attachment to its on the belly, and then devour it. It lives master, but never becomes docile. Marin woods, preferring those which are low tins burrow in the ground. the female and damp. This animal is much valued is smaller than the male. Her time of for its fur, and considerable numbers are gestation is said to be only six weeks, and taken in the state, annually. The price she brings forth from four to seven at a of the skin varies from $1 to $2. It is litter, about the last of April. A full CHPp. 2. QUADRUPEDS OF VERMONT. 33 THE SKUNK. THE AMERICAN OTTER. grown martin weighs about four pounds. no disagreeable odor, and whole nests of The price of prime skins is from $1, to them may lie under a barn floor for $1.25. months, without betraying their presence by their scent. The flesh of the skunk GENUS MEPHITIS.-Cuvier. when the odorous parts have been removed Generic Characters.-Teeth 34-incis- is well flavored and wholesome food. ors, A canine A1-. grinders 4.4 canines l' 5 5 GENUS LUTRA.-Briss. strong and conical; superior tuberculous teeth very large and as broad as they are long; the inferi- Generic Characters.-Teeth 36-Incisor grinders with two tubercles on the inside. ors, a canines 1.1 grinders 5r. canines of 6 51I I, 55' Head short; nose projecting; feet five toed, moderate length and hooked; the first superior hairs on the bottom, and furnished with nails grinder small and blunt, the second and third cutsuitable for digging; trunk of the tail of moderate ting, the fourth with a strong spur on the inner length, or very short; hair of the body long, that side, the fifth with three external points and a of the tail very long; and glands, which secrete broad internal spur; the inferior vary from five to an excessively fetid liquor. six but resemble the superior. Head large and flattened; ears short and round;'body very long, and low upon the legs; tail long, flattened horizontally and tapering; feet webbed; nails crooked and sharp; body covered with a fine fur mixed with long bristlyhairs; two small oval glands secreting a fetid liquor. THE SKUNK. Mephitis americana.-DEs M. DEscRIPTIo N. —General color black, with a white spot between the ears, which often extends along the sides towards the hips in the form of the letter V, and a narrow strip of white in the face; tail bushy, THE AMERICAN OTTER. tipped with white; nails of the fore feet Lutra brasiliensis.-DEsm. strong and about the length of the palm; hair on the head short, longer on the body DESCRIPTION. —COlor dark reddish glosand very long on the tail. Length from sy brown; pale or whitish about thethroat the nose to the insertion of the tail 16 inch- and face; head globular; neck long; body es, head 44 inches, body 11A inches, tail long and cylindrical; tail depressed at (trunk 10, tuft 4) 14 inches. the base; feet webbed, short and strong; HISTORY.-The skunk is a very com- 5 toes on the anterior feet, and 4 with the mon animal in Vermont. It is not con- rudiment of a 5th on the posterior. Tofined to the forests, nor to the thinly set- tal, length of one of the largest size, 4 tled parts of the country, but frequently feet; length of the head 44 inches, tail makes its residence in the midst of' our 17 inches, height 10 inches, circutnfervillages. During the day he shelters him- ence at the middle of the back 19 inches. self in stone walls, or beneath barns, or HISTORY.-The Otter lives in holes in out buildings, and prowls for his'food du- the banks of creeks and rivers, and feeds ring the night. This consists of eggs, principally upon fish, frogs and other young birds, mice and other small quad- small animals. They were formerly very rupeds and reptiles. He frequently does common in this state, particularly along considerable mischief in our poultry yards, the streams which fall into lake Chamby the destruction of eggs and fowls. plain and lake Mernphremagog. Otter What renders this animal most remarka- Creek derives its name from the great ble is its peculiar weapon of defence. abundance of otter, which formerly inWhen pursued, or attacked, it has the habited its banks. They are now become power of ejecting in the face of its enemy scarce, but are occasionally taken at seva fluid of the most nauseating and stifling eral places within the state. scent, which exists in nature. This fluid The Otter is an active, strong and vorais secreted by glands situated near the cious animal. When attacked and unaroot of the tail, and seems to be designed ble to escape they fight with great fiercewholly as a means of defence, being total- ness, and when fully grown are more ly independent of the ordinary evacua- than a match for a common-sized dog. tions. When undisturbed the skunk has The teeth of the Otter are sharp and strong PT. I. S34 NATURAL HISTORY OF VERMONT. PART I. THE COMMON WOLF. THE COMMION WOLF. and his bite very severe. His legs are Length of the specimen in the collections very short and his feet webbed, on which of the College of Natural History of the account he seems to be better fitted for Vermont University, from the nose to the swimming than for running upon land; tail 4 feet 3 inches, tail 17 inches; height and he is so eminently aquatic in his hal- at the shoulder 2 feet.* its that he is seldom seen at much distance HISTORY.-For some years after the setfrom the water. This animal when fully tlement of this state was commenced, grown measured according to Dr. Wil- wolves were so numerous and made such liams, 5 or six feet in length and weighed havoc of the flocks of sheep, that the keepabout 30 pounds, but the total length of ing of sheep was a very precarious busithose taken at present seldom exceeds ness. At some seasons particularly in 4 feet. The price of the skin is at pres- the winter they would prowl through the ent from 5 to 7 dollars, but it has been at settlements by night in large companies, times in such demand as to be worth 10 destroying whole flocks in their way, and, or 12 dollars. after merely drinking their blood and perhaps eating a small portion of the choicest and tenderest parts, would leave the carGENUS CAN1S.-Linnmus-. cases scattered about the enclosure and Generic Characters.-Teeth 42-Incis- go in quest of new victims. Slaughter ersa, canine X, grinders 6_-, The three and destruction seemed their chief defirstgrinders in the upper jaw are small and edged, light; and while marauding the country and are termed false molars, or grinders; the they kept up such horrid and prolonged great carnivorous tooth above bicusped, with a howlings as were calculated, not only to small tubercle on the inner side, and two tubercu- thrilI terror through their timorous vici)us teeth behind each of the carnivorous ones. tims, but to appall the hearts of the inMuzzle elongated, naked and rounded at the ex- habitants of the neighborhood. Though tremity; tongue smooth, ears pointed and erect in the sheep seems to be their favorite victim, the wild species; fore feet with 5 toes and hind wolves sometimes destroy calves, dogs, feet with 4, having robust nails. and other domestic animals; and in the forest they prey upon deer, foxes, hares and such other animals as they can take. Impelled by hunger they have been known in this state to attack persons,* but they usually flee from the presence of man. The wolf bears a strong resemblance to our domestic dog; is equally prolific, and its time of gestation is said to be the same. It produces its young in the early part of summer, having from four to eight at a birth. Between the dog THE COMMON WOLF. and the wolf prolific hybrids have often been produced, which however partake Canis lupus. —LIrNnEUs. more of the nature of the wolf than of the DESCRIPTION. —General color yellow- dog. ish or reddish gray, blackish on the shoul- Wolves have always been so great an ders and rump, and yellowish white be- annoyance that much pains have been taMeath, but varying much according to age ken for their extermination, but at presand climate, being in some cases nearly ent, their number is so much reduced black and in others almost white.* On that comparatively very little damage is the back and sides there is usually an done by them in this state. The legisintermixture of long black, and white hairs lature, however, continues in force a law, with a grayish wool, which partially ap-: giving a bounty of $20 for the destrucpears, giving to those parts a grayish hue, tion of each grown wolf within the state, which deepens along the back into blatk; and $10 for each'sucking whelp of a wolf; hair on the back part of the cheeks, bushy; and the amount paid annually for wolf tail'straight and bushy like that of the fox certificates is usually from one to two hunand nearly the color of the back; eyes dred dollars. The largest wolves killed oblique; ears erect; teeth: very strong. in Vermont have weighed from 90 to 100 pounds. The only part of the wolf which *Difference of colour has been the occasion of the is valuable is its skin, which affords a division of this species into the following varieties: warm and durable fur. Variety 1. Lupus griseuss Common Gray Wolf. 9 2. Lupus albav, White Wolf. c' 3. LsUpus alwcte Pied Wolf. * This specimen is distorted by too much stuffing. 34. Lupssbi tue, Dusk Wolf. It was killed in Addison county about ten years ago. 4. Lupus nubilu, Dusky Wolf' " 5. Lupus ater, Black Wolf. *Williams Hist. I. 101. CGAP. 2. QUADRUPEDS OF VERMONT 35 THE RED FOX. - THE CROSS FOX. ed. The law authorizing the bounty was repealed in 1841. The red Fox is the common fox in Vermont, as well as in all the northern parts of the United States and Canada. Much doubt has existed with regard to the identity of this fox with the common fox of Europe, Canis vulpes,but it is at present regarded by the best naturalists as a distinct species. The particulars in which the THE RED FOX. two species differ are pointed out by Dr. Richardson in his Fauna Boreali Americana, Vol. I. p. 91. This fox is sometimes DEscRIPTION.-General color yellow- taken in traps, but he is so sly and susish red, or straw yellow, less brilliant to- picious that to trap for him successfully wards the tail; chin white; breast dark requires much skill. The best fox hunters gray; belly whitish, tinged with red to- attribute their success to the use of assawards the tail; fronts of the legs and feet famtida or castoreum, with which they black; tail very bushy and less ferrugin- rub their traps, believing the foxes to be ous than the body, the hairs being mostly attracted by such perfumes. The fox is terminated with black, giving it a dark ap- however more commonly taken in Verpearance, with usually a few white hairs mont, by being shot under the pursuit of at the tip; eyes near to each other;- the hound. When the hound is put upon length- of the head and body 28 inches; their track they do not retreat directly to tail including the hair 16 inches; height their holes, nor lead off to any consideraof the shoulder 13 inches. ble distance in one direction, but take a HISTORY.-The Fox has always been circuit around the base of some hill which proverbial for slyness and cunning, and they will often encompass many times beto illustrate these traits of character in fore they proceed to their burrows. The the human species this animal has been hunter, knowing this to be the habit of largely taxed by fabulists, particularly by the fox, can judge of the course he will ZEAsop,who composed his fables 2400 years, take and is enabled to place himself in a aguo. Foxes have their xesidence chiefly situation to shoot the animal as it passes. in holes, which they dig in the earth, or The skins of red foxes, if prime, are alof which they get possession by ejecting ways valuable and the price for several the woodchuck from his. These burrows years past has been from $1 to $1,25 and have two or more entrances and usually sometimes a little higher according to extend under ledges of rocks or roots of quality. The fox is a prolific animal. It trees so that digging out the animal is of- produces its- young usually in April and ten attended with considerable labor. has from three to six at a litter. Though sometimes seen skulking about in the day time, or basking in the sun, THE AMERICAN CROSS FOX. the Fox does not usually venture much abroad excepting in the night. He then Canisfulvus.-Var. decussatus. prowls for his prey through the woods DESCRIPTION.-A blackish stripe passand fields and even among our out-build- ing from the neck down the back and ings. His food consists of hares, rats, another crossing it atright angles over the mice, small birds and poultry. He is said shoulders; sides ferruginous, running into sometimes to feed upon frogs, snails and gray on the back; the chin, legs and insects, and is fond of several kinds of under parts of the body black, with a few berries and fruits. The fable of the fox hairs tipped with white; upper side of the and sour grapes, shows that the partiality tail gray; under side and parts of' the of this animal for the fruit of the vine body adjacent, pale yellow; tail tipped was understood in the days of ]Esop. with white. The cross upon the shoulThe Fox is a great annoyance in mnany ders is not always apparent even in speciparts of the state, sometimes destroying mens, which, from the fineness of the fur, young lambs and oftenmaking great hav- are acknowledged to be Cross Foxes. oc among the poultry. A bounty of 25 Size the same as the common Fox. cents each has been for several years HisTORY.-Instead of considering the paid for killing Foxes within the state; Cross Fox a distinct species, as most Aand the amount paid out of the treasury merican writers have done, I have conon this account has varied from $1000 to eluded to adopt the opinion of Dr. Rich$2000 annually, showing that from 4000 ardson, who regards it merely as a variety to 8000 foxes have been annually destroy- of the common fox. In form and size 36 NATURAL HISTORY OF VERMONT. PART I. THE BLACK, OR SILVER FOX. THE LYNX. the Cross Fox agrees very nearly with in general short and triangular; pupils of the the red fox, and differs from it chiefly eyes in some circular and in others vertically in color, and perhaps a little in the fineness oval; fore feet with 5 toes, hind feet with 4, all of its fur. The skin of the Cross Fox furnished with long sharp retractile claws. bears a much higher price than the red fox, which is owing almost entirely to the color. The price of a prime skin of this fox in Vermont is from $11,50 to $2,50. THE BLACK, OR SILVER FOX. Canisfulvus. —V ar. argentatus. DEscRIPTION.-Color sometimes entirely black and shining, with the exception of the tip of the tail, which is white; but THE LYNX. more commonly hoary on some parts from' Felis candensis.-LniNLus. an intermixture of hairs tipped with white; the nose, legs, sides of the neck, black, or DEscRIPTIoN.-General aspect hoary, nearly so; fur long and thick upon the sometimes mottled; lighter and yellowbody and tail, and short on the paws and ish beneath, the extremity of the hairs beface; soles of the feet covered with woolly ing white, and below, yellowish brown; fur. One of the largest of this variety head rounded; ears erect, terminated measured from the nose to the insertion with black pencils or tufts, 14 inch long, of the tail 31 inches, and the tail, includ- black at the tip, with a black border on ing the hair, 18 inches. the posterior side. Anterior border yelHiSTORY.-The Black or Silver Fox is lowish. Base of the jaws surrounded by regarded by Dr. Richardson as another va- a fringe of long hair, intermixed with riety of the common fox. It is much less gray black and white; brownish around common than the preceding variety and the mouth, white beneath; whiskers black usually grows to a larger size. It has and white; tail terminated with black; sometimes been taken in Vermont, but legs yellowish; toes 4 on each foot, much very seldom. Its fur is exceedingly valu- spread; nails sharp, white and concealed able, prime skins being worth from $10 to in long silky fur or hair. Total length 3 $15 each. feet 4 inches; tail 5 inches. Height of the There is another variety in Vermont, back 1 foot 4 inches; height of the ear 1I whichis not uncommon,called theSampson inches. Fox. The fur is coarse resembling wool HiSToRY.-The Lynx was never very and of little value. The Gray Fox, Canis greatly multiplied in Verniont, but when virginianus, is said to have been taken in the country was new, it was frequently this state, but as I have seen no Vermont met with, and individuals have been taspecimen, it is here omitted. As we have ken occasionally, down to the present before said, it is disputed whether our time. It resembles in fierceness and subtcommon red fox is, or is not identical with lety the other animals of the cat kind, the common fox of Europe. Harlan, preying upon hares, rabbits, mice and othGodman, Richardson, and others, de- er small animals. Nor does it confine scribe it as a distinct species. But Dr. itself to small game, but sometimes desMcMurtrie, the translator of Cuvier's An- troys larger animals, such as deer, sheep, imal Kingdom, says that the Canisfulvus, calves &c. This it is said to do by dropor American red fox, is identical with the ping upon them from branches of frees, European, and was introduced into the clinging upon their necks with their sharp United States many years ago by some claws and opening their jugular veins Englishmen, who thought they afforded and drinkingtheirblood. Sheepandlambs better sport than the American species.* have sometimes been destroyed by them in this state. This animal is found in GENUS FELIS.-Linnavus. large numbers in the vicinity of Hudson's Generic Characters.-Teeth 30-Incis- Bay. Their skins are valuable and the ors 6 canines L grinders 44 Inferior in- Hudson Bay Company procure annually 6 5 1 3 3' from seven to nine thousand of them. The cisors forming a regular series; canines very flesh of the Lynx is used for food and is strong; grinders, above, two conical ones on each said to resemble that of the hare. It is a side, one carnivorous one with three lobes and a timid animal and makes hut little defence small tuberculous one, below, two false compres- when attacked. Its gait is by bounds but sed simple grinders and one carnivorous bicusped. not swift. It swims well and will cross Head round, jaws short, tongue aculeated; ears v....... lakes 2 miles wide. It breeds once a year * Cavler's Animal Kbigdom, Vol. 1, p. 433; and has two'young at a time. CHAP. 2. QUADRUPEDS OF VERMONT. 37 THE BAY LYNX. THE CATAMOUNT. sides and belly, longer, looser, lighter, and tipped with white; hairs of the face like the back, with whitish hairs intermingled, giving it a reddish gray tinge; body long, head round, jaws strong; 1teeth strong; canines conical; claws strong, retractile, and of a pearly white color. Dimensions of the specimen from which the above description is drawnTHE BAY LYNX. length from the nose to the tail, 4 ft. 8 Felis rufa.-GuILIDENSTED. inches; tail, 2 ft. 6 inches; from the top of the head to the point of the nose, 10 DEscRIPTION.-Color yellowish, or red- inches; width across the forehead, 8 indish brown. Inferior parts of the throathes; length of the fore legs, 1 ft. 2 inwhite, or whitish. Eyes encircled with ches the hind legs, 1 ft. 4 inches. a whitish band. Front and portions about HISTORY.-This ferocious American anthe upper lip striped with darkish; irides imal has been known in different places yellow. Ears short, tufted with black under a great variety of different names. hair springing from the back of the ear, In the southern and western parts of the near the tip. Inside of the legs spotted United States it is called the Cougar with brown. Tail short, terminated with Painter, or American Lion; in New Engdark brown, and obscurely banded.- land it is known by the name of CataFringe of hair longer than in other parts mount, or Panther; while in Europe it near the base of the jaw. Ears surround- has more commonly borne the name of ed posteriorly with a black border, within Puma. This is the largest and most forwhich is a triangular patch of yellowish midable animal of the cat kind found in white. Length of the head and body, 2 America. In form it bears considerable ft. 3 inches; tail, 4 inches; height, 16 resemblance to the domestic cat, but inches. when fully grown is about two-thirds the HISTORY.-This animal has been fre- size of a lion. It, however,-differs from qulently met with in our woods, and has the lion in not having the tail tufted, and perhaps been most generally known by the male being without a mane. These the name of Wild Cat. It is, however, to animals, though scattered over all the be distinguished from the smaller wild temperate and warner parts of the conticats with long tails, which are met with, nent, do not appear to have been any and which have probably sprung from the where very numerous. They were fordomestic cat. In its habits it resembles merly much more common in Vermont the preceding species, preying upon squir- than at the present day, and have at times rels, birds,and othersmall animals. This done much injury by destroying sheep animal is now very rare, being only occa- and young cattle. They usually take sionally seen, in the most unsettled parts their prey, like the common cat, by creepof the State. ing softly within proper distance, and then leaping upon it and seizing it by the throat. If the victim be a large animal, like a calf, sheep, or deer, they swing it upon their back, and dash off with great ease and celerity, into some retired place, where it is devoured at leisure. Some years ago one of these animals took a large calf out of a pen in Bennington,. where the fence was four feet high, and'carried it off on his back. With this load, he ascended a ledge of rocks, where one THE CATAMOUNT. of the leaps was 15 feet in height.* DurFelis concolor.-LINN2EUS. ing the day the Catamount usually lies DESCRIPTION.-General color, brown- concealed, but in the night prowls for his ish red on the back, reddish gray on the prey, and in early times his peculiar cry sides, and whitish or light ash on the bel- has often sent a thrill of horror through a ly; tail, the same color as the back, ex- whole neighborhood. When the country cepting the extremity, which is brown- was new, much precaution was considerish black, not tufted; chin, upper lip, ed necessary, when travelling in the and inside of the ears, yellowish white; and inside of the ears, yellowish white; woods in this state, in order to be secure the hairs on the back are short, thick, from the attacks of this ferocious beast. the hairs on the back are short, thicke iiams y, Vol. brownish, and tipped with red; on the * Wiliams' History, Vol. 1, p. 104. NATURAL HISTORY OF VERMONT. PART. I. THE COMMON SEAL. THE BEAVER. Travellers usually went well armed, and Be not surprised, kind reader. It is even at night built a large fire, which served so, and there are living witnesses of the to keep this cautious animal at a distance. fact. While several persons were skaUnder such circumstances a catamount ting upon the ice on lake Champlain, a will sometimes approach within a few little south of Burlington, in February, rods of the fire, and they have been thus 1810, they discovered a living seal in a shot in this state by aiming between the wild state, which had found its way glaring eye-balls, when nothing else was through a crack and was crawling upon visible. The Catamount will seldom attack the ice. They took off their skates, with a person in the day time, unless provoked which they attacked and killed it, and or wounded. In the New York Museum is then drew it to the shore. It is said to the skin of one of these animals, of which have been 4A feet long. It must have the following account is given in Dr. God- reached our lake by way of the St. Lawman's Natural History.* "Two hunters, rence and Richelieu; but it was not asaccompanied by two dogs, went out in certained whether the poor (fat) wanderquest of game, near the Catskill moun- er had lost his way, or having taken a miff tains. At the foot of a large hill, they at society, was seeking voluntary retireagreed to go round it in opposite direc- ment from the world-of seals. tions,and when either discharged his rifle, r' -, the other was to hasten towards him to aid him in securing the game. Soon after parting, the report of a rifle was heard by one of them, who, hastening towards the spot, This is the same as the order Glires of after some search, found nothing but the Linnueus, and embraces those animals, dog, dreadfully lacerated and dead. He whose teeth are fitted for gnawing. They now became much alarmed for the fate of'have two large incisors in each jaw, sephis companion, and, while anxiously look- arated from the grinders by a vacant space, ing round, was horror struck by the harsh No canine teeth. The grinders in some growl of a catamount, which he perceiv- of the genera have flat or ridged crowns, ed on a large limb of a tree, crouching up- and in others blunt tubercles. Under on the body of his friend, and apparently jaw articulated by a longitudinal condyle; meditating an attack on himself. Instant- stomach simple; intestines long; cuecum ly he levelled his rifle at the beast, and large; mammte variable in number. was so fortunate as to wound it mortally, They feed generally on vegetables, but when it fell to the ground along with the the species with tuberculated grinders body of his slaughtered companion. His are nearly omnivorous. dog then rushed upon the wounded catamount, which, with one blow of his paw, GENUS CASTOR.-Linnaeus. laid the poor creature dead by its side. Generic Claracters.-Teeth, 20-incisThe surviving hunter now left the spot, ors no canines, grinders, 4-4 Incisors, and quickly returned with several other 2' 4 4a persons, when they found the lifeless cat- very strong, smooth on the outside, and angular amount extended near the dead bodies of within; grinders have a fold on the internal edge, and three similar folds on the outer edge of the the hunter and the faithful dogs." So hehunter an0 the of thfl ds." mas upper teeth, which are inverted in the lower ones. recently as 1830, one of these animals sprang upon an unfortunate woman, as Eves, small; ears, short and round; feet, five toed; fore feet short; hind feet longer and palshe was passing along a road in Pennsyl- mated; tail, large, flat, and scaly; a pouch near vania, and killed her instantly.t the root of the tail in the male filled with an uncThe weight of a full grown catamount tuous, odoriferous secretion. is usually about 100 pounds. One of the largest taken in this State, to my knowledge, was killed in Roxbury, in December, 1821. It measured 7 feet from the nose to the extremity of the tail, and weighed 118 pounds. Under the name of panther, our legislature give a bounty of $20 each for the destruction of this animal within the state. THE COMMON SEAL. THE BEAVER. Phoca vitulina.-LIsNNUs. Castor fiber.-LIN]NeUs. But what.! exclaims one, the Seal in DEscRIPTION.-Fur r dense, consisting Vermont-that inland mountain state? of two sorts, one coarse, long, and of a * Vol. 1, p. 301. t Griff. Part V, p. 438. chestnut, or reddish brown color, the oth CHAP. 2. QUADRUPEDS OF VERMONT. 39 THE BEAVER. THE BEAVER. er shorter, very fine and of smoky or sil- their houses. The beaver dams differ in very gray; head flattened; nose short shape, according to the nature of the and thick; eyes small; ears short, thick, place in which they are built. If the warounded and covered with short fur; neck ter in the stream have but little motion, short; body thick; back arched; tail flat the dam is almost straight; but when the and broad horizontally, oval and covered current is more rapid, it is always made with oval angular scales; fore legs very with a considerable curve convex towshort and small; and the fore feet are us- ards the stream. The materials made ed as hands for conveying food to the use of, are drift-wood, green willows, mouth; hind feet with long, hard and birch and poplars, if they can be got; alcallous soles, and long toes connected by so mud and stones, intermixed in such a' a web. The usual length of the beaver manner, as must evidently contribute to from the nose to tle origin of the tail, is the strength of the dam; but there is no from 30 to 40 inches, and the tail about 1 1 order or method observed in the dams exinches long and 6 broad at the widest cept that of the work being carried on part. The usual weight of a full grown with a regular sweep, and all the parts Beaver is stated by Dr. Richardson to be being made of equal strength. In places' about twenty-four pounds. which have been long frequented by beavHIsToRv.-The beaver, though former- ers undisturbed, their dams, by frequent ly a very common animal in Vermont, is repairing, become a solid bank, capable of probably now nearly or quite extermina- resisting a great force both of water and ted, none of them having been killed ice; and as the willow, poplar and birch, within the state, to my knowledge, for generally take root and shoot up, they by several years. The last, of which I have degrees form a kind of regular planted any account, was killed, in Essex county, hedge, which I have seen in some places 12 years ago.* The vestiges of its la- so tall that birds have built their nests bors are, however, still found in " the among the branches. beaver meadows" in all parts of the coun- "The beaver-houses are built of the try.- The peculiarities in the form of the same materials as their dams, and are albeaver, and especially the remarkable in- ways proportioned in size to the number stinct, which guides him in the construc- of inhabitants, which seldom exceeds four tion of his dwelling, have always render- old and six or eight young ones; though, ed him an object of admiration, and ma- by chance, I have seen above double that ny accounts of him have been published, number. Instead of order or regulation most of which abounded in exaggeration being observed in rearing their houses, and fable. The following account by they are of much ruder structure than Hearne, who studied the habits of this an- their dams; for, notwithstanding the saimal for 20 years, in the fur countries gacity of these animals, it has never been around Hudson's Bay, is pronounced by observed that they aim at any other conDr. Richardson,* who, himself, had the venience in their houses, than to have a best opportunity for ascertainingits truth, dry place to lie on; and there they usuto be the most correct and free from ex- ally eat their victuals, which they occaaggeration, which has ever been publish- sionally take out of the water. It freed. quently happens that some of the large'" Where beavers are numerous, they houses are found to have one or more construct their habitations upon the partitions, if they deserve the appellation; banks of lakes, ponds, rivers, and small but it is no more than a part of the main streams; but when they are at liberty to building, left by the sagacity of the beavchoose, they always select places where er to support the roof. On such occathere is sufficient current to facilitate the sions, it is common for those different transportation of wood and other necessa- apartments, as some are pleased to call ries to their dwellings, and where the them, to have no communication with water is so deep as not to be frozen to the each other but by water; so that, in fact, bottom during the winter. The beav- they may be called double or treble housers that build their houses in small riv- es, rather than different apartments of ers and creeks, in which water is liable the same house. I have seen a beaverto be drained off, when the back supplies house built in a small island, that had are dried up by the frost, are wonderfully near a dozen different apartments under taught by instinct, to provide against that one roof; and, two or three of these only evil, by making a dam quite across the excepted, none of them had any commustream, at a convenient distance from nication with each other but by water. As there were beavers enough to inhabit * Letter of the Hon. J. Parker, of Orleans, to the each apartment, it is more than probable Author, Sept. 27, 1841. each amn ti o an al Fauna Boreali Americana, Part L. pago 1. that each family knew their own, and al 40 NATURAL HISTORY OF VERMONT. PART I. THE BEAVER. THE BEAVER. ways entered at their own doors, without Judge Parker, who has devoted considany further connection with their neigh- erable attention to the habits of our native bors than a friendly intercourse, and to quadrupeds, after confirming the above join their united labors in erecting their statement of Hearne, in relation to the separate habitations, and building their structure of the dams and houses of the dams where required. Travellers, who beaver, observes: " I have thought the assert that beavers have two doors to correct judgment exercised by the beaver their houses, one on the landside, and the in the selection of the place for his dam, other next the water, seem to be less ac- to be the most remarkable part of his quainted with these animals than others, character. The choice seems to be made who assign them an elegant suite of apart- with reference to the plenty of timber ments. Such a construction would ren- suitable for his food, and the proportion, der their houses of no use, either to pro- which the space to be, overflowed bears tect them from the attacks of their en to the length of the dam; and with regard emies, or guard them against extreme to these, they seem to judge as correctly cold weather. as man. So far as they have fallen under "' So far are beavers from driving stakes my own observation, I have always found into the ground, when building their them at the very best places, which could houses, that they lay most of the wood be selected on the whole stream. One chief crosswise, and nearly horizontal, and object of their pond seems to be, to float without any other order than that of leav- timber, which is to serve them for food, ing a hollow, or cavity in the middle; to their dwellings; and where the water when any unnecessary branches project does not prove deep enough for that purinward, they cut them off with their teeth, pose, they deepen it by digging a trench and throw them in among the rest, to pre- along the bottom, and cutting off the logs vent the mud from falling through the roof. which lie in their way, with their teeth. It is a mistaken notion, that the wood work I have seen logs 20 inches in diameter, is first completed and then plastered; for which had been thus cut off and removthe whole of their houses as well as their ed."' dams, are, from the foundation, one mass Their fo6d during the winter consists of mud and wood, mixed with stones, if principally of the root of the pond lily, they can be procured. The mnudis always JXupthar luteum, which they find in the taken from the edge of the bank, or the water beneath the ice. They also feed bottom of the creek or pond, near the door upon the bark of' the poplar, birch and of the house; and, though their fore paws willow, which they cut down in the fall are small, yet it is held so close up between and drag into the water opposite the doors them under their throat, that they carry of their houses, as a part of their supply both mud and stones, while they always for the winter. In the summer they rove drag the wood with their teeth. All their about, feeding upon different kinds of work is executed in the night; and they herbage and berries, and do not return to are so expeditious, that in the course of repair their houses and lay in their winter one night I have known them to have stock of wood till towards fall. When collected as much mud as amounted to they are to erect a new habitation, they some thousands of' their little handfulls. fell the timber for it in the spring, but do It is the great policy in these animals to not begin to build till August, and never cover the outside of their houses every complete it till cold weather sets in. fall with fresh mud, and as late as possi- The beaver is a cleanly animal, never ble in the autumn, even when the frosts allowing any excrement or filth within become pretty severe, as by this means it its lodge. They are said to pair in Febsoon freezes as hard as a stone, and pre- ruary and bring forth their young in the vents their common enemy, the wolver- latter part of May, producing from four ene, from disturbing them during the to eight at a litter. Beavers seldom cut winter. And as they are frequently seen down trees which exceed 5 or 6 inches in to walk over their work, and sometimes diameter, and they always leave the top to give a flap with their tail, particularly of the stump in the form of a cone. They when plunging into the water, this with- gnaw all round the tree, but direct its out doubt, has given rise to the vulgar fall by cutting one side higher than the opinion that they use their tails as a trow- other. The weight of a full grown beav-'el, with which they plaster their houses; er does not often exceed 30 pounds, whereas that flapping of the tail is no though, according to Dr. Williams, they more than a custom, which they always have taken in Vermont weighing from preserve, even when they become tamne 40 to 60 pounds.t and domestic, and more particularly so *Letter to the Author. when they are startled." t Mis. of Vermtont, Vol. 1. p. il. CHAP. 2. QUADRUPEDS OF VERMONT. k41 THE MUSK-RAT. THE MEADOW MOUSE. GENUS Fll:EIt.-Cuvier. These are made principally of mud mixed Genrric Caractrrls. —Teethl, 15 —ncisors 1with grass,and in the form ofa dome, with no canines, grinders t t Lower incisors a iwarm bed of leaves and grass within. 1shar pointed an 3 conve~x jlent; inders withl The only pllace ofenltrance is fromn beneath, sharp pointed and convex in fi'ont; grinders will) and fron this there are usually several flat crowns, firnished withi scaly, transverse zig-e are lly several zag lamini; four t