A 58186 6 K K GENERAL LIBRARY -OF- UNIVERSITY OF MICHIGAN. PRESENTED BY Board of World's Fair Managias of W Va 1893---- TO READ MERING IN PARet Au 3.. + OAN TI F 241 $45 THE MOUNTAIN STATE. 1 A DESCRIPTION OF THE NATURAL RESOURCES OF WEST VIRGINIA. PREPARED FOR DISTRIBUTION AT THE WORLD'S COLUMBIAN EXPOSITION BY 1 GEO. W. SUMMERS, B. PH, EDITOR OF THE CHARLESTON DAILY GAZETTE. UNDER THE DIRECTION OF THE BOARD OF WORLD'S FAIR MANAGERS FOR WEST VIRGINIA. CHARLESTON, W. VA. MOSES W. DONNALLY, PRINTER. 1893. : . : 15538 BOARD OF WORLD'S FAIR MANAGERS FOR WEST VIRGINIA. HON. W. N. CHANCELLOR, President.. HON. GEORGE M. BOWERS, Treasurer. HON. ROBT. S. CARR. HON. JOHN S. NAYLOR. HON. SIDNEY HAYMOND.. M. C. MCKAY, Secretary · • • • Parkersburg. Martinsburg. Charleston. Wheeling. ..Quiet Dell. Ravenswood. · D : 4 Pen Reclass Į ? INTRODUCTORY. By an Act of the Legislature of West Virginia, approved March sixteenth, 1891, the Board of World's Fair Managers for West. Virginia was created, and the Governor directed to appoint the members of the Board. On the seventh day of May, 1891, the gentlemen named on the preceding page were appointed. At their first meeting, held in Charleston, an organization was effected by the election of Hon. W. N. Chancellor, President; Hon. Geo. M. Bowers, Treasurer, and M. C. McKay, Secretary. In June, 1892, contract was made by the Board with Geo. W. Summers to prepare, as a supplement to the State's exhibit at the Columbian Exposition, a work on the resources of West Virginia, and several months were spent by him in visiting the various. counties of the State in search of the information desired to be con- tained in the work. Circumstances beyond the control of either the Board or Mr. Summers put a stop to the work and it was not till in March, 1893, after the publication of the book had been pro- vided for by an additional appropriation by the Legislature, that a new contract was made and steps taken to complete the work. In the main the work has been prepared from personal visits to every county in the State and from interviews with the leading and best informed citizens of each of the counties, and it may be relied upon as being as nearly accurate as any similar work extant. While some of the statements made concerning the resources of the State may seem extravagant, investigation will show that they are in the main correct. Every effort has been made not to over-esti- mate the value or extent of any resource, but to present for the in MY 4 INTRODUCTORY. formation and guidance of those who wish to know more of the magnificent commonwealth of the Alleghanies than they do, the facts as they are found, without any attempt at exaggeration. Be- lieving that more injury could be done to the State by making erroneous claims which could not be substantiated, than by leav- ing unsaid a part of the truth, the aim has been to err in the latter way rather than in the former. Mistakes will undoubtedly be found, but the intent of the board and of the writer to present to those who seek it such information as will give them valuable knowledge of the State has never been lost sight of and the work is presented to the public with the hope and in the belief that it may draw to West Virginia more of the capital required to make her vast resources available, the labor that must go hand in hand with capital, the settlers who are to people our hills and valleys, the pros- perity that must come, soon or late, to a State so endowed by kind- ly Nature as is West Virginia. To those who have rendered their assistance in the preparation of the work, the writer desires hereby to tender his acknowledge- ments, knowing that without their generous aid he could not have prepared it. G 2 - Į 9 WEST VIRGINIA. 5 い ​J [1 WEST VIRGINIA. Born West Virginia had an unfortunate start in life as a State. in the midst of that fearful civil strife which plunged the entire na- tion into a debt from which it has never yet recovered, which plucked in their prime so many thousands of the fairest flowers of all the land and saw them wither and decay, which plunged deep into debt and desolation the whole fair southern land, wrecking at once great fortunes and happy homes, bringing death and destruc- tion and poverty over all the southern States and sadness over all, the early days of West Virginia were not conducive to the rapid ad- vancement of the State. In the old State, that part west of the mountains had always been looked down on as more of a wilderness than anything else, and little attention was ever given to it. The people complained for years that they were permitted by the State to do nothing but pay their taxes. Their representation in the coun- cils of the State was small, and by the "Old Dominion" that portion of her domain west of the mountains was practically ignored. Ham- pered and held down by the proud and powerful "Mother of Pres- idents," at the beginning of the civil war the part of Old Virginia which was afterwards set apart to form the new State gave but little promise of the glorious destiny that was in store for her. Her wealth was little known. The immense value of her timber forests, the al- most inexhaustible deposits of her coal, the flowing wells of oil and gas, the richness of her iron ores, the great fertility of her hills and valleys were never dreamed of, and, aside from the desire to have the new State pay the old State debt, Virginia did not care for the loss, by separation, of her better half. 6 WEST VIRGINIA. At first the new State's prospects were not bright. Along the border of the north and south, the sympathizers of both sides were numerous in the new State's bounds, and both sides felt most keenly the depressing results of the terrible civil war. The unhappy polit- ical situation, the poverty of the country, particularly of the people. of this State, many of whom had lost their every dollar, the un- settled condition of the times in general, prevented at the first the development of any of the vast resources of the State. After the lapse of a few years, when the situation had been somewhat relieved, when the constitution had been altered and the liberties of the people much increased, when capital was coming in and the State was building up, then came the panic which brought again disaster through the Union and set the State of West Virginia back ten years. * The Centennial Exposition in 1876 brought prominently before the world the wonderful resources of the State and West Virginia took a fresh start. With its fine exhibit of the coals and irons and timber here to be found the State attracted capital from all parts of the world. The development of the State dates practically from that time. Soon after the State had shown to the world the vast- ness of her resources and had drawn the attention of the entire civilized world to her possessions, new mines were opened, new saw mills built, new people came in and settled among us, and rail- road building took a start that brought the State up gradually to the front, till last year no other State in all the Union exceeded West Virginia in the amount of its railroad mileage completed with in the year. From practical oblivion, known only as the muddy, mountain- ous part cut off from old Virginia, our State has grown and still is growing until it now stands near the top among the list of States, and takes high rank among them all in the production of all those things to which her hills and vales are fitted. We have come out of the woods and in the place of the forests are springing up new towns. The State is not yet fully explored, the real extent of all her vast resources is hardly known, each new year adding some new discovery of value to the State; but step by step the forest fastnesses are being penetrated, the homes of man replace the haunts of beasts of prey and every part of the State is being brought in # ང་ J مه WEST VIRGINIA. 7 ! 0 LI U . 43 touch with the busy life of the outside world. In 1863 a single line of railroad passed through a few of the northern counties of the State. To-day there are but 11 out of the 54 that have no railroad, and from the present prospects, within the next few years the iron arteries of trade will pierce the confines of them all and not a county in the State will be without its railroad and the industries. that always accompany and follow the building of a road. In 1863 a few small coal mines produced a little coal principally for domes- tic consumption, and some was used for the manufacture of "cannel. coal oil," but the coal trade so far as the shipment of coal to other markets than our own was concerned was almost unknown. In 1870 the coal production was but 608,878 tons. Last year two hundred mines were in operation, employing over 15,000 men and producing nearly nine million tons of coal in addition to the small mines for local consumption which still exist in the State as they did at that day. The timber then was only cut to get it out of the way of the farmer who wished to improve his land, and was burned or deadened and allowed to decay To-day the timbering and lumbering industries of the State employ some fifteen thousand men, saw mills are in operation in every county of the State and the lumber produced from the West Virginia forests is shipped to every country in the world. The oil production of the State is next to that of Pennsylvania now, while thirty years ago the only oil produced was that which was extracted from the cannel coal. To-day the Sistersville oil field is the largest oil field in the world or rather the oil field producing the largest amount of oil. In 1863 no coke was made in West Virginia. Last year there were 1,314,- 449 tons of coke made in the State. In every way the State is rap- idly forging forward toward the front. The population is rapidly increasing, the increase for the last decade being about 19 per cent. The capital invested is many times that of a few years ago. Devel- opment is bringing to the markets of the world the hidden riches Providence has bestowed upon the Mountain State. Manufactur- ing is growing in extent and variety and we stand upon the thresh- hold of a new era of prosperity, which will cause the State to grow in people and in wealth, in the variety of its products and in all that goes to make a State great and prosperous. { The abundance of opportunity and the absence of capital for the # 8 WEST VIRGINIA. proper development of the State invite the attention of all who are in a position to aid in bringing West Virginia to the front and at the same time to reap a share of the prosperity that is surely com- ing to the State. The possibilities for West Virginia are not ex- ceeded by those of any other State in the Union, and to the atten- tion of those who will aid in its development these possibilities are in this volume called. WHA. t # 湿 ​COAL. 9 .. COAL. . It is a difficult matter to convey to the mind of one not familiar with the facts any adequate idea of the immensity and value of the West Virginia coal fields. To say that sixteen thousand out of the twenty-four thousand square miles of the territory in the State is underlaid with coal, gives but a vague idea of what there really is. To say that over ten million acres of West Virginia is coal land, on which there is an average thickness of ten feet of coal, means but little more. When we say that there is a sufficient quantity of coal hidden away in the hills and beneath the surface of the State to supply the wants of the entire world for centuries to come, then does the mind begin to realize the real extent of the coal deposits of the State. Going further and estimating the amount of the coal in the State at the usual average rate of production, the ten million acres would yield one hundred billion tons. The coal production in this State for 1892, the greatest for any year in the history of the State, was something over eight million tons. Increasing this to an average rate of ten million tons a year, the coal of West Virginia, constantly mined, would last ten thousand years. The entire amount of bituminous coal consumed in the United States during the year 1889, according to the last census, was a little over ninety-five million. tons. Increasing this to one hundred million tons a year, the coal in West Virginia alone would supply the entire United States with all its coal for the next one thousand years. If all the coal in West Virginia were, by some miraculous means, mined at once and loaded into railroad cars of twenty tons capacity, the whole would make a continuous train that would reach one thousand five hundred times 10 COAL. 2 2 .. ; around the earth. According to the last United States census, the average value of the coal of the United States, on cars at the mine, was 99 cents a ton. At this rate the value of the coal of West Vir- ginia, still unmined, would be ninety-nine thousand million dollars, enough to make ninety-nine thousand millionaires in the State of West Virginia. When the facts are looked at in this light, and the value of the hidden deposits of coal within the State are made apparent in such a way that they can be appreciated, there seems little room to doubt the statement made by Professor I. C. White, one of the best authorities in the country on geological matters, that the coal alone of West Virginia is worth more than all the gold and silver of the Pacific coast. Of the fifty-four counties in the State, there are but three-Jefferson, Hardy and Monroe-in which no coal has yet been found. Every other county in the State contains coal of some kind in varying quantities, most of them having an abundance. All kinds are found-anthracite, splint, bituminous, cannel and all the intermediate varieties--in some places all of them except the anthracite being found in the same counties and fre- quently on the same property. The veins range in thickness from a few inches to nearly thirty feet, and frequently the veins are found on the same property one above the other until the entire thickness of the combined veins aggregates very many feet. In one mountain in the State there are no less than eleven veins, one above the other, from 2 feet 7 inches to 20 feet in thickness, aggregating 68 feet 11 inches of coal. Aggregate thicknesses of from 25 to 50 feet of coal over the same property are not infrequent. The following brief description of WEST VIRGINIA COAL FIELDS is taken from an article written recently by Prof. White for the Kanawha Gazette: To the largest and most valuable coal field in the world, geolo- gists have given the name Appalachian. It covers an area of nearly 60,000 square miles, and beginning near the northern line of Pennsylvania extends southward across that State, and taking in nearly the whole of West Virginia, and a broad strip from the southern part of Ohio, passes on through eastern Kentucky and Tennessee to end in Alabama, nearly 900 miles from its northern + 1 COAL. 11 1 I 77 ۱۳ JA P terminus. The shape of this great field is roughly that of a canoe, and West Virginia lies within the zone of its broadest and richest portion. In only four of the fifty-four counties in West Virginia is it im- possible to find bituminous coal, viz: Jefferson, Berkeley, Morgan, and Monroe. The column of rocks which holds the coal beds in the Appa- lachian field has been subdivided into several groups, and as these come to the surface in different portions of the State, and contain coals of distinctly different qualities, I shall briefly describe each, and trace the lines of their outcrops across the State. At the base of the series, and therefore the lowest group of the true coal measure rocks, we have what is usually termed the con- glomerate measures; because the great sandstones which are there interstratified with the beds of coal and slate often contain pebbles of quartz and other hard rocks in great abundance. The group has also received several other names, among which may be men- tioned No. 12 conglomerate, Pottsville conglomerate, seral conglom- erate and the millstone grit of the English geologists. The group of coal beds which these rocks contain have been termed the New River coal series, from that region of our own State where the beds, as a whole, have their grandest development. - The sandstones of this series are noted for their hardness and con- sequent power to resist the action of the elements. Being com- posed almost entirely of quartz pebbles and sand grains, they form great sheets of protecting rock which is almost indestructible by atmospheric influence, and thus it happens that this group of beds is the principal factor in forming the picturesque scenery of our Mountain State. The wild gorges and canyons of the Cheat, the Gauley, the New, the Guyandotte, the Big Sandy and other West Virginia rivers are all formed by this series of rocks. All of the ridges and peaks of the Alleghanies are capped and protected by this friendly mantle. Wherever these rocks come to the surface, wildness, barren soils, and precipitous slopes prevail, but when they dip below the drainage levels the mountains disappear, and in their stead we find rounded hills, with gentler slopes and broader valleys. Another peculiarity of this series is that although it forms a con- tinous sheet of beds under all of the 60,000 square miles of the Ap- ; 12 COAL. : Eve palachian coal field, yet it contains coal in workable thickness and purity only around the borders of the field in a comparatively narrow rim. Thus while there are valuable coal beds in Jackson county, Ohio, along the northwestern border of the group, and also opposite this along the southeastern border, in Fayette county, West Virginia, no workable coal would be found, if a shaft shoul 1 be sunk to the series, say at the mouth of the Great Kanawha, or at any other point 20 to 30 miles distant from the respective borders of the field. The same hard sandstones and pebble-beds would be encoun- tered, but they would hold only thin streaks of coal and bituminous slates. Another feature of these conglomerate coal measures is the great purity of the coal beds when they attain workable dimensions. These early formed coals are singularly free from injurious quanti- ties of sulphur and ash, the bane of some coals. Their purity in this respect is probably due to the fact that just previous to the spread of the great peat swamps of this early epoch, the floor of the entire Appalachian coal field was sheeted with a deposit of clean sand and gravel, thus effectually covering up the muddy sediments of a previous epoch, and causing the streams which drained into the peat or coal marshes of the time to be clear and free from im- purities, like our own mountain brooks of the present; but however this may be, the fact remains that these conglomerate coals are of exceptional purity. Another strange thing about these coals is that along the north- western border of the Appalachian field, the quality of the coal is entirely different from that found on the opposite, or southeastern rim of the field. Along the former, through Pennsylvania and Ohio, these coals are nearly always non-coking and can frequently be used in furnaces just as they are brought from the mines, and are hence often called "block" coals; but on the southeastern side, through West Virginia, Virginia, Kentucky, &c., the coals of this series are universally of the coking kind, and being so pure they are fast becoming justly celebrated for the production of coke of the highest grade. The conglomerate rocks crop out on the surface in West Virginia through the following counties, beginning at the north: Preston, Mineral, Grant, Tucker, Randolph, Webster, Pocahontas, Greenbrier, COAL. 13 } 13 ti Nicholas, Fayette, Raleigh, Summers, Mercer, Wyoming, McDowell and Logan. Until we get southward as far as Nicholas and Webster, there ap- pears to be but one workable bed of coal in these conglomerate measures, and it lies near the bottom of the series, I have observed it at several localities, however, in Preston, Tucker and Randolph, in each of which the bed is about three feet thick, and very fair coking coal But on southward through Webster and Nicholas, into Fayette, the whole group of rocks increases in thickness very fast, and when we come to the New River, in Fayette county, these rocks have a thickness of 1,400 feet, and contain three workable coal beds, with thicknesses of three to five feet. It is from these beds that the famous New River coke is manufactured, which now sells in the market at a higher figure than the Connellsville product. But although Webster, Nicholas, Greenbrier, Fayette and Sum- mers all have splendid fields of these purest of coals, yet it is not, however, till we come to Raleigh, Mercer, Wyoming and McDowell counties, at the extreme southwestern corner of the State, that we find the thickest and most productive coal beds in this series of rocks; for here the great Pocahontas bed attains a thickness of six to ten feet over an area of several hundred square miles, while at many localities two other beds may be found above the Pocahontas vein, with a thickness of four to six feet. The proximity of this great field of pure coking coals to the im- mense iron ore deposits of the South, renders it valuable beyond computation. and yet its development has only just begun. It is only about six years since the first car load of coal was shipped from the Pocahontas region, near the line of Mercer county, and yet during the past year, one million tons of coal and coke have gone to market from this region alone. Lying on top of the conglomerate, or New River coal measures, we find another group of rocks with valuable coal beds included, and to this series has been given the name of Lower coal measures. To this group belong the coal beds which have recently attracted so much attention and capital to Clearfield, Jefferson and Cambria counties, Pennsylvania. Within the limits of these measures there are usually five coal beds which at one time or another furnish valuable fuel, viz: in descending order: Upper Freeport, Lower ¿ 14 COAL. Freeport, Upper Kittanning, Middle Kittanning, Lower Kittanning and Clarion Coal beds. This coal series enters West Virginia from Pennsylvania in Monongalia and Preston counties, with a thickness of 250 to 300 feet, and contains two valuable coal beds, the Upper Freeport and the Lower Kittanning, the former being locally known as the "Austin coking" coal, and the latter as the "Newburg shaft" seam, on the Baltimore & Ohio Railroad. These two beds are separated by an in- terval of shales and sandstones 100 to 180 feet thick, and they are both easily accessible over a very large area in Monongalia and Preston. They have an average thickness of five to six feet each, and both make splendid coke. The same two beds reappear on the North Potomac, where they underlie an immense area along the West Virginia Central Railroad, in Mineral, Tucker and Grant counties. They are both mined near Davis, the upper one being called the "Thomas seam," and the lower one the "Davis seam. Both have been successfully tested for coke in the Davis region. On southward from the counties already mentioned, the outcrop of this series may be traced through Taylor, Barbour, Randolph (where the U Freeport is the celebrated "22-foot seam"), Upshur, Braxton, Webster, Nicholas, Clay, Kanawha, Fayette, Raleigh, Wy- oming, Boone, Logan, Lincoln, Wayne and Cabell. These are the counties along the eastern side of the Appalachian field, where the coals of this series come up to the surface, while on the opposite side of the fields the only locality where they come up to daylight is in Hancock county, and for a short distance along the Volcano up- lift in Wood and Wirt. The series, hovever, underlies all the other counties of the State, which lie west from the belt first mentioned, and unlike the conglomerate series below, seems to have valuable coal beds in it at every locality. This we learn from the records of drill holes which have been made in nearly every part of the State. One of these beds is now mined at Wellsburg by a shaft 200 feet deep, and the drill shows that the same valuable bed underlies Wheeling at a depth of only 500 feet, while at Parkersburg a good bed of coal seven feet thick and belonging to this same series was passed at a depth of 1,100 feet, and the same bed has been drilled through at Mannington, 1,300 feet below the valleys. These depths. may be regarded by some as rendering the coal beds in question en- 4 19 : COAL. 15 .. " tirely valueless, but such should remember that the development of this country has only just begun, and that England raises nearly all her immense output of coal from depths of 1,000 to 3,000 feet. These facts are mentioned simply to show the vastness of our resour- ces in coal, and the permanency of supply of this "main-spring of civilization," and hence that the railroads, cities and manufactories which may be built within our borders, can depend on an abund- ant supply of fuel for many centuries, even from the beds of coal which can be operated from the surface; but when these shall have been exhausted, we shall still have an infinite wealth of these "black diamonds," which can be easily obtained by going down a few hun- dred feet below the surface. When that time comes West Virginia will possess a monopoly of coal in the Appalachian field, for it will be practically exhausted from all the States around us before that from our easily accessible beds is used up. In passing from the northern part of the State south-westward to the region of the Great Kanawha, the lower coal measures expand won- derfully in thickness, and instead of a rock series of 250 or 300 feet as in Preston and Monongalia, we get 1,000 feet of rock between the uppermost coal bed of the group and the top of the conglomerate series below. Accompanying this expansion of the measures there is a great change in the character of the coal in the different beds. Instead of soft coking coal, we find cannel (in Wayne, Lincoln and Boone, the Upper Freeport coal forms one of the largest areas of pure cannel known in any country of the world) and "block" and "splint," which being quite hard, and crumbling with difficulty, make splen- did shipping coals, and the perfection of domestic fuel. The lowest. bed, however, the Clarion or Eagle seam, makes a splendid coke, and the Lower Kittanning or Campbell's Creek seam, can also be coked successfully in some regions. Hence the territory along the Elk and its tributaries, the Great Kanawha and its tributaries, as well as the Guyandotte, Twelve Pole and the Big Sandy, abounds in splen- did coal beds of this Lower coal measure series. To the next higher group of rocks geologists have given the name of Barren measures, because the coal beds they contain are usually thin, irregular in thickness and poor in quality. Along with much group of beds con- sand stone, thin limestone and other rocks, this tains a great deal of soft red shale, and hence it makes a broad belt 3 16 t COAL. of red soil almost exactly in the central line of the State, from Mon- ongalia clear through to Wayne. The thickness of the series varies. usually between 500 and 600 feet, except toward the southwestern. portion of the State, where it expands in thickness like all the other groups, and measures 800 feet near Charleston. Although usually meriting the name "Barren Measures," yet oc- casionally some good coal is found in this group over restricted areas. The Masontown coal or "four foot" bed of Preston county, is one of those exceptions, and the Brush Creek bed which caps the hills at Coalburg on the Kanawha, and furnishes some fine "block" coal in several counties of the southwestern part of the State, is another. These two beds belong in the lower half of the group, and the last named is the lower one. The "Barren Measures" are lim- ited above by a great bed of coal, the most important one in the Appalachian field, the famous Pittsburg bed. This bed marks the beginning of another, and the last of the groups of the true coal measure rocks, which is termed the "Upper Coal Measures." This series, unlike those below it, attains its maximum thickness and importance at the northern end of the State, instead of the southern. In Monongalia county it has a thickness of 380 feet, and contains. four valuable coal beds, disposed as follows: At base, the great Pitts- burg bed, with a workable thickness of seven to nine feet; forty feet. above this comes the Redstone bed, with a thickness of four to five feet; sixty feet above the latter lies the Sewickly bed, having a thickness of five to six feet, while 260 feet above the last, and capping the series, we get the Waynesburg bed, with a workable thickness of six to seven feet. Thus it happens that in many of the hills of Monongalia twenty to twenty-five feet of merchantable coal may be mined without shafting. In coming southward from Monongalia the Pittsburg, Sewickly and Waynesburg coals hold their usual thickness through Marion county, but the Redstone beds thin out before reaching there, and on beyond Marion the Sewickly and Waynesburg beds dwindle down to thin and unimportant layers, leaving the Pittsburg as the only valuable coal in the group, but the latter maintains such a standard of thickness and value as to amply compensate for the loss of the higher members possessed in more favored Monongalia and Marion. As we pass westward from the Monongahela river, in Ca ¦ COAL. 17 the last mentioned counties, these Upper coal measure beds dip be- neath the surface down into the great trough of the Appalachian basin and do not come up to daylight again till we reach the Ohio river valley near Wheeling, and here we find that only the Pitts- burg remains important, the others being represented by thin and slaty beds, hence it will be observed that so far as our State is con- cerned the Upper coal measures derive their chief importance from the presence of one bed, the Pittsburg, but it is so valuable as to merit a more detailed description than could be given to the other individual seams within the limited space of this article. This Pittsburgh bed, as we have already stated, is the most im- portant seam in the entire Appalachian field. It is the same bed which furnishes the coal for the manufacture of the famous Con- nellsville coke, and hence is often called the Connellsville and Youghiogheny bed. Coming as it does so high up in the series of rocks, it has suffered more from erosion than any other of the coal beds below it, having been worn away from many thousands of square miles, where it once existed. This we realize when crossing the Alleghanies to Piedmont, and find the same Pittsburgh bed represented in the "Big Bed" of that region and the George's creek basin, where it is fifteen to twenty feet thick. We also discover the same coal bed on the heights at Elk Garden, on the West Virginia Central Railroad, and in the isolated patch at Fairfax Summit, more than 3,300 feet above the sea. The remnant of this bed in Copeman's Knob, near Kingwood, the scattered patches on the hill top around Newburg, and the few acres of it on the highest sum- mits near Belington, taken in connection with the Fairfax and Elk Garden areas will give the reader some idea of the vast inter- mediate surface from which it has already been mined by the cease- less action of the elements. But fortunately for our State, the deepest portion of the Appalachian trough passes across its territory from the Pennsylvania line clear through to the Kentucky border in Wayne county, and has thus preserved for us in its ample fold, a very large area of this valuable bed. Its outcrop has been fol- lowed from the State line southward past Morgantown, Fairmont, Clarksburg, Weston, Troy, Glenville, Sutton, Sissonville, and on the Great Kanawha at Raymond City. Beyond this river the coal is thin, and found in interrupted patches, but it has recently been } "A ! 18 COAL. opened in the tops of the hills back from Huntington, and the last patch of it within the State is in the summit of a high knob over- looking the Big Sandy, and ten miles above its mouth. Kentucky receives all of the coal beds under this one from our State, but she gets not an ounce of the great Pittsburgh seam, for it passes into the air over the tops of her highest hills, from a point in our State with- in a stone's throw of her territory. On the Ohio river side of West Virginia, this bed comes into the tops of our hills opposite Steubenville, and dipping down from the north is only 100 feet above water level at the mouth of Wheeling creek. It has thus been the bed rock of Wheeling's industries and prosperity, and it is the foundation stone on which her sister city, Pittsburgh, has built such a grand superstructure of manufacturing interests. And notwithstanding the temporary advantages of natu- ral gas, this coal bed will be the main source of the future greatness of the two cities. Followed below Wheeling, this coal gradually approaches the river level and passes beneath the same a short distance below Benwood, and although it is reached by the shafts at Moundsville, the horizon of the coal keeps constantly below water level till we reach the Vol- cano oil uplift, a short distance below St. Marys. Here the place where it should be is lifted 250 to 300 feet above the river for two or three miles, but the coal is wanting or so thin that it is practically absent, and the same thing is true all along this arch from Eureka through by Volcano to Burning Springs and beyond toward Spencer. How broad this barren belt may be we cannot yet certainly deter- mine, owing to want of observations in the central part of the State, but there are some reasons for believing that this barren region is coincident with the course of the Volcano arch, and that it thus extends from Eureka through to Burning Springs on the Great Kanawha, 10 miles above Charleston; and that along this line for a distance of several (10 to 15) miles on each side, no valuable deposits of this coal can be found. We know, however, that the coal comes in again west of this arch, for when the Ohio turns north below Letart Falls the rise of the rocks soon brings the coal to the surtace at Hartford City and other points in that region, where it is still a valuable bed, though much reduced in thickness from its normal size at the northern end of the State. COAL. 19 N The counties then which have this great coal bed may be enumer- ated as follows: About one-half of Brooke, nearly all of Ohio, all of Marshall, Wetzel, Tyler, Doddridge, the eastern halves of Ritchie and Gilmer, the northern half of Braxton, the large areas in western Upshur, Barbour and Taylor, much of Lewis, nearly all of Harrison, three-fourths of Marion, and two-thirds of Monongalia. On the west side of the barren strip, this coal will be found in the portions. of Putnam and Mason north from the Great Kanawha, probably all of Jackson, and the most of that portion of Kanawha north from the Elk and Kanawha rivers. Of course under much of this large area, the bed can only be reached by shafting, but a depth of 300 to 400 feet will reach it along most of the valleys, even where it is deepest, except near the summits of the divides, where it is deeper of course, but still within. the limits of easy access whenever the time shall come that it is needed for fuel supply. One of the finest areas of this coal, and the most easily accessible, lies along the Monongahela river, between the Pennsylvania line and the tier of counties through which this river flows, viz: Lewis, Harrison, Marion and Monongalia. The distance from the State line to Weston, by the meanders of the river, is more than one hun- dred miles, and throughout this long distance the great Pittsburgh bed is almost constantly above water level, and cropping out from either bank of the stream at a moderate elevation above the same, so as to be most fortunately situated for cheap and successful mining. The universal excellence of this coal for all purposes of fuel, gas, coke and every other use to which coal can be put, renders the field in question one of the most valuable in the country, or in the world for that matter, and the railroad that first opens it up to market will have a monopoly of good things in the coal traffic for a long time. It was formerly supposed that this coal would not make mer- chantable coke, but the successful working of nearly 200 ovens at Montana, on the Fairmont, Morgantown and Pittsburgh railroad, together with the successful plants at Fairmont, Clarksburg, Tyr- connell, Monongah, etc., have set this question happily at rest, and proven that the coal in question will make a coke but little inferior, 20 COAL. ¿ if any at all, to that from the celebrated Connellsville region, of which the Monongahela country is simply a southward extension. THE BASIS OF OUR PROSPERITY. - It will be seen from the hasty and imperfect review of the coal fields of our State that the quantity of this valuable fuel which underlies the surface of our hills and valleys and mountains, is al- most beyond conception, and it does not aid the mind much to be told that if we put the workable thickness of coal underlying the 10,000,000 acres of our coal field, at only ten feet, the available. product will be at least 100,000,000,000 tons. But impossible as it may be to comprehend the real meaning of such an array of figures, we can at least be assured that the basis of our future prosperity is grounded so firmly in this wealth which lies hidden in our hills, that nothing conceivable to human reason can thwart our growth or prevent our continued progress in everything pertaining to in- dustrial welfare. J The West Virginia coal field is one and a half times larger than that of Great Britain, the production of whose mines is now nearly two hundred million tons annually. In the not distant future when the network of railways which the benefactors of our State are now planning for its development, shall have connected our mines with links of steel to the great arteries of trade and com- merce, and our production of coal shall have risen to even half what Great Britain's is, then will our people begin to realize more clearly the enormous value of the fuel wealth to which we are heirs. Sp The outline of the distribution of the coals of West Virginia, by Professor White, given above, together with the brief descriptions. of the coal of each county given in the subsequent pages of this volume, will suffice to give a general idea of the coal fields of the State. The space at our command is not sufficient to permit a more full description. With this almost limitless amount of coal locked up in the bowels of the earth, comparatively little has ever been done toward its development. With sixteen thousand square miles of coal but 200 collieries are now in operation. The total capital invested in the production of coal in this State, according to the last census, is $ سم COAL. 21 7 .. e $10,508,050. The total number of persons employed in and about the mines of the State in the last year was 15,393. It is only within the last few years that the coals of West Virginia have attracted any attention from the men in other States who had the capital to develope them, but the growth of the mining industry since that time has been rapid. Twelve years ago less than a sixth as much coal was produced annually as is now mined. In 1880 the State ranked seventh in the Union in the production of coal; last year but three other States produced as much as West Virginia. The growth of the business is shown by the following table: 1880... 1881 1882.. 1893.. 1881.. 1885. 1886 1887. 1888. 1889.. 1890 . 1891.. 1892. .. YEARS. ··· Inside Miners. 2.553 3,063 3,573 4,438 4,627 5,4861 6.081 7,023 7,269 7,764 9,173 10,434 9,884 Outside Laborers and Coke W'rk'rs 1,173 1,407 1,641 1,956 1.724 1.806 1.181 1,582 1,705 1.882 2,324 2,589 5,509 Total Production Ton 2,000 lbs. 1,404,008 1,803,984 2.416,960 3,142.234 3.249,839 3.369,062 3,598,664 4.936,820 5,375,564 5,405,173 6.002,080 8,155,202 8,710,888 Percentage of Increase. 28.48 33.90 30.00 3.40 3.60 6.80 37 18 8.89 0.55 11.04 35.87 6.81 Average Annual Increase. Average annual percent- age of increase from 1881 to 1892, 17.21. This increase, rapid as it has been, would have been much larger, but for the want of adequate facilities for the transportation of the coal. Every railroad in the State that passes through coal regions has all it can do to handle the product of the mines along its line and the development of new fields is much retarded from this cause. The construction of new roads, the double tracking of old ones, and the purchase of hundreds of new cars and other equipments are assisting materially in developing the coal, but still there is room for more. The railroads can little more than handle the present output of the mines and as fast as new ones are built they are crowded to their fullest capacity. Those sections which are favored with river transportation suffer less from this cause than the others, but every new facility for reaching the market materially increases the output of the mines. The activity in railroad building in this State indicates that this can not longer remain the cause for the want of proper growth of the mining industry. Last year the State 22 COAL. ¿ stood first of all in the amount of railroad built within the year, and from all the indications, bids fair to do the same again this year. New lines are projected in every direction and through all the coun- ties of the State, and ample facilities will soon be afforded for all the shipments of coal that may be desired. Several causes combine to give the coals of West Virginia their enormous value—the great area and thickness of the beds, making the largest deposit of coal in any State in the Union; the purity of the coal, which is singularly free from sulphur and other impuri- ties; the variety of the kinds found, anthracite, splint, cannel and bituminous all being found, and all but the first in enormous quanti- ties and frequently upon the same property; the value of the coal, much of which commands a higher price in the market than other similar coals; the ease with which it can be worked, in half the State, perhaps, the coal all being above the water level, and in all the rest being much nearer the surface than is the coal of other places which is constantly worked, as in England where shafts are put down as deep as 2,600 feet below the surface of the earth, the shaft costing half a million dollars; the nearness to market, being much nearer to the southern and western markets than is the coal of Pennsylvania, its only competitor, and having several through lines to the north-west and the east; its nearness to the great Vir- ginia iron ore fields, where much iron is now made and more will be; the cheapness of the lands upon which the coals are found and the cheapness with which it can be mined, the average cost of min- ing coal in West Virginia being lower than in any other State in the Union save one. ANTHRACITE COAL. The amount of anthracite coal in the State is comparatively small, though there is enough of it to be of considerable value. It is found in but two counties -- Berkeley and Morgan-lying in the hills that separate the two. As long ago as 1835 the owners of some property in these counties had some investigations made to see what amount of coal there was there and the value of it. A six-foot vein of an- thracite coal was then found, but water filled the mine and it was abandoned. At various times since then efforts have been made to ascertain the extent and value of the coal deposit, but until f COAL. 23 At the bot- This is cut recently nothing was done in a determined way, and little more was known than that there was anthracite coal in the hills, and that it was pretty hard to get at. In 1883 further efforts were made by other parties to get at the coal and a ten-foot vein was struck. This shaft also filled with water and remains so to the present time. In 1889 an experienced mining engineer was sent from Pottsville, Pa., to look into this property and report upon it. His report says the coal is "of fair quality and compares favorably with Pennsylvania anthracite coal." Later a New York geologist was sent to look into the field. He made an opening and at five feet from the surface, struck the top of the largest seam of coal yet found. The shaft was sunk to the distance of forty-two feet. His report >ays: "At five feet from the surface the top of the coal was reached and the shaft continued in coal to the bottom. tom a cut is made across the vein from east to west. from wall rock to wall rock, and is 24 feet 9 inches wide and de- velopes a width of 15 feet 7 inches of good anthracite coal." The coal is found in four beds, separated slightly, one of which con- tains 5 feet 9 inches of solid coal, another 4 feet, one 26 inches and the fourth 44 inches. He says, "There are not less than five seams of anthracite coal in 'Third Hill' mountain." This seam has been followed and its presence shown by openings for a distance of twenty- five miles. No coal has ever been mined here save the few samples taken out by persons prospecting. Several analyses have been made of the coal from this deposit, a few of which we give as follows: One gives the water and volatile matter at 11 per cent., the fixed carbon 82.54, and the ash 6.46. Another gives: fixed carbon 88.05, volatile matter 5.28, and ash 6.66. Still another gives: moisture at 100 degrees, 2.45, volatile matter 6.85, fixed carbon 86.29, ash 4.40. SPLINT COAL. The splint coal is a very hard variety found principally in the Middle and Lower measures and almost entirely in that part of the State between Braxton county in the center and Wayne in the southwest, the borders of the area extending for a consider- able distance on either side of the central line. The coal is thus spoken of by Professor Maury: "For the combined purposes of ? 24 COAL. AMPATTI, ATKAKAA betale steam, domestic use and the manufacture of iron, it may be looked upon as the most useful and valuable coal of the State. Its value is due to its firmness and solidity, which enables it to be handled, shifted and stored with very little loss; it burns well, leaving but little ash; has both high calorific power and intensity; is usually remarkably free from sulphur (iron pyrites) and other impurities; has little or no tendency to clinker; is free from the danger of firing by spontaneous combustion-a great desideratum in storage and ocean transportation; is first rate as a steam and household fire and has a particular adaptability in the raw state to the manufacture of iron in the blast furnace, for which purpose it is eagerly sought in districts accessible to market, as it makes a quality of iron which can only be surpassed by the use of charcoal." It is an especial favorite for shipping because of the small loss in handling or from exposure to the weather and finds a ready market from the variety of uses to which it is adapted. It is mined extensively in the Great Kanawha valley and along the western end of the Norfolk & Wes- tern railroad in this State. The coal is very hard but splits easily and smoothly and is mined in large lumps. In some of the Wayne county mines the coal has a tendency to split into long and thin pieces so that it has been likened by some to fence rails. CANNEL COAL. The cannel coal is one of the most valuable varieties found in the State. It is rich and oily, and contains a larger proportion of vola- tile matter than any of the other coals found in the State. Its ap- pearance is doubtless known to all our readers. Of a dull, black color, the coal will take, when polished, a brilliant lustre. It is more tenacious and less brittle than other coals and may be cut or carved into any shape. The coal is clean and will not soil the whitest sur- face and yet contains a large amount of oil. It was from the rich and oily cannel coal that oil was made before the war. From good cannel coal from 40 to 80 gallons of crude oil were produced to the ton; the Peytona coal yielding 20 gallons of crude illuminating oil, 52 gallons of crude lubricating oil, and 7.2 gallons of oily paraffine. Total 79.2 gallons to the ton. The discovery of petroleum made oil so much cheaper than it could be made from coal that the "cannel coal oil" was soon displaced and gradually fell into disuse. But for COAL 25 12 making gas there is no better coal, more gas and that of greater brilliancy being produced from a pound of cannel coal than from any other coal found in America. For fuel the cannel coal is not surpassed. It burns with a brilliant light, makes an intense heat and leaves but little refuse. It brings a much higher price than any other coal found in the State. BITUMINOUS COAL. By far the most widely distributed coal found in the State is the ordinary bituminous coal, valuable for fuel, gas, steam and coking. purposes. It is found in almost every county in the State and in great variety. Not only is it found in counties where the other coal is not, but nearly always in the same veins with other coals, bitu- minous is also found. This coal is mined more than any other in the State, and by reason of the greater variety of uses to which it may be put and the cheapness with which it may be mined, the demand for it is greater than for any other kind. The veins vary in thickness from a few inches to more than 20 feet and the char- acter of the coals varies almost as much. While splint and cannel coals are largely mined, it is the softer coals that give the value to the coal fields of West Virginia, and employment to thousands of its people. From them the fa.nous West Virginia coke is made, which rivals the celebrated coke from Connellsville, and in the manufacture of which long rows of blazing furnaces may be seen. from almost any passing railroad train, brightening the hillsides with their lurid light and filling the valleys near them with their smoke. The character of the West Virginia coals can be seen from the analyses given in the following tables. Their richness in both vol- atile matter and fixed carbon, their freedom from injurious sulphur and ash, their many points of excellence and their superiority over other coals whose analyses are also given may all be noted by the careful observer. ! 26 COAL. * NAME OF COLLIERY. Crown Hill Coalburg... Paint Creek.. Paint Creek.. Acme. Acme. Black Band.. • Blacksburg. Cedar Grove. Winifrede.. Peel Splint Coal Co.. Average Kanawha Gas Coals.. Gauley Mountain. Powellton.. Clements. Montana Monongah. Despard.. Howard. ► · W Tug Fork.. Cassville. Ferguson.. Peytona Canne)…… Cannelton Cannel... Lost Run Canuel... Twelve Pole Cannel. Redstone Coal. Redstone Coal.. Sewickley Coal. Waynesburg Coal. • · -- +4 + • Austen Davis... Thomas Boggs Run. Moundsville.. · · County. Great Kanawha.. Great Kanawha. Crescent..... Black Peerless... Campbell's Creek. Nuttallburg. Nuttallburg. Fire Creek.. Quinuimont Average of all New River • * Mines... Average of 10 samples Mercer and Flat Top Coal... Pratt's Lands...... Twelve Pole……. Stevens' Branch.. $6 CL (4 0.35 6+ Kanawha . 62.61 33.26 2.14 0.18 62.00 33.50 3.65 63.74 30.13 .. Li 66 Fayette MA เเ 6. 6. 60 * SA $6 CC "" Kanawha * Fayette " 26 .. Wayne. " McDowell. Webster.... ANALYSES OF COALS. · Marion.. "" Preston Tucker. < → Harrison... 66 61.18 38.74 44.89 43.22 51.35 38 70 41.00 46.00 Kanawha .. 23.50 58.00 Boone, Taylor...... 42.32 23.08. Wayne. 42.59 49.40 Monongalia 54.36 37.88] 0.37 Marion ... 50.33 40.97 1.01 Monongalia 54.31 35.78 0.44 AL Fixed *G Carbon. Ohio Marshall. Volatile Matter. Water. 60.77 36.26 1.84 57.90 37.09 1.93 0.62 53.22 41.36 1.66 0.80 57.48 38.58 2.24 56.75 41.17 1.23 61.27 36.83 58.73 36.33 1.36 57.781 35.34 1.75 Sulphur. 56.26 37.36. 1.25 64.00 32.60 1.40 1.28 0.23 61.75 34.91 0.94 0.16 58.43 38.48 0.62 0.56 0.81 59.89 34.61 1.14 59.10 36.72 1.27 0.77 0.37 0.57 58.62 38.05 0.90 61.07 35.64 1.51 70.67 25.35 1.35 69.00 29.59 0.34 .0.78 75.50 22.42 0.73 0.53 79.29 18.65 0.76] 0.23 74.04 23.20 0.83 0 50 0.76 0.55 74.06 18.83 0.69 68.20 29.40 0.95 56.35 37.60 1.60 60.10 36.40 1.70 0.57 0.72 • 1.56 3.45 0.36 1 0.82 1.92 Ash. 1.81 Dewey, Vance & Co. 1.50 D. G. M. Levette. 6. 13 R. O. Doremus. 1.13 P. B. Wilson. 3.08 E. L. Howard, U. S. G. S. 3.75 1.70 R. M. Byrnes. 0.85 1.90 2.72 Winifrede Coal Co. 5. 13 A. R. Otter. 3.85 C. & O. Coal Agency. 2 00 W. N. Page. 2.40 Hy. Froeling. 1.91 (" 2.87 4.27 7,691 3.10 9.47 56.36 35.36 0.74 0.70 7.55 55.02 37.00 1.00 0.80 56.57 36.78 1.42 0.71 53.48 36.92 1.52 1.08 53.03 34.00 55.76 37.36 1.10 58.00 38.00 1.50 1.82 0.50 67.18 26.84 0.80 1.68. 72.76 22.90 0.96 0.59 46.30 43,29 1.20 44.30 45.17 1.01 1.23 8.29 4.36 A. S. McCreath. 2.91 J. W. Mallet. 2.43 F. P. Dewey, U. S. Govt. 1.21 Riverside Iron Co. Authority. 2. 10 Prof. Eggleston. 1.07 C. E. Wright. 0.80 A. S. McCreath. 1.11 Prof. Eggleston. 1.43 M. F. Spruce. 5.64 A. S McCreath. 1.45 Hy. Froeling. 6.05 Wormley. 3.50 .. 1.88 Taylor. 10.33 Dwight, 6.50 Hy. Froeling. 13.00 Manhattan Gas Light Co. 18.50 66 34.01 C. E. Dwight. 7.41 7.39 66 * 66 (6 (L C 6.00 A. S. McCreath. 4.51 (C 7.00 6.07 Washingt'n Gas Light Co 3.96 S. C. Ford. 0.20 P. B. Wilson. 3.50 66 2.79 J. W. Powell. 9.30 C. E. Dwight. : * 7 TIMBER. 27 TIMBER. The claim is made, and figures are given to prove it, that West Virginia has a greater amount of hard wood timber in its forests. than any other State in the Union. Ex-Governor Wilson says: "I have the statistics to prove that West Virginia has more of a surplus of hard woods than any other ten States in the Union." This is rather an extravagant claim for so small a State but a thorough examina- tion of the forests will show that nearly or quite one-half the State is still uncleared, and by far the greater portion of the uncleared lands is still in virgin forests where the axe of man has never found its way and where the magnificent specimens of forest growth stand thickly side by side and reach a towering height which gives the forests of the State their splendid values. Except in California where the redwood trees attain tremendous size no finer timber may be found within the confines of the Union than that which grows in West Virginia. The splendid forests of thousands of acres. of untouched timber, where nearly every kind of timber found in the North American continent may be seen, where trees grow to such size that ordinary methods will not suffice to handle them and where the forests are so thick that the light of day scarce penetrates their shade and pathways must be cut before the axemen can find room to work, have yielded annually many million feet of timber which has gone to nearly every country on the earth and given the West Virginia timber a world-wide reputation. From European countries capital has come and been invested in the woods of West Virginia, and agents come from England every year to purchase West Virginia timber. No finer oak or poplar grows beneath the sun than that which may be found in almost any county in the State. The magnificent size, the excellent quality of the timber and the great variety give to the timber lands of West Virginia unusual value and have, particularly in the last few years, attracted *M 28 TIMBER the attention of timber men from almost every quarter. Some ten or fifteen thousand men are now engaged in one way or another in timber, lumber, sawmill or kindred business. Tre- mendous onslaught has been made upon the forests. Great armies of choppers have, with their axes, made inroads on the woods throughout the State and every rise brings out of every stream, how- ever small, its quota of logs or ties or other timber. It is almost impossible to get any statistics on the lumber business and the amount of lumber cut annually in the State. In 1880 the total amount of various kinds cut within the State was about 180,000,- 000 feet. To-day it is far more than twice as much. New saw- mills are building every day, new territory being opened, and it is safe to say that now the total cut of all the mills is no less than 500,000,000 feet a year. The forests are being rapidly destroyed. Not only trees of proper timber size are being cut, but smaller ones for telegraph poles and railroad ties are also taken out. The trees both large and small, the bark for tanbark and small hickories for hoop-poles are all removed and but a short time is required to change. a forest to a farm, to bare the mountain tops and clear their sides, to turn the timber into ties or work it into lumber or its products. To show the size of some of the trees cut from the West Virginia forests we give the following measurement of a poplar tree recently milled at Camden on the Gauley, cut in Nicholas county in one of the finest poplar regions in the State: 2 Logs 60 Iuches Diameter, 16 Feet Long, Scaled 5,912 Feet, Board Measure. *) 6. 63 *C 66 16 CA 6.802 63 69 Broken, Sca led 1 1 に ​* 46 ་་ Total.. ++ L6 › 66 61 12 10 ( ܀ << 66 CC 2,611 2,611 6,761 24,727 66 66 66 66 DISTRIBUTION AND VARIETY. + • ¿ " (i (¿ Writing of the forests of West Virginia for the World's Fair edi- tion of the Baltimore Evening News, Maj. Jed Hotchkiss, one of the best posted men in the South, particularly on the resources of the two Virginias, has the following to say: "West Virginia is undoubtedly the timber State of all the States east of the Mississippi; in fact of all the States on the Atlantic slope + TIMBER. 29 $ [ 1 1 of the continent. Fully three-fourths of its 24,645 square miles of area are still covered by virgin forests, and in all the remainder of the State where the forest maps indicate that the valuable timber has been largely removed, there are still large numbers of timber trees included in the portions of farms that are held for forest pur- poses. "This State is very favorably located for the growth of forests. It is in the favored belt of temperature between about 37 degrees and 41 degrees of north latitude. Within its boundaries, trending northeast and southwest, thus opening the country to the damp, warm winds from the Gulf, are numerous ranges of the great Appa- lachian, or Atlantic Highlands, but by far the larger portion of the State lies on the westward slope of these mountains in the Trans- Appalachian belt, the waters of which mostly run to the north west- ward to the Ohio. The altitude of the country descends from the Backbone or Alleghany range of the Appalachians, from an alti- tude of from 2,500 to 4,500 feet to from 500 at the southwestern corner of the State on the Ohio, at Kenova, to about 600 on the same river at Wheeling. The altitude of the eastern corner of the State at Harper's Ferry is 272 feet; so the range of altitudes in the State is from 272 feet to about 5,000, giving a climatic range of 4,728 feet or the equivalent of about 16 degrees of latitude; consequently this State has extensive areas of adaptability for every variety of forest growth that is found within the limits of the United States east of the Rocky Mountains. Dr. Charles F. Millspaugh, in his Preliminary Catalogue of the Flora of West Virginia, 1892, says of this State: 'It appears to be the southern limit of many boreal, the northern of many austral and the eastern of many occidental forms. It bids fair also to continue to present many novelties.' "The most e'evated portion of the State, the great eastern border of the ridgy plateau from which the Trans-Appa achian country descends, a territory some 200 miles in length from the head waters of the Big Sandy to the head waters of the North Branch Potomac, a region that in the main is from 3,000 to 5,000 feet in altitude, furnishes a congenial home to the black spruce, the white pine, and other evergreen trees peculiar to northern latitudes. "It is probab'e that nowhere in the United States are now exist- ing denser forests than those of black spruce in the belt of country, 30 TIMBER. : more than 100 miles in length and from 10 to 20 in breadth, that extends through Greenbrier, Pocahontas, Rando'ph and Tucker counties. From measured acres of this territory as many as 60,000 feet of board measure of lumber have been cut. Only the northern end of this vast spruce forest has been penetrated by railways, the West Virginia Central & Pittsburg R. R. being the only one that has yet really entered into it. In this same e'evated region there are extensive forests of wild cherry of a luxuriant growth. One white pine belt, with a length of 70 mi es and an average breadth of 10 miles, borders this spruce belt on the southeast in the basin of the Greenbrier river. Another white pine belt, some 60 miles in length and having an average breadth of 10 miles, pene- trates this spruce belt from the northeast up and along the basin of Cheat river; while another white pine area, some 30 miles in length and 10 in breadth, is found in the counties of Raleigh and Wyo- ming. On the crests and higher slopes of the dozen or more moun- tain ranges of the Appalachian system that traverses the State in a northeast south west direction from its eastern border to the west- ward, are found other species o pine and several species of birch, oak, maples and other trees such as are peculiar to the higher alti- tudes of the country. "The remainder of the State is covered mainly with hard- wood forests interspersed with a per centage of the soft- woods such as poplars, ash, etc. As an illustration of the kinds and distribution of these trees an example may be taken from the southwestern portion of the State, from the basin of the West Fork of 12-Pole river, in Wayne and Logan counties, where the merchantable timber on 12,263 acres, or nearly 20 square miles, was actually measured and counted. The trees that were measured were those that were 18 inches in diameter and upward, four feet above the ground, with the exception of locusts, hickories and black walnuts which were measured from a diameter of 10 inches and upward. The varieties and numbers of commercial timber trees at this time growing on this area are as follows: n TIMBER. 31 2 ** 1. White Oaks. 2. Chestnut Oaks. 3. Black Oaks.. 4. Red Oaks.. 5, Hickories.. 6. Chestnuts... 7. Locusts.. 8. White Maples. 9. Sugar Maples. 10. Birches.. 11. Gums.. 12. Black Walnuts. 13. Sycamores. • • 1. Tulip-Poplars 2. Pines.... 1.—TABLE OF HARDWOODS. Whole number of Hardwood Trees 3 Lindens 4. Cucumbers. 5. Buckeyes.. 6. Ashes.. 7. Hemlocks.. * D · 2.--TABLE OF softwoods. 24,760 38,848 8,525 943 21,298 7,681 1,996 1,583 450 1,344 1,044 393 13 . 108,878 12,450 3,472 2,325 240 28 271 903 Whole number of Softwood Trees. 19,689 "This summary shows that this area contained 128,567 timber trees of 32 species; 25 of these kinds or 108,878 trees, were hard- woods; and 7 of these, or 19,689 trees were softwoods; making the percentages of the whole number of timber trees as 84 per cent. of hardwoods and 16 per cent of softwoods. The average number of these timber trees to the acre is ten and a fraction. "Interspersed with the trees of these tables are found nearly all of the varieties of smaller trees that are subsequently named in this article as exhibited in the West Virginia collection at Chicago. These countings were made on lands extending from the West 12- 32 TIMBER. Pole River up to the summits of the dividing ridges on either side taking in a range of altitude from about 650 feet to a little over 1,000 feet. This specimen of forest fairly represents the entire north- western portion of the State from the Ohio River to the southwest for about 75 miles. In other words, a belt of country 160 miles long from northeast to southwest and 75 miles wide from northwest to southeast. "Another illustration of the distribution of commercial trees for the intermediate country between the high plateau and the belt above mentioned may be taken from the counting of a thousand acres on the headwaters of Cherry River in Greenbrier county, West Virginia, in a region having from 2,500 to 3,000 feet of alti- tude. The trees counted and measured were all from 18 inches and upward, except the hickories and locusts. The species and numbers. were as follows: 1. White Oaks... 2. Chestnut Oaks. 3. Red Oaks 4. Hickories. 5. Chestnuts.. 6. White Maples. 7. Sugar Maples. 8. Locusts 9. Beeches. 10. Birches. 11. Gums.. 12. Cherries 13. White Walnuts.. • 1.—TABLE OF HARDWOODS. • Whole number of Hardwood Trees.. 2.—-TABLE OF SOFTWOODS. 1. Tulip-Poplars.. 2. White Lindens 3. Yellow Lindens. 4. Ashes... 5. Hemlocks.. 6. Yew Pines. Whole number of Softwood Trees.. • • G 132 159 889 86 1,513 3.258 7,291 4 1,965 1,120 104 349 1 16,871 529 1,014 937 576 2,303 34 5,393 1 TIMBER. 33 "Of these 19 species of trees, 13 are hard woods and 6 soft woods. The whole number of trees is 22,264, of which 16,871, or 76 per cent. are hard woods, and 5,393, or 24 per cent. are soft woods. The average number of timber trees per acre is over 22. "The differences in the varieties, numbers and percentages of trees The timber belt shown in these two tables are quite remarkable. which is represented by this second table is one that extends across the State for full 200 miles, from McDowell county in the south- It has an average west to Preston county in the northwest. breadth of about 25 miles and is probably the most valuable of the timber regions of the State. As it is bordered on the east by the high region of evergreen timbers first described, it is evident that, taking this belt and that together, making a belt of timber extending somewhat centrally across the State from southwest to northwest for 200 miles, and with an average breadth of about 35 miles, that West Virginia has in this 7,000 square miles of territory one of the most valuable timber regions, in the extent, variety, quality and quantity of its timber now remaining in the United States." VALUE OF TIMBER. - In addition to this, further information as to the extent and value of the timber forests of the State may be found in the fol- lowing extract from the article written recently by Maj. John Moulton for the Kanawha Gazette, at Charleston, in which he esti- mates-and his estimate is rather low than high-the value of tim- ber standing in the State at seventy million dollars. He says: "With the exception of the highest mountain ranges, where there are to be found large forests of white pine and spruce, the timber throughout the State consists almost wholly of hard woods, comprised of the different kinds of oak, chestnut, hickory, poplar (tulip), cherry, black walnut, white walnut, ash, birch, locust, sugar maple, etc. Of these, the oak family is by far the best represented, comprising probably one-third of the entire growth; and of the oaks the white is by far the most plentiful. Next among our valuable timber trees in quantity is the poplar which, owing to its adaptability to so many uses, makes it one of the most valuable timber trees in the whole country. Black walnut and cherry are our most valu- able woods and are found scattered throughout the State, but no- 34 TIMBER. 7 ¿ where in great quantity. Ash is also found throughout the State, in greater quantities than walnut or cherry, but much less than poplar. "Of all the different species of hard woods, oak, poplar, black walnut, cherry and ash comprise principally the hard woods which have been manufactured into lumber, owing to the fact that they only furnished lumber whose price would justify the cost of manu- facturing and transportation to distant markets and of these, only excepting walnut, such trees have been used as would make largely the better qualities of sawed lumber, or in oak, staves. "The mountainous character of the State has also confined opera- tions in lumbering to streams large enough to float logs on to the lines of the railroads, leaving a large part of the State untouched. "While this characteristic of the State increases the cost of put- ting the manufactured lumber into the hands of the consumer and preventing its manufacture entirely over large districts, it is not without its future benefit to the State and to the owner as it has curtailed the manufacture, preventing a cut of timber beyond the demands and increasing its value in decreasing the aggregate amount by use only of that more attainable. "Any estimate of the standing timber in the State can only be a matter of opinion but taking the amount of the surface of the State still covered with timber, which I believe is nearly two-thirds, and deducting from it the lands cut over for good timber along streams. and railroads, by a liberal estimate two-fifths of the State is still in the virgin forest or about seven million acres which estimating at two and one-half thousand feet per acre at an average price of two dol- lars per thousand would make the large sum of thirty-five million dollars as the value of the standing good timber. "This estimate of the number of acres of timber lands and amount per acre, may be considered small, but it must be taken into con- sideration that I am only considering such timber, oak, poplar, walnut, cherry and ash, as would make lumber mostly suitable for shipping, and also that parts of the land, such as barren south hillsides, are substantially bare of timber, and that I do not include the white pine and spruce of the upper mountain regions. "But in regarding the timber values of the State, shipping lum- . + TIMBER. 35 # ber, or the best grades, should not by any means be alone taken into account. "Our wild lands, it is well known, are held very generally in large bodies, and valued to a great extent for the minerals under- lying them. For the development of these minerals all the coarser grades of timber, comprising every kind of hard wood, will be needed, and will aggregate in value for this home consumption fully as much as that of the higher and better grades. ! "Again, unlike some other sources of national wealth, the quan- tity and quality of the timber of our State, depends on no contin- gency, and its value must increase, as everywhere the consumption of lumber is greater than the natural growth of the forests. "Of the quality of our timber there is no longer any question of its being eagerly sought after by manufacturers all over the country.' * $ 36 IRON. In 1856 In 1867 In 1878 In 1889 In 1890 In a recent pamphlet on the iron ores of the two Virginias, Judge Homer A. Holt, of the Supreme Court of Appeals of West Virginia, and Adam C. Snyder, ex-Judge of the same court, give facts and figures to show that in the world's iron production in the future the Virginias must take a prominent part. From an exhaustive treatise on the subject we take the following extracts: The world's production of iron in round numbers has been as fol- lows: - IRON. 6,600,000 gross tons. 46 (C 9,300,000 14,100,000 25,000,000 26,500,000 (L (6 (C (( (( (6 The ratio of increase is thus shown to be for the first period of eleven years about forty per cent.; for the second period over fifty- one per cent; for the third a little less than eighty per cent., and for the single year ending in 1890 nearly seven per cent. If this accel- erating ratio of increase is maintained, and the probabilities are that it will be greatly exceeded, then the production for the year 1900 will be in excess of fifty million tons. A : J IRON. 37 ! The relative per cent. of the world's product from 1867 to 1890 has been as follows: United States Great Britain 52.80 France, Germany and Belgium 26.00 All other countries 6.70 MAG In 1856 the product was (C 66 In 1867 " In 1878 " In 1889 " In 1890 " 66 It is thus shown that the production of the United States, which was only 14.50 per cent. in 1867, rose in the succeeding twenty- three years to 33.00 per cent., equal to one-third of the entire pro- duction of the world, while Great Britain, which up to 1889 pro- duced more iron than any other nation, fell off in the same twenty- three years from 52.80 to 28.23 per cent., nearly five per cent. less than the United States, which is now the leading iron producing country of the world. 66 The following table shows the pig-iron production in the United States for the past thirty-five years and the per cent. of increase at stated periods: (6 (( 1867. Per cent. 14.50 (6 (6 1878. Per cent. 16.80 45.20 28.75 9.25 1889 Per cent. 30.57 33.16 27.98 8.29 - 1890. Per cent. 33.00 28.23 Nel tons. Increase. 883,137 1,461,626 65 pr. ct. 2,577,361 76 pr. ct. 8,516,068 238 pr. ct. 10,309,028 20 pr. ct. This presents the capabilities and progress of the iron industry in the United States in a degree unprecedented in any othér country of the world. The rate of increase in the eleven years ending in 1889 was more than three-fold as great as it was for the eleven years immediately preceding, and that for the year 1890 was over twenty per cent. more than the very heavy product of 1889. Great Britain, France, Germany and Belgium, together with the United States, produced more than ninety per cent. of the entire iron product of the world. In regard to these the statistics show that neither Great Britain nor France has produced as much in any one year since 1882 as it did in that year, and that the aggregate production of Germany and Belgium in any year since 1883 has ex- ceeded their aggregate product for that year less than one million 38 IRON. tons. Since these, the principal iron producing countries of Europe, have not increased their production to any appreciable extent in the last seven years, during which period the United States has doubled its production, it is safe to assume that they are not likely to increase it to any greater extent in the future. The increased production of iron in the United States for the year 1889 over the year 1888 was about 800,000 tons greater than it was in all the other countries of the world, and notwithstanding this startling fact the consumption of iron in one form or another by the people of the United States during the year 1889 exceeded the domestic production of that year nearly one million tons It will therefore be concluded that the increased demand of the world for iron must be mainly, if not entirely, supplied by the United States. In support of this conclusion, Mr. Edward Atkinson, in a paper on the future situs of the principal iron production of the world, says: "What will be the product in the United States in 1900 as com- pared to 1889 if the world demands forty to fifty million tons of iron? Where will it come from? Who will supply it? Will it not be sixty per cent. of the whole or more? *** If the increase from 1890 to 1900 should be ten per cent. per annum the product of the year 1900 will be about 42,000,000 tons. From what other sec- tion of the earth's surface will an additional supply of iron, rated at the lowest at 1,000,000 tons a year, year by year, and perhaps rising in years of extensive railroad construction to double or treble, be derived? * * * I may not venture to say in this treatise that the supremacy in this branch of industry has passed away from Great Britain, but the increasing scarcity of her fine ores, the increasing depth of her coal mines, the great heat and difficulty in working them, the near exhaustion and consequent high price of coking coal and the change in the condition of the workmen in Great Britain. may sustain such a conclusion. The question is not, however, whether the United States will take away any part of the present iron production from Great Britain. The true question is: Can the iron producing countries combined, readily meet the prospective increase of demand?" Ever since iron has been produced by the use of mineral fuel in this country, Pennsylvania has made more than one-half of the entire output. Next to Pennsylvania, though far behind her, the States 2 IRON. 39 # i of Ohio, New York, Illinois and New Jersey have, until the last few These older pro- years, been the principal iron producing States. ducing States have, in a measure, exhausted all their easily available ores. They are obliged to depend largely upon a basis of supply hundreds of miles from their furnaces. Of these States, Pennsyl- vania and Ohio are the only ones that have any considerable quan- tity of both iron ore and coal within their own territory, and each of these States obtains the greater part of its iron ore supp'y from the Lake Superior mines, or by the importation of foreign ores on which latter they have to pay a duty of seventy-five cents per ton. Neither New York nor New Jersey has any coal, and Illinois has no iron ore within the State. In the growing competition of the iron industry and the lessening of its profits, iron must be made where the conditions are most favorable and where it can be made the cheapest, and not where it is made at present, simply because it has been made there hereto- fore to advantage. Industry must, and always will, sooner or later, adjust itself to the most favorable conditions. It finally becomes simply a question of "the survival of the fittest." The present state of the iron pro- duction in these older States is largely maintained by the momen- tum of the great capital invested in plants and ways for transporta- tion in the centres of iron making. This cannot be changed on a sudden, but when competition from points possessing more favor- able conditions reduces the price of the product below the cost of production, then, if not sooner, the change will be made. It may not be ventured to assert that this state of affairs has already arrived, but it is possible to believe that the present depression in the iron industry is in part, if not largely, due to the persistent efforts of interested capitalists and railroad companies to maintain the major part of the industry at points. where iron production has ceased to be remunerative. If the capital which is invested in plants and means of transportation in the older iron producing sections were transferred to more favorable localities, iron could be produced there at present prices at a fair profit. The depression, therefore, is due less to the price of iron than to the disadvantages and unfavor- able conditions under which it is produced. Three things are essential to the production of iron, namely, ore, 22. 40 IRON. S coal and limestone; and these must be so situated geographically as to be cheaply brought together; for the value of raw material does not more consist in what it is than where it is. The "centre of gravity" of the iron industry will, sooner or later, adjust itself at the point where the facilities for obtaining the raw material are the best and the cost of assembling them at the furnace is the least. These requisites, as we have seen, do not, to the extent desirable, exist at the points where the principal iron production is now and has heretofore been maintained. The important inquiry then presents itself: Are there any points within the United States possessing conditions more favorable for the production of iron cheaply? In maintaining that the South has superior natural resources for the production of iron, and that in the near future it will attain an important, if not the controlling, position in this industry, it is not necessary to assert that there will be any immediate decrease in the production in other sections. It is maintained, however, and the facts seem to warrant the conclusion, that in view of the more favorable natural conditions of the South, it is not probable that any important part of the increased production necessary to meet the prospective demand will be had in the older producing States. It may, and probably will for years, tax the capabilities of all points and sections within the United States to supply, not only the present, but the enormous prospective demands of the world. In 1870 the South produced only 184,540 tons of iron; in 1880 she increased her production to 359,436 tons, and in 1890 she made the phenomenal advance to 1,780,909 tons, or over eighteen per cent. of the entire product of the United States. This was an in- crease of seven per cent. of her relative production in the decade from 1880 to 1890, thus showing that the North and West fell off that much. ایل The greatest activity in the development of the iron industry in the South during the last decade was in Alabama, and in the past few years it has been very great in Virginia. The increase over the production in 18S0 in the former was 1,328 per cent. and in the latter 1.589 per cent. Of the thirty-nine furnaces under construc- tion at the close of the census year 1890, nine were in Virginia and seven in Alabama and only five in Pennsylvania. IRON. 41 The facts above stated show the great importance that must attach to West Virginia ores, which, though yet practically unde- veloped, nevertheless are known to abound in many, if not most, of the counties of the State. At various times, before and since the organization of the State, iron has been made from West Virginia ores. Small furnaces have been operated in nearly all the counties where iron ores are found and in many counties utensils are now in use which were made many years ago at local furnaces and foundries. The ores, in nearly every instance, produced an excellent article of iron and made the business profitable while it lasted. The mountainous character of the State, the absence of railroad facilities and the difficulty of getting articles of iron into the country homes from far-away markets, was the necessity which brought about the erection of iron furnaces throughout the counties of the State where iron ores are found. They were operated only for local use and were necessarily small. When railroads began to be built into the State and iron made at larger furnaces in older localities and with better facilities began to be sent in by rail, the business of the local furnaces ceased. Gradually they all closed down, and now there is not a furnace running in the State. But still the ores are here, of sufficient richness and in sufficient quantities to be prof- itably worked, if railroads were to open up the valuable ores. In nearly all the counties through the centre of the State, from Monon- galia and Preston southward clear to Wayne, ores of greater or less value may be found. In many of these counties iron has been made but the finest ores, the richest and the most, are found in the eastern border counties along the Alleghany mountains. In all these counties ores abound, of splendid quality and in large seams, but owing to the difficulty with which they can be reached by rail, no development has ever yet been made. Just across the border, in Virginia, numerous furnaces have been in operation making iron for years, and for all these furnaces the coal and coke is taken from the West Virginia beds to use in making iron. On this side of the mountains we have the same iron ores which are so success- fully worked in the old State, we have the limestone for the fluxing, we have the finest coking coal in the world and almost at the mouth of the ore pits, so that iron at least the equal of the Virginia iron. · ܀ S 42 IRON. vladavati A ; could be successfully made in our own State and at a smaller cost than on the eastern side of the line. The Alleghany mountains form the entire eastern border of the State, and from Jefferson county, in the north-east, to Mercer and McDowell on the south-west, the same kinds of valuable iron ores are found in great abundance. The same are found on both sides of the mountains in the two Virginias. In the old State more has been done toward their development than in the new and they are better known, but in some parts, at least, of the western State, the ores excel those of the eastern neighbor and in nearly every part. are similar to those similarly situated across the border. Professor Orton, a somewhat noted geologist of Ohio, who has made an exam- ination of the Potts Valley ores, lying partly in Virginia and partly in West Virginia, has made a very favorable report upon them. As the greater part of the iron ores in the eastern border counties of the State are similar to these described, we quote from Professor Orton to give a general idea of the ores of the Alleghany counties of the State. He says: Iron Silica - "The Oriskany ore is in all cases a hydrated peroxide or limonite, popularly known as brown hematite. * * * Potts Creek ores, which I sampled in the field and the analyses of which have just been completed by Prof. N. W. Lord, Chemist of the State Geolog- ical Survey of Ohio, show the composition given below, the samples having been selected from eight different points in the ore field, numbered, respectively, from one to eight. 1 2 3 4 5 6 7 S 49.90 50.03 51.94 50.00 49.90 49.90 55.50 56.00 11.61 13.26 10.15 9 67 15.76 12.05 4.45 10.69 .18 .11 .14 2.96 .39 .25 .29 .09 Phosphorus 1.64 2.78 .65 .68 18 .95 1.07 .18 "The average of the eight is as follows: Iron, 51.70; Silica, 10.95; Manganese, .55; Phosphorus, 70. Manganese, "In regard to these results it remains to be said that so far as the first three elements are concerned we have nothing to ask. The Potts Creek ores will certainly give a larger yield of iron than any of the Oriskany ores now worked in Virginia. They can be depended upon for nearly fifty per cent. of iron. One sample is seen to contain an exceptional amount of manganese, but even this is scarcely outside IRON. · 43 the allowable limits. In any case, it would be easy to exclude this phase of the ore in mining. "There remains to be considered the last of the constituents re- ported in our analyses, viz., phosphorus. It would be too much to expect that all possible advantages should be concentrated in a single district, and accordingly we find by examination of the fore- going analyses that some of the Potts Creek ores run higher in phosphorus than is to be desired. Excluding, however, a single sample (No. 2) from the list above given, the average of the seven remaining samples is .574. "When account is taken of the high percentage of iron that these ores carry, it is obvious that they must come within the limits of acceptance. * * * "I must not fail to call attention to the splendid showing of the Upper Bennett bank (No. 8) in the table of analyses. The finest outcrop of brown hematite in Virginia is at the same time the richest and purest ore of its class.” Of the same ores Prof. A. S. McCreath, a Pennsylvania geologist, says: "These ores may be classed as Brown Hematite, which are hy- drated oxides of iron. But the proportion of chemically combined water varies considerably, and they may be said to vary between the extremes of a true Limonite with 14.40 per cent. combined water, and Red Hematite with theoretically no combined water. far as the percentage of iron is concerned, the ores are all of high grade, and many of them equal the very best brown ores that are mined.” The ores thus described in the pamphlet above referred to lie in the counties along the southern border of West Virginia, while northward through all the border counties of the State the same va- rieties of ore may generally be found. In subsequent portions of this work where the counties are taken up separately and described, more full descriptions of the iron ores of those localities will be found. The red fossiliferous ore, which is found in large deposits in some of the north-eastern counties, is a valuable ore, comparing most favorably with the ores of more successful and more noted iron regions of the country. While most of the best and most valuable iron ores are found along the eastern border of the State, they are not all found there, : 2 44 IRON. 2 * N for to the westward throughout most of the counties of the State ores of greater or less value are to be found. The western border counties do not seem to have much iron, but through the center of the State to the eastward the ores are plentifully scattered. Through the central part of the State in the coal measures two kinds of ores are found-carbonates of iron and black band ores. Speaking of the former, Prof. M. F. Maury says: "Under this head may also be classed the brown hematites of the coal measures, as they are merely the results of the decomposition of the carbonates, and in fact, when a seam of the former is discovered, we may expect it to turn into the latter as soon as we go far enough under ground to get beyond atmospheric influences. "We see the result of this decomposition in the pieces of Brown. Oxide that are found on the hills in every portion of the State. These have led to many erroneous ideas as to the richness of certain localities in this mineral, which came originally from the carbon- ates of iron existing in the beds that were once superimposed upon the present strata, and have long since been worn away by erosion. As this took place, the lighter materials were washed off by the cur rents, while the heavier ore settled down and was left resting on our hill sides. Sometimes a great deal was deposited in one place, and the soil is full of it, while in others but a single lump was left, and hence it is that on many of our mountains we find the 'blossom' of good ore, and yet have no bed of it near by." Of the black band ore, a very valuable ore, found in the central to the south-western part of the State, principally south of the Great Kanawha river, Prof. Maury says: "This is nothing more than a carbonate of iron, of a more or less black color, by reason of an admixture of bituminous matter. So far as yet known, it is confined entirely to the southern part of the State, where it has been discovered only within the last few years. From the fact of its very often resembling black slate in its struc- ture, it may often have been passed over unnoticed, and careful search will no doubt show it in many places, where it is not now suspected. "It is a class of material that makes an excellent iron, and from which much of the celebrated Scotch-pig is smelted. It possesses an especial value, from the fact that, in many cases, a low grade ore IRON. 45 22 2 : F can be roasted into a higher grade. For instance take that from Davis Creek, in Kanawha county. When mined, it contains 33 per cent. of metallic iron, and 26 per cent. of carbonaceous matter. By piling it in heaps, and setting fire thereto, the carbonaceous matter is burnt out, and in the process of combustion, generates enough. heat to convert the carbonate of iron in the ore into a richer oxide, so that the mass, after being thus roasted, analyzes 65 per cent. of metallic iron. "Unfortunately, we can never reckon or depend upon any seam of it continuing of a uniform value, for in one place it will contain an ore well worth working, while half a mile off it may become so mixed with slate or earthy impurities as to be utterly valueless. As an example: On Bell creek, Fayette county, an excellent bed about 4 feet thick was found by Mr. L. Bemelmans, of Charleston. Some 2 or 3 miles from this place, up a ravine a short distance be- low the mouth of Bell, the same seam showed only 12 to 14 inches of the good material, while on Little Elk run, of Gauley river, some three miles to the north, the results of two analyses from the same seam gave only 5 and 7 per cent. respectively of metallic iron. If we search for it in another direction, it may open to a very valuable deposit. From this irregularity and from the fact that it has been well proven in this field, it will be readily understood that careful search may find it in many places where it has never yet been no- ticed, and wherever it is found in workable quantity its presence. adds great value to the land." Otto Wuth, of Pittsburg, who made an analysis of some black band ore found in Kanawha county, says: "Thoroughly roasted, it would then contain about 65 per cent. of metallic iron, while there is more than enough carbonaceous matter to roast it. I consider it a black band ore of the first quality." Analyses of the iron ores taken from various counties of the State will be shown in the following table: 2 46 IRON. ܢ ..: KIND OF ORE. Carbonate. CL ( (6 6 "C เ Average of vari ous Samples. ) Carbonate.. * ↓ 看着 ​** CC 16 && .. << (C เ Brown Hematite.. Fossil.. Pipe.. Hematite Bluff Ore.. Brown Hematite.. Red Fossiliferous. Red Hematite.. Red Fossiliferous. Red Hematite Brown Hematite. Red Fossiliferous "K Co (6 6 < [( * • << C County. Red Fossiliferous. Manganetic Mineral 38.42 34.29 and Grant 38.28 16. 33. 17 44.43 39.87 46.67 Preston 46 CC 44 เ GA C 32.52 0.66 0.13 "C Monongalia 31.86 0.23 0.15 34.69 0.31 0.12 49.69 0.19 0.13 41.94 0.16 0.20 0.87 0.30 41 35 40.71 30.24 0.27 0.22 0.30 0.33 44.95 43.04 CC 38.91 0.29 35.98 0.20 39.10 0.23 Raleigh 55.54 0.81 Greenbrier 52.23 } (" <+ << (3 Taylor 156.58 159.36 51.09 62 01 52.52 Grant .88 Brown Hematite.. Hampshire 51.47 .10 (" .. (( Li 52.67 .03 Monroe 58.83 0.44 0.71 66 58.40 48.50 1.02 (6 C 4. (6 17 Hardy 66 .c CC CC C " tt Metallic Iron. 66 + Pendleton 66 '' Phosphorus. 61.75 57.17 36.69 44.42 56.23 .13 .58 .012 .69 .05 .16 57.11 0.71 151.95 0.59 50.22 1.04 45 92 0.66 52.09 1.25 51.80 1.06 57.10 .438 55.15 .5881 542 .292 · Sulphur. 0.05 0.48 0.42 0 35 .73 .42 .169 .04 .03 .04 .09 .48 .82 Silica. 24.96 Manganese. 2.82 0.21 3.60 0.74 17.67 0.27 6.23 0.08 14.85 15.34 0.14 21.20 0.10 12.74 0.11 0.10 13 02 3. 64 7.31 19.11 140.78 AUTHORITY. Prof. W. B. Rogers. CC (6