Page:Encyclopædia Britannica, Ninth Edition, v. 24.djvu/554

518 WEST VIKGINIA The drainage system of the State is in some respects peculiar. Although the general slope is towards the north-west, the Potomac, which flows south-easterly to the Atlantic Ocean, has cut its way far back into the plateau, and drains, by means of numerous long branches, the north-eastern quarter of the State. The remainder of the State is drained to the Ohio by means of several large branches which flow in a general north-westerly direction. Heading in the south-west is the Big Sandy, forming a portion of the State boundary. Fourteen miles above its mouth enters the Guyandotte, and 50 miles above the Guyandotte comes the Great Kanawha, one of the principal branches of the Ohio. This large and powerful stream has cut its way back beyond the crest-line of the plateau, tapping numerous streams in south-west Virginia and western North Carolina, so that its sources are now against the Blue Pudge in the latter State. It is known in North Carolina and Virginia, and in West Virginia to the Great Falls, by the name of New Eiver. In West Virginia it has numerous large tributaries the Big and Little Coal rivers, Piney, and Bluestone from the south, and the Pocotaligo, Elk, Gauley, and Greenbrier from the north. The next branch of the Ohio, proceeding northward, is the Little Kanawha, which empties into the Ohio at Parkersburg. The north-western part of the State is drained by the Monongahela, one of the two head branches of the Ohio, and its tributaries, the principal of which are the Tygart s Valley, Cheat, and Buckhannon rivers. Of these streams the Ohio is navigable for river steamers at nearly all stages of water. The same may be said of the Kanawha to a point near the Kanawha Falls, while the Big Sandy, the Guyandotte, and the Monongahela are navigable for flat boats for long distances, and these, as well as numerous other streams, are largely used for the floating of lumber. All the streams of the State, and especially the smaller ones, have a rapid fall, but their enormous water-power has as yet been utilized only to a trifling extent. Climate. The climate is nowhere severe, although, owing to the range in elevation within the State, there is a considerable range in tem perature. The mean annual temperature ranges from 54 to 55 F., being highest in the neighbourhood of the Ohio, in the western part of the State, and lowest upon the high mountains in the eastern and north-eastern portion. The maximum is rarely above 95 in any portion of the State, while the minimum occasionally reaches 10 in the more mountainous section. The rainfall may be given broadly at between 40 and 50 inches annually. It also varies with the elevation, being less in the lower portions and greatest upon the high mountains. Fauna. The fauna of the State is that common to the whole southern Appalachian region. Much of the area being as yet in a state of nature, deer of the white-tailed species are still abundant, and black bear are not unfrequently met with in the more rugged and remote portions. Wild turkeys are still found iu some localities, and the mountains have long been a popular resort for hunters, while the streams, abounding in trout, ali ord an equally attractive Held for the angler. Timber. The timber resources of the State are enormous, and a small pro portion of its area, amounting to only about 25 per cent. , has been cleared. The remainder is covered with virgin forest. This consists mainly of broad-leafed trees of the most valuable sorts for lumber, such as chestnut, black walnut, cherry, ash, poplar, hickory, locust, maple, oak, &c. Considerable areas of white pine are found in the highest portions of the plateau, being practically the only original forests of this wood left in the United States. Besides these there are considerable quantities of yellow pine, hemlock, spruce, and cedar scattered through the State. Minerals. Viewed broadly, the geological structure of Vest Virginia is extremely simple. Practically the entire State is overlaid by nearly horizontal beds of the Carboniferous formation. The coal of West Virginia forms its principal mineral wealth. It is estimated that of its entire area not less than 16,000 square miles are underlaid by workable beds of coal. The llcporl of the United States Geo logical Survey upon mineral resources defines the general boundaries of the coal fields of the State as follows : " The eastern boundary begins at the south on the mountain range just east of the Bluestone River, and proceeds east to Little Sewell Mountain ;..... thence with the common boundary of Nicholas and Greenbrier and of Webster and Focahontas counties to Rich Mountain in Randolph county; following this last-named ridge to Laurel Mountain, the dividing line between Upshur county on the west and Randolph and Barbour counties on the east, and thence with the Briery Mountain into Preston county, and soon to the Pennsylvania State line." All the area to the west of this line is underlain by coal. To the east of it there are small outlying patches, as in Greenbrier, Meadow Mountain, and possibly in Pocahontas, Tucker, Grant, and Mineral counties, but these are unimportant as compared with the vast areas in the west. In the gorge of every large stream flowing through this area are seen outcropping beds of coal, easily acces sible to the miner, and requiring only facilities of transportation to render the mineral of commercial value. In the matter of coal production the State is rapidly acquiring prominence. From a production in 1873 of 600,000 tons, it reached in 1886 a production of over 4,000,000 tons, being exceeded by only four of the States, viz., Pennsylvania, Illinois, Ohio, and Iowa. The production is limited only by the demand, as the supply is almost inexhaustible. The coals of the State are of every variety except anthracite, and are noted for their purity for coking, steam, and gas purposes and for domestic fuel. Iron ore is abundant in various portions of the State, but is worked only to a comparatively limited extent. Salt springs are found in the valley of the Kanawha and in that Mineral of the Ohio, and there are extensive evaporating works in both these springs, localities. The production, however, has been retarded by the competition of those in Michigan, owing to the greater cheapness of fuel and better facilities for transportation in the latter locality. The production of salt in West Virginia iu 1886 amounted to 250,000 barrels. West Virginia contains numerous valuable mineral springs, among the best known of which are the Greeubrier White Sulphur springs iu Greenbrier county, Capon springs in Hampshire count} , Iron dale springs in Preston county, and Red Sulphur springs and Salt Sulphur springs both in Monroe county. These are well-known and popular summer resorts iu the mountains, and the waters from them are shipped to all parts of the United States. While the entire State may be said to be either mountainous or Agricul- hilly, it contains a large extent of arable land. Nearly all of the ture. . lower hill country can be cultivated, while in the mountainous region there are numerous broad valleys of excellent soil, and everywhere the hill and mountain sides can be cultivated if the slope is not excessively steep. The tenth census (1880) reported an area of 10,193,779 acres of land in farms, of which 3,792,327 acres, or about one-fourth the area of the State, was improved land, this being mainly iu the lower and less mountainous portion. The average size of farms was 163 acres, showing as compared with the average 10 years earlier, viz., 214 acres, a decided decrease. The value of farms and farming implements was very nearly 136,000,000. The numbers of live stock upon farms, as distinguished from animals owned for business purposes in cities, consisted in January 1888 of 138,231 horses, 6475 mules, 474,933 sheep, 432,778 hogs, 171,273 milch cows, and 780,892 other cattle, showing that the live-stock interests of the State are very large. The estimated value of all farm products sold, consumed, or on hand, as returned in 1880, was 19,360,049. The principal agricultural products are wheat, Indian corn, hay, tobacco, oats, and garden vegetables. The cereal products for 1887 consisted of 12,516,^000 bushels of corn, 2,840,000 of wheat, and 2,531,000 of oats. The manufactures, which are not extensive, are concentrated Manufac- mainly at Wheeling, the largest city, on the Ohio, in the northern tures. part of the State ; they consist mainly of manufactures of iron and steel, glass, flouring and grist mill products, lumber, and leather. There were in 1880 2375 manufacturing establishments, employ ing a capital of $13,883,390 and 14,351 persons. The value of manufactured products was 22,867,126. There are 1200 miles of completed railroads, with several Railways, branches and one trunk line in process of construction. The Baltimore and Ohio Railroad traverses the State from Parkersburg and Bellaire on the Ohio, the two branches meeting at Graf ton, and running thence eastward to Washington, Baltimore, and New York. The Newport News and Mississippi Valley Railroad runs across the State from the mouth of the Big Sandy on the west to the Alleghanies near White Sulphur springs, and thence extends to Richmond and Newport News. The Ohio River line runs from AVheeling to Huntington on the Ohio. The West Virginia Central extends from Piedmont on the Baltimore and Ohio line to a point in Randolph county, and is now in process of construc tion south-westward to intersect the Newport News and Mississippi Valley line. The Clarksburg and Weston, intersecting the Balti more and Ohio at Clarksburg, extends to Westou in Lewis county, and this has two branches, one to Glenville in Gilmer county, and the other to Buckhaunon in Upshur county. The Grafton and Greenbrier Railroad, intersecting the Baltimore and Ohio at Grafton, extends up the Valley river to Belingtoii in Barbour county. The Norfolk and Western Railroad, one of the main trunk lines of the

Atlantic States, has a part of its lines in the southern portion of