Page:Encyclopædia Britannica, Ninth Edition, v. 14.djvu/55

 K E N T U K Y 43 to be found in the Ohio valley. In descending order are beds of white sand and clay and shales of the Eocene (Tertiary), only slightly exposed in the extreme western part of the State, where the streams have cut deepest. Nowhere in the State have evi dences of glacial action been found. Over the uplifted Blue Grass region are often thick deposits of what has been called drift material ; but such deposits are composed altogether of silicified remains from the several formations above the Lower Silurian, and the evidences are conclusive that they are the remains of rocks decomposed in situ. Minerals. No precious metals have been discovered in Kentucky. The amount of coal hitherto mined has not been as large as the quantity and quality in the State would justify, but the increased facilities of transport have stimulated production, and the out put will increase from year to year. In 1870 the amount mined was 150,582 tons, and in 1880 1,050,095 tons, a larger percentage of increase than in any other State in the Union. Iron ores of good quality abound in various parts of the State. In Bath county is a large deposit of Clinton ore similar to the red fossil ore occurring in this formation from New York to Alabama. The same ore pro bably is iu position along the western base of Pine Mountain. Along the south-eastern border of the State it extends for many miles in Tennessee and Virginia with a thickness of from 18 inches to 7 feet, where the very near proximity to the excellent coking coal of Kentucky renders it of peculiar value in determining the future development of that portion of the State. In the Cumber land valley of western Kentucky a high grade limonite is abundant in the subcarboniferous limestone, and in eastern Kentucky a superior iron-ore rests upon the top of the St Louis group of this formation. Excellent carbonates and limonites abound in the eastern Coal-measures, and have been mined extensively in the north-eastern part of the State. In the Lower Coal-measures of western Kentucky are a number of iron-ore strata ranging in thick ness from a few inches to 5 feet. Galena associated with sulphate of baryta occurs in veins in the lower members of the blue limestone of central Kentucky, and also in the subcarboniferous strata in the lower Cumberland valley, where it is associated with valuable deposits of fluor-spar. Petroleum has been produced from wells in Barren county for a number of years. The oil is here derived from the Devonian black shale. Heavy lubricating oil is produced from the same forma tion in Wayne county. There is a wide area in the State where petroleum may be obtained by boring. Salt-brine is obtained from wells in the eastern coal-field, and in the subcarboniferous limestone of western Kentucky. Fire and pottery clays abound in the Coal-measures ; potteiy clays occur in the surface deposits in valleys of central Kentucky, and in the flat lands where the soil is derived from the decomposi tion of the Devonian black shale, and the argillaceous shales of the &quot;Waverly group. In the Tertiary shales, below the gravel bed west of the Tennessee river, are pottery-clays, and fire-clays occur in great abundance. Building stones of great variety abound in almost every sec tion. Forests. Probably two-thirds of the State is yet covered by virgin forests of valuable timbers. At the time of the settlement of the State by the whites it was covered by forests excepting a por tion of the south-western part known as the &quot;Barrens,&quot; which was a prairie covered by tall grass known as &quot;barren-grass.&quot; Here only the roots of certain hardy trees had withstood the annual burning of the dry grasses ; from these roots &quot;sprouts&quot; grew every year, only to be destroyed by fire, and the roots or base grew hori zontally under the soil. When the country was settled and the fires checked, the saplings springing from these roots soon grew into trees, and the region was speedily covered with a dense growth, the prevailing timbers being black-jack oak (Qucrcus nigra), post oak (Q. oblusiloba), and black oak (Q. tinctoria). The outline of these barrens was almost identical with the outline of the cavernous group of the subcarboniferous limestone. On the lower limestones and shales of the Subcarboniferous, the most valuable timbers remaining are yellow poplar (Liriodcndron tulipifcra), white oak (Q. alba], the hickories, and some black walnut (Juylans nigra). The several divisions of the Lower Silurian are characterized by a variation in the forest growth. On the lower rocks the most characteristic timbers are over-cup oak (Q. macrocarpa), white oak, shell bark hickory (Carya alba), black walnut, and black ash (Fraxinus sambucifoHa). The pre valent timbers -on the best soils of this region are sugar maple (Acer saccho.rinum], blue ash (Fr. quadrangulata), black wal nut, pig-nut hickory (C. glabra), hackberry (Ccltis occidentalis), mulberry (Mortis rubra), buckeye (sEsculus glabra), honey-locust (Gleditschia triacanthos), box elder (Ncgundo aceroidcs), and Ken tucky coffee-tree (Gymnocladus). On the soils derived from the silicious member of the Cincinnati group, the prevalent timbers are yellow poplar, beech, white and red oak, and hickory. White oak is the prevailing timber on the upper portion. On the Upper Silurian lands the timbers are mainly white oak, of superior quality, sweet gum (Liquidambar styraciflua), and water maple (A. rubrum). The growth on the corniferous limestone is very similar to that .on the best soils of the blue limestone, with the exception that beeches and yellow poplars are more numerous. On the black shale of the Devonian are over-cup oak, black oak, sweet gum, beech, and elm, and, in places where the soil is well drained, yellow poplar, wild cherry, and black walnut. The growth on the flat lauds of the Waverly is elm, beech, sweet gum, and white oak ; on the uplands chestnut, oak (Q. Prinus), and small hickories, and on the thin uplands the above timbers and yellow pine (Pinus mitis). The great stores of valuable timbers are in the Coal-measures. In eastern Kentucky there is an area of 10,000 square miles of virgin forests of white oak, ash, hickory, wild cherry, and other valuable timbers. On the outcrop of the conglomerate sandstone, on the western edge of the coal-field, and on the top and eastern slope of Pine Mountain, and the western slope of Cumber land Mountain, the prevailing timbers are chestnut, oak, and yellow pine, and hemlock (Abies canadcnsis) where the streams have cut deep in the rocks, with an undergrowth of rhododendrons and kalmias, and on the drier slopes azaleas. The above is also the growth where the conglomerate is thick on the eastern outcrop of the western coal-field. In the valley of Red river, on the con glomerate series, there is an area of about 40,000 acres where the prevalent timber is white pine (P. strobus). There are fine forests remaining on the Quaternary west of the Tennessee river. On the lowlands are forests of large cypress (Taxodium distychum). In this region the Catalpa speciosa and pecan (Carya olivseformis) abound, and cotton-wood (Populus angulata) on the banks of streams. Many valuable timbers, in addition to the above, are to be had in various parts of the State. Owing to the large demands for timber on the treeless prairies, and the rapid exhaustion of tim bers in the States north of the Ohio river, the extensive forests of Kentucky have an especial value. Soils and Agriculture. With, the exception of the area west of the Tennessee river, all the soils are derived from the decomposi tion of rocks in situ. The soils over an area of about 22,000 square miles are derived from the decomposition of limestones of various geological horizons. The soils of the Blue Grass region, derived from the decomposition of phosphatic limestone and shales, and the soils of a portion of the subcarboniferous limestone groups, are of great fertility, and are easily restored by a judicious rotation with clover and grasses. The State was peopled almost exclusively with agriculturists from Virginia and Maryland, and agriculture has remained the favourite occupation. Out of a total population of 1,321,011 in 1870 only 44,197 were engaged in manufacturing, mechanical, and mining industries. The peculiarity of Kentucky agriculture is its great diversity. It will be seen from the United States census that in each decade from 1810 to the present time the State ranked first in the production of one or more staple articles. Thus in 1840, though sixth in rank of population, it was the first in the produc tion of wheat and hemp, and the second in the production of swine, Indian corn, and tobacco. In 1850 it ranked first in the produc tion of Indian corn, flax, and hemp, and second in swine, mules, and tobacco. In 1870, when it was the eighth State in population, and the eighth in the total value of agricultural products (notwithstand ing over one-half the area of the State was in virgin forests), it ranked first in the production of hemp and tobacco, sixth in Indian corn, and eighth in wheat. In 1880 it ranked first in the production of hemp and tobacco, and seventh in Indian corn and rye. The decline in the relative position in the production of Indian corn and wheat was not caused by a decreased production, but by the increased production of those cereals by States in the west where these are almost the exclusive crops. In Kentucky a more diversi fied agriculture is found to be more profitable. Especial care has been devoted to the importation and improvement of domestic animals, until the State has become the great centre for fine stock of all kinds. In arriving at this pre-eminence, the breeders have doubtless been assisted by the climate, the water, and the perfection of pasturage. The blue grass (Poa pratensis) attains perfection in this region, making a beautiful turf ; it grows in the shade of woodlands, and affords an excellent winter pasture. Virginia, in early times, imported choice horses from England (when the breeders there paid attention to endurance). The Kentucky breeders have kept those strains pure, and have from time to time added by importations from England, until a race horse having endurance and speed is the result. Probably over 75 per cent, of the winnings on the American turf is by Kentucky-bred horses. The attention of many of the Kentucky stock breeders of late years has been turned to breeding trotting horses, with very marked results. The production of the very fleet trotting horses of Kentucky is the result of intelligent breeding, under favourable conditions. Kentucky is the principal tobacco-growing State in the Union. In 1870, of the total of 262,735,371 Ib produced in the United States, Kentucky produced 105,305,869 ft; and in 1880, out of the total of 473,107,573 ft, Kentucky produced 171,121,134 ft. The ten prin cipal tobacco-growing counties are :