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See also:OHIO See also:RIVER , the See also:principal eastern tributary of the See also:Mississippi river, U.S.A. It is formed by the confluence of the See also:Allegheny and See also:Monongahela See also:rivers at See also:Pittsburg, See also:Pennsylvania, and flows N.W. nearly to the W. border of Pennsylvania, S.S.W. between Ohio and See also:West See also:Virginia, W. by N. between Ohio and See also:Kentucky, and W.S.W. between See also:Indiana and See also:Illinois on the N. and Kentucky on the S. It is the largest of all the tributaries of the Mississippi in respect to the amount of See also:water discharged (an See also:average of about r58,000 cub. ft. per sec.), is first in importance as a See also:highway of See also:commerce, and in length (967 m.) as well as in the See also:area of its drainage See also:basin (approximately 210,000 sq. m.) it is exceeded only by the See also:Missouri. The slope of the river at See also:low water ranges from 1 ft. or more per mile in the upper See also:section to about o•75 ft. per mile in the See also:middle section and o•29 ft. per mile in the See also:lower section, and the See also:total fall is approximately 500 ft. Nearly two-thirds of the See also:bed is occupied by 187 pools, in which the fall is very See also:gentle; and the greater See also:part of the descent is made over intervening bars, which are usually composed of See also:sand or See also:gravel but occasionally of hard See also:pan or See also:rock. The greatest falls are at See also:Louisville, where the river within a distance of 2.25 M. descends 23.9 ft. over an irregular See also:mass of See also:limestone. The rock See also:floor of the valley is usually 30 to 50 ft. below low water level, and when it comes to the See also:surface, as it occasionally does, it extends at this height only part way across the valley. In the upper part of the river the bed contains much coarse gravel and numerous boulders, but lower down a sand bed prevails. The See also:ordinary width of the upper See also:half of the river is quite See also:uniform, from 1200 to 1500 ft., but it widens in the See also:pool above Louisville, contracts immediately below the Falls, and then gradually widens again until it reaches a maximum width of more than a mile about 20 M. from its mouth. Islands are numerous and vary in See also:size from an See also:acre or less to 5000 acres; above Louisville there are fifty or more, and below it about See also:thirty. Many of them are cultivated. Besides its See also:parent streams, the Allegheny and the Monongahela, the Ohio has numerous large branches. On the N. it receives the See also:waters of the Muskingum, Scioto, See also:Miami and See also:Wabash rivers, and on the S. those of the Kanawha, Big Sandy, Licking, Kentucky, See also:Green, See also:Cumberland and See also:Tennessee rivers.
The drainage basin of the Ohio, in which the See also:annual rainfall averages about 43 in., is, especially in the S. part of the river, of the " See also:quick-spilling " See also:kind, and as the See also:swift See also:mountain streams in that section are filled in See also:February or See also: See also:Cincinnati, Louisville and Pittsburg on its banks were extensively engaged in See also:building these vessels. The river was dotted with floating shops—drygoods boats fitted with counters, boats containing a tinner's See also:establishment, a blacksmith's See also:shop, a factory, or a lottery See also:office. Until the See also:Erie See also:Canal was opened in 1825 the Ohio river was the See also:chief commercial highway between the See also:East and the West. It was connected with See also:Lake Erie in 1832 by the Ohio & Erie Canal from See also:Portsmouth to See also:Cleveland, and in 1845 by the Miami & Erie Canal from Cincinnati to See also:Toledo. In the natural See also:state of the river navigation was usually almost wholly suspended during low water from See also:July to See also:November, and it was dangerous at all times on See also:account of the numerous snags. The Federal See also:government in 1827 undertook to remove the snags and to increase the See also:depth of water on the bars by the construction of contraction See also:works, such as dikes and wing dams, and appropriations for these purposes as well as for dredging were continued until 1844 and resumed in 1866; but as the channel obtained was less than 3 ft. in 187o, locks with movable dams—that is, dams that can be thrown down on the approach of a See also:flood—were then advocated, and five years later See also:Congress made an See also:appropriation for constructing such a See also:dam, the See also:Davis See also:Island Dam immediately below Pittsburg, as an experiment. This was opened in 1885 and was a recognized success; and in 1895 the Ohio Valley Improvement Association was organized in an effort to have the system extended. At first the association asked only for a channel 6 ft. in depth; and between 1896 and 1905 Congress authorized the necessary surveys and made appropriations for thirty-six locks and dams from the Davis Island Dam to the mouth of the Great Miami river. As the association then urged that the channel be made 9 ft. in depth Congress authorized the secretary of war to appoint a See also:board of See also:engineers which should make a thorough examination and See also:report on the See also:comparative merits of a channel 9 ft. in depth, and one 6 ft. in depth. The board reported in 1908 in favour of a 9-ft. channel and stated that fifty-four locks and dams would be necessary for such a channel throughout the course of the river, and Congress adopted this project. At the Falls is the Louisville & See also:Portland Canal, originally built by a private See also:corporation, with the United States as one of the stockholders, and opened in 183o, with a width of 5o ft., a length of 200 ft., and three locks, each with a lift of about 8; ft. In 186o-1872 the width was increased to 90 ft. and the three old locks were replaced by two new ones. The United States gradually increased its holdings of stock until in 1855 it became owner of all but five shares; it assumed the management of the canal in 1874, abolished tolls in 188o, and thereafter improved it in many respects. Sixty-eight locks and dams have been constructed on the principal tributaries, and the Allegheny. Monongahela, Cumberland, Tennessee, Muskingum, Kanawha, Little Kanawha, Big Sandy, Wabash, and Green now afford a total of about 96o m. of slack-water navigation. See the Board of Engineers' Report of Examination of Ohio River with a view to obtaining Channel Depths of 6 and 9 ft. respectively (Washington, 1908) ; A. B. Hulbert, Waterways of Westward Expansion (Cleveland, 1903) and The Ohio River, a Course of See also:Empire (New See also:York, 1906); also R. G. Thwaites, Afloat on the Ohio (New York, 1900). Additional information and CommentsThere are no comments yet for this article.
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