The drainage of Illinois is far better than its low elevation and
comparatively level surface would suggest. There are more than 275
streams in the state, grouped in two river systems, one having the
Mississippi, which receives three-fourths of the waters of Illinois,
as outlet, the other being tributary to the Wabash or Ohio rivers. The
most important river is the Illinois, which, formed by the junction of
the Des Plaines and the Kankakee, in the N.E. part of Grundy county,
crosses the N. central and W. portions of the state, draining 24,726
sq. m. At some points, notably at Lake Peoria, it broadens into vast
expanses resembling lakes. The Kaskaskia, in the S., notable for its
variations in volume, and the Rock, in the N., are the other important
rivers emptying into the Mississippi; the Embarrass and Little Wabash,
the Saline and Cache in the E., are the important tributaries of the
Wabash and Ohio rivers. The Chicago river, a short stream 1 m. long,
formed by the union of its N. and S. branches, naturally flowed into
Lake Michigan, but by the construction of the Chicago Drainage Canal
its waters were turned in 1900 so that they ultimately flow into the
Mississippi.
The soil of Illinois is remarkable for its fertility. The surface
soils are composed of drift deposits, varying from 10 to 200 ft. in
depth; they are often overlaid with a black loam 10 to 15 in. deep,
and in a large portion of the state there is a subsoil of yellow clay.
The soil of the prairies is darker and coarser than that of the
forests, but all differences disappear with cultivation. The soil of
the river valleys is alluvial and especially fertile, the "American
Bottom," extending along the Mississippi from Alton to Chester, having
been in cultivation for more than 150 years. Along the river bluffs
there is a silicious deposit called loess, which is well suited to the
cultivation of fruits and vegetables. In general the N. part of the
state is especially suited to the cultivation of hay, the N. and
central parts to Indian corn, the E. to oats, and the S.W. to wheat.
Public-domain text, read in full here on John Shaqi.
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