James's Account of S. H. Long's Expedition, 1819-1820, part 4James, Edwin
History
James's Account of S. H. Long's Expedition, 1819-1820, part 4
James, Edwin
Indians of North America; Rocky Mountains; United States -- Discovery and exploration; West (U.S.) -- Description and travel
The most extensive tract of valley country east of the Mississippi is
that situated within the bluffs of this river, usually denominated the
American Bottom, extending from the mouth of the Ocoa, or Kaskaskias
river, northwardly to that of the Missouri. This spacious bottom,
although at present elevated much above the range of the highest
freshets, is nevertheless alluvial. Its length along the Mississippi
is about eighty, and its average breadth about four miles. It is
generally destitute of a timber growth, except along the margin of
the river, upon which there is a skirt of woodland extending almost
from one end of the tract to the other. The alluvion of the American
Bottom is composed of the rich mud brought down by the turbid Missouri,
united with an abundance of vegetable matter yielded by the waters of
the upper Mississippi, which also characterizes the bottoms of this
extensive river from the Missouri downward to its mouth. Upon this
bottom are situated the town of Kaskaskias, the villages of Prairie de
Rocher, Harrison, Prairie de Pont, Cahokia and Illinois, together with
many other settlements.
On the same side of the river another large tract of valley land,
called the Mississippi Bottom, commences a few miles below the mouth
of the river Kaskaskias, and extends downwards along the Mississippi,
between fifty and sixty miles, having an average width of about
three miles. This tract, in regard {207} to soil and aspect, is of
a character similar to that of the American Bottom, except that the
former is more plentifully stocked with timber.
Besides these, there are numerous other bottoms on the Mississippi,
within the limits prescribed for this report, all of which are composed
of a rich alluvion. Those in particular situated below the confluence
of the Mississippi and Missouri are possessed of a soil exceedingly
luxuriant, being composed, as before observed, of the rich and
fertilizing mud deposited from the water of the Missouri. Most of them
are covered with deep and heavy forests of timber, accompanied with a
luxuriant undergrowth of vines, shrubs, grass and other herbage.
The bottoms of the Wabash, Kaskaskias, Illinois, and Rock rivers, are
also made up of a rich alluvion of sand and loam, containing a large
proportion of vegetable mould. Their surfaces, like those of the
Mississippi bottoms, are generally flat, exhibiting tabular elevations
or benches, formed by the washing of their rivers at different periods.
Large tracts of prairie land are to be met with upon them; but for the
most part the proportion of woodland is amply sufficient to supply the
adjacent country with timber and fuel.
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