James's Account of S. H. Long's Expedition, 1819-1820, part 1James, Edwin
History
James's Account of S. H. Long's Expedition, 1819-1820, part 1
James, Edwin
Indians of North America; Rocky Mountains; United States -- Discovery and exploration; West (U.S.) -- Description and travel
The sandstone, which is the rock of most common occurrence about
the rapids, very closely resembles that of Pittsburgh. It is
commonly of a compact texture, having an argillaceous cement, with
a laminated structure. At Shippingsport, and at Clarksville,[036]
in Indiana, it is succeeded by bituminous clay-slate. While we
were waiting at the rapids, several of the party made an excursion
to visit the boiling spring, at the foot of the Silver Creek
hills, in Indiana, at a little distance from New Albany.[037] This
spring is small, discharging no water above the surface of the
ground. It is an artificial excavation in the clayey bank of a
small stream, called Fountain Creek. It is filled to the level of
the water in the creek, the spring itself evidently discharging
very little, if any water. That which fills the basin is turbid,
being kept in constant agitation by the bubbles of inflammable air
which rise through it. The {26} smell of sulphuretted hydrogen is
perceptible at considerable distance about the spring; and a piece
of silver, held near the surface of the water, was quickly
tarnished. The Silver Creek hills are of argillaceous sandstone,
and secondary clay-slate; and this spring seems to be placed near
the meeting of the two strata.
In the bed of the Ohio, opposite Shippingsport, is a tabular mass
of rocks, visible above water for great part of the year, and
called Corn Island.[038] On the highest parts of this, are
remaining some small portions of the limestone stratum, which
appears in many places to have been worn through, and removed by
the river. Five or six acres of the surface of this island are of
the smooth compact argillaceous sandrock before mentioned, lying
horizontally, and divided into squares and parallelograms by the
natural fissures. These fissures contain some soil which supports,
in the summer, a dense growth of herbaceous plants. Among these,
we noticed the hypericum sphæcrocarpum of Michaux, (apparently not
the plant mentioned by Nuttall, under that name, which has been
noticed near Philadelphia, by Collins and others, but without
doubt that originally described by Michaux). Two species of
andropogon, the panicum virgatum, solanum nigrum, polygala
verticillata, leplanthus gramineus, chenopodium botrys, &c. The
lower part of the island is covered with loose sand; bearing some
small cotton-wood and willow trees.
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