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
with the apparent solemnity of the great numbers of people,
assembled for religious worship, made considerable impression on
our feelings.
On the 9th May, we arrived at Cincinnati.[021] Since our departure
from Pittsburgh, Dr. Baldwin's illness had increased, and he had
now become so unwell, that some delay appeared necessary on his
account; as we wished also for an opportunity of making some
repairs and alterations in the machinery of the boat, it was
resolved to remain at Cincinnati some days. Dr. Baldwin was
accordingly moved on shore, to the house of Mr. Glen, and Dr.
Drake was requested to attend him. Cincinnati is the largest town
on the Ohio. It is on the north bank of the river, and the ground
on which it stands is elevated, rising gradually from the water's
edge.[022]
Compact limestone appears here, in the bed of the Ohio, and
extends some distance in all directions. This limestone has been
used in paving the streets, for which purpose its tabular
fragments are placed on edge, as bricks are sometimes used in
flagging. The formation of limestone, to which this rock belongs,
is one of great extent, occupying a large part of the country from
the shores of Lake Erie, to the southern boundary of the state of
Tennessee.[023] It appears, however, to be occasionally
interrupted, or overlaid by fields of sandstone. It abounds in
casts, and {20} impressions of marine animals. An orthocerite, in
the museum of the college[024] at Cincinnati, measures near three
feet in length. Very large specimens of what has been considered
lignite, have also been discovered and parts of them deposited in
that collection. We saw here no remains of ammonites. Numerous
other species appear to be similar to those found in the limestone
of the Catskill and Hellebergh mountains.
The soil, which overlays the limestone of Cincinnati, is a deep
argillaceous loam, intermixed with much animal and vegetable
matter. Vegetation is here luxuriant; and many plants unknown
eastward of the Alleghany mountains, were constantly presenting
themselves to our notice. Two species of æsculus are common. One
of these has a nut as large as that of the Æ. hippocastanum, of
the Mediterranean, the common horse-chesnut of the gardens.
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