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
Large boats ascend the rapids at the time of the spring floods, by
the aid of a cable made fast to a tree, or some other object
above, and taken in by the capstan. In 1821, the Maysville, a
steam-boat of about two hundred tons, was taken up, and had nearly
reached the head of the rapid, when the cable broke; and the boat
swinging round, was thrown against the rocks, in the bed of the
river, and placed in such a situation as to render hopeless all
attempts to get her off before the next annual rise of the water.
Arks and small barges descend, by the aid of skilful pilots, for
great part of the year. It is expected that the navigation of this
dangerous rapid will soon be rendered more convenient, by
canaling, which can be accomplished at a very inconsiderable {25}
expense. The direction of the Ohio, above and below the rapids, is
nearly from north-east to south-west, but where the stream passes
the rocky obstruction occasioning the fall, it is a little
deflected from its course, making a bend towards the west. Thus a
point is formed on the south-eastern side projecting from the
elevated bank, which, from its present position, would seem to
indicate that the bed of the river had changed its place, having
formerly traversed the point from north-east to south-west, in a
direct line. In times of high floods the water is, in part,
discharged through this old channel, and large boats are said to
have ascended by that route within a few years past.
On this point stands the small town of Shippingsport, at the foot
of the rapids.[034] The proposed canal will traverse the point in
the rear of this village. The obstacles to be encountered in
opening a canal at this place are but trifling. The soil is firm
and gravelly, being based on horizontal strata of compact
limestone, and fine argillaceous sandstone.[035]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account