Flint's Letters from America, 1818-1820Flint, James, active 19th century
History
Flint's Letters from America, 1818-1820
Flint, James, active 19th century
Ohio River Valley -- Description and travel; United States -- Description and travel
Amongst the business of the court, the trial of a man who had
stolen two horses excited much interest. On his being sentenced
to suffer thirty stripes, he was immediately led from the bar to
the whipping-post. Every twitch of the cowhide, (a weapon formerly
described,) drew a red line across his back. This was the second
infliction of the kind that had been sanctioned by {253} court in
the State, since my coming into it. I do not notice the infrequency
of punishments as wishing to occasion a belief that misdemeanours
are seldom committed. Indeed, were it not for the absolute impunity
obtained in most cases, we might soon see the partial development of a
new system of physiognomy, one not founded on the features of the face,
but on the striped lineaments of the back. Never, till now, did I so
much value the usage of Scotland, where the inhabitant, on removing
from one parish to another, carries with him the testimonial of the
church.
The surface of the land in the neighbourhood of Charlestown is
beautifully diversified, varying between gently undulated and steep of
broken ground. The soil is of the first rate quality, and covered with
luxuriant crops of Indian corn. The crops of wheat are what you would
call a second rate crop, and several fields of oats, which I saw, were
headed out, and were as bulky as any that I have seen in Mid-Lothian;
but, for a reason formerly stated, the grain cannot be expected to
arrive at fine quality. The banks of Fourteen-Mile-Creek, (which joins
the Ohio at the distance of fourteen miles above the falls,) are cliffs
of limestone that are overtopped by tall woods, and form, by their
windings, many romantic scenes, of which I can convey no adequate idea.
The stream is at present almost entirely dried up, but the extent of
its bed, and the marks of inundation by its margin, convince me that
its floods are nearly equal to those of the Clyde at Glasgow. Some
salt springs that percolate through the rocks in the bottom, have
been discovered during the present dry season: the existence of these
were first surmised by an ingenious gentleman, with whom I am well
acquainted. He proceeded by introducing a small tube into a {254} deep
and still part of the river, and drew water from the bottom that was
perceptibly saline. He has now some people engaged in boring, by which
means the discharge of water has been considerably augmented, and
has commenced evaporating on a small scale. This process is usually
performed by filling a number of iron kettles, of about three feet in
diameter, and six inches deep, with the water, and placing them on
loose stones, or over a trench that is dug in the ground for receiving
the fuel. Boring for salt water is a work that is occasionally
accompanied with a considerable degree of difficulty. Where the bore
communicates with a fresh water spring, on a higher level than the
saline one, a tube of tinned iron is let down to exclude the former.
Public-domain text, read in full here on John Shaqi.
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