A Guide to the Virginia Springs: Giving, in addition to the routes and distances, a description of the springs and also of the natural curiosities of the stateMoorman, J. J. (John Jennings)
Science
A Guide to the Virginia Springs: Giving, in addition to the routes and distances, a description of the springs and also of the natural curiosities of the state
Moorman, J. J. (John Jennings)
Health resorts -- Virginia; Springs -- Virginia; Virginia -- Description and travel
Visiters to the Virginia Springs from the south or west by the Ohio
River, generally leave the river at Guyandotte, taking the stage to
Charleston, 48 miles. This beautiful town is in the rich valley of the
Kanawha, immediately on the banks of the river. About five miles from
this place are the Salines, where are to be seen the Gas-Wells. The
following interesting account of these is from the Lexington Gazette of
1843:
"These wonderful wells have been so lately discovered, that as yet only
a brief and imperfect notice of them has appeared in the newspapers.
But they are a phenomenon so very curious and interesting, that a more
complete description will doubtless be acceptable to the public.
"They are, in fact, a new thing under the sun; for in all the history
of the world, it does not appear that a fountain of strong brine was
ever before known to be mingled with a fountain of inflammable gas,
sufficient to pump it out in a constant stream, and then by its
combustion, to evaporate the whole into salt of the best quality.
"We shall introduce our account of these wells by some remarks on the
geological structure of the country at the Kanawha Salt Works, and on
the manner in which the salt water is obtained.
"The country is mountainous, and the low grounds along the river are
altogether alluvial, the whole space of a mile in width, having been at
some time the bed of the river. The rocks are chiefly sandstone of
various qualities, lying in beds, or strata, from two inches to several
feet in thickness. These strata are nearly horizontal, but dipping a
little, as in other parts of the country, towards the northwest. At the
Salt Works they have somehow been heaved up into a swell above the line
of general direction, so as to raise the deep strata nigher to the
surface, and thus to bring those in which the salt water is found
within striking distance.
"Among the sand-rocks are found layers of slate and coal; this latter
being also, by the same upheaving, made more conveniently accessible
than in most other parts of the country.
Public-domain text, read in full here on John Shaqi.
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