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 — John Shaqi
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
"The salt water is obtained by sinking a tight curb, or gum, at the
edge of the river, down about twenty feet, to the rock which underlies
the river, and then boring into the rock. At first the borings did not
exceed 200 feet in depth, but the upper strata of water being
exhausted, the wells were gradually deepened, the water of the lower
strata being generally stronger than the upper had ever been. Until
1842, none of the wells exceeded 6 or 700 feet in depth. Mr. Tompkins,
an enterprising salt-maker, was the first to extend his borings to a
thousand feet, or more. His experiment was attended with a most
unexpected result. He had somewhat exceeded a thousand feet, when he
struck a crevice in the rock, and forth gushed a powerful stream of
mingled gas and salt water. Generally, the salt water in the wells was
obtained in rock merely porous, and rose by hydrostatic pressure to the
level of the river. To obtain the strong water of the lower strata,
unmixed with the weak water above, it is the practice to insert a
copper tube into the hole, making it fit tightly below by means of
wrapping on the outside, and attaching the upper end to the pump, by
which the water is drawn up to the furnaces on the river bank.
"When Mr. Tompkins inserted his tube, the water gushed out so forcibly,
that instead of applying the pump, he only lengthened his tube above
the well. The stream followed it with undiminished velocity to his
water cistern, 60 feet above the level of the river.
"In the next place, he inserted the end of the spout from which the
water and gas flowed, into a large hogshead, making a hole in the
bottom to let out the water into the cistern. Thus the light gas was
caught in the upper part of the hogshead, and thence conducted by pipes
to the furnace, where it mingled with the blaze of the coal fire. It so
increased the heat as to make very little coal necessary; and if the
furnace were adapted to the economical use of this gaseous fuel, it
would evaporate all the water of the well, though the quantity is
sufficient to make five hundred bushels of salt per day. The same
gentleman has since obtained a second gas-well near the former, and in
all respects similar to it. Other proprietors of wells have also struck
gas-fountains by deep boring. In one of these wells the gas forces the
water up violently, but by fits, the gush continuing for some two or
three hours, and then ceasing for about the same length of time. In
another of these wells there has been very recently struck, a
gas-fountain that acts with such prodigious violence as to make the
tubing of the well in the usual way impossible; when the copper tube
was forced down through the rushing stream of brine and gas, it was
immediately flattened by the pressure; and the auger-hole must be
enlarged to admit a tube sufficiently strong and capacious to give vent
to the stream without being crushed. In another well, a mile and a half
Public-domain text, read in full here on John Shaqi.
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