The history of salt : $b with observations on its geographical distribution, geological formation, and medicinal and dietetic propertiesBoddy, Evan Marlett
History
The history of salt : $b with observations on its geographical distribution, geological formation, and medicinal and dietetic properties
Boddy, Evan Marlett
Salt; Salt -- History; Salt -- Physiological effect
Though the sea is so destructive an element, it is also an agent in the
reproduction of land. The rocks and sand washed away from one place
are conveyed by tides and currents far into the sea, and are deposited
in strata, and then, in course of time, form shoals and banks, which
subsequently become promontories and islands. Alluvial land has thus
been formed, and in a similar way have many of the stratified rocks
been deposited; and as animals and plants have been carried away and
imbedded in the deposits of rivers, or floods, so at some future
period, though countless ages may elapse during the process, will such
animals and plants be discovered deposited in these newer strata, just
as we find organic remains in the older rocks. The gradual deposition
of strata has been the work of an incalculable period of time, but the
process may be traced every day in the sections of marine estuaries
and lakes. Owing to this continual receding of the land in one part,
and elevation of land in another, there is an incessant change, from
which, though occupying many ages, and proceeding so slowly that it
would be unobservable were it not for accurate investigation, we may
easily conjecture that what is now land may at one time have been the
bed of the ocean, and where the sea now sweeps with overpowering fury,
there may once have been meadows and forests. The salt lakes, if not
originating from volcanic force, no doubt are the remains of the great
ocean, which, when it receded, left here and there, in what once were
luxuriant valleys, large reservoirs, indicating that in bygone ages it
had covered the land.
In Germany, Spain, Italy, Hungary, and Poland, there are extensive
mines of rock-salt, and also in various other parts of Europe.[36]
There are also large mountains wholly composed of this fossil salt,
two of which are in those provinces of Russia known as Astrakhan and
Orenburg; and in the Crimea salt is said to be daily accumulating in
the inland lakes. In Asiatic Russia there are extensive beds of salt,
near Lake Indur, in lat. 48° 30´, long. 69°. The Caspian Sea, called
by the Turks “Cozgoun Denghizi,” “the sea of crows and cormorants,” is
“a great salt-water lake,” according to Dr. William Smith, though Dr.
Lemprière says that “its waters are sweet.”
Public-domain text, read in full here on John Shaqi.
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