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
We have also seen that the base of all mineral waters is the chloride
of sodium, and that their ingredients are collected and dissolved as
they ascend to the surface; therefore they may probably both have the
same origin as the sea, as regards the chloride of sodium, which they
both hold in solution. We can account for their other characteristics
by the wide expansiveness of the sea, which is perpetually absorbing
and emitting vapours, and by the several strata through which the
mineral waters pass. There may be, though there is nothing that we can
advance as corroborative, a subterranean communication existing between
them, which would imply a common origin, the differences arising from
the physical surroundings, atmospheric influences, and the absorption
of soluble salts from the several strata.
What is the origin of salt lakes and salt marshes? This is, to a
certain extent, more easily explained. One theory as to the origin of
salt lakes (we naturally include inland seas, such as the Caspian and
the Aral) is the overflow and subsequent retirement of the sea-water,
their sites having been originally the bed of the ocean when it receded
to its present limits, leaving in its course depressions of land,
volumes of water of various depths, elevations, and extent of surface,
according to their deepness, altitude, or angles of declivity.[47]
Other ingenious hypotheses have been broached, which, I need hardly
say, are not worth considering, as they are entirely visionary. In
the case of isolated salt lakes, the above theory is not applicable;
and geologists tell us that they are doubtless the result of volcanic
agency, but at what period of time it is impossible to estimate, for
the density of the water found in them is not equable, and neither is
their specific gravity the same as that of sea-water, nor are there any
remains of marine organisms; and as their depth is variable, they are
not confined to any particular strata.
I have hinted previously that these isolated salt lakes are (if I may
venture to designate them as such) geological abortions. Had the power
which forced them into their present situation been accompanied by
that agency which has raised such huge masses as those near Cordova,
in Spain, and by the Dead Sea, and which probably brought about their
present crystalline form, others by reason of some unexplainable and
gradual transition, by chemical means, or decrease of temperature,
which naturally would occur the nearer it approached the earth’s
surface, these lakes might have developed into beds or mountains of
salt.
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