Buffon's Natural History, Volume 01 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Mineral, &c. &cBuffon, Georges Louis Leclerc, comte de
History
Buffon's Natural History, Volume 01 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Mineral, &c. &c
Buffon, Georges Louis Leclerc, comte de
Natural history
All these rivers carry to the sea a great quantity of mineral and saline
particles, which they have washed from the different soils through
which they have passed. The particles of salt, which are easily
dissolved, are conveyed to the sea by the water. Some philosophers, and
among the rest Halley, have pretended that the saltness of the sea
proceeded only from the salts of the earth, which the rivers transport
therein. Others assert, that the saltness of the sea is as ancient as
the sea itself, and that this salt was created that the waters might not
corrupt; but we may justly suppose that the sea is preserved from
corruption by the agitations produced by the winds and tides, as much as
by the salt it contains; for when put in a barrel it corrupts in a few
days; and Boyle relates, that a mariner, who was becalmed for 13 days,
found, at the end of that time, the water so infected, that if the calm
had not ceased, the greatest part of his people would have perished. The
water of the sea is also mixed with a bituminous oil, which gives it a
disagreeable taste, and renders it very unhealthful. The quantity of
salt contained in sea water is about a fortieth part, and is nearly
equally saline throughout, at top as well as bottom, under the line, and
at the Cape of Good Hope; although there are several places, as off the
Mosambique Coast, where it is salter than elsewhere.[317:A] It is also
asserted not to be so saline under the Arctic Circle, which may proceed
from the amazing quantities of snow, and the great rivers which fall
into those seas, and because the heat of the sun produces but little
evaporation in hot climates.
Be this as it may, I conceive that the saltness of the sea is not only
caused by the banks of salt at the bottom of the sea, and along the
coasts, but also by the salts of the earth, which the rivers continually
convey therein; and that Halley had some reason to presume that in the
beginning of the world the sea had but little or no saltness; that it is
become so by degrees, and in proportion as the rivers have brought salts
therein; that this saltness is every day increasing, and that
consequently, by computing the whole quantity of salt brought by all the
rivers, we might attain the knowledge of the age of the world by the
degrees of the saltness of the sea.
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