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
The waters which run on the surface of the earth, and support its
verdure and fertility, are not perhaps one half of those which the
vapours produce; for there are many veins of water which sink to great
depths in the internal part of the earth. In some places we are certain
to meet with water by digging; in others, not any can be found. In
almost all vallies and low grounds water is certain to be met with at
moderate depths; but, on the contrary, in all high places it cannot be
extracted from the bowels of the earth, but must be collected from the
heavens. There are countries of great extent where a spring cannot be
found, and where all the water which supplies the inhabitants and
animals with drink is contained in pools and cisterns. In the east,
especially in Arabia, Egypt, and Persia, wells are extremely scarce, and
the people have been obliged to make reservoirs of a considerable extent
to collect the waters as it falls from the heavens. These works,
projected and executed from public necessity, are the most beautiful and
magnificent monuments of the eastern nations; some of the reservoirs
occupy a space of two square miles, and serve to fertilize whole
provinces, by means of baths and small rivulets that let it out on every
side. But in low countries, where the greatest rivers flow, we cannot
dig far from the surface, without meeting with water, and in fields
situate in the environs of rivers it is often obtained by a few strokes
with a pick-axe.
The water, found in such quantities in low grounds, comes principally
from the neighbouring hills and eminences; at the time of great rains or
sudden melting of snow, a part of the water flows on the surface, but
most of it penetrates through the small cracks and crevices it finds in
the earth and rocks. This water springs up again to the surface wherever
it can find vent; but it often filters through the sand until it comes
to a bottom of clay or solid earth, where it forms subterraneous lakes,
rivulets, and perhaps rivers, whose courses are entirely unknown; they
must, however, follow the general laws of nature, and constantly flow
from the higher grounds to the lower, and consequently these
subterraneous waters must, in the end, fall into the sea, or collect in
some low place, either on the surface or in the interior part of the
earth; for there are several lakes into which no rivers enter, nor from
which there are not any issue; and a much greater number, which do not
receive any considerable river, that are the sources of the greatest
rivers on earth; such as the lake of St. Laurence; the lake Chiamè,
from whence spring two great rivers that water the kingdoms of Asam and
Pegu; the lake of Assiniboil in America; those of Ozera in Muscovy, that
give rise to the river Irtis, and a great number of others. These lakes,
it is evident, must be produced by the waters from the high lands
passing through subterraneous passages, and collecting in the lowest
places.
Public-domain text, read in full here on John Shaqi.
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