Buffon's Natural History. Volume 10 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Minerals, &c. &cBuffon, Georges Louis Leclerc, comte de
History
Buffon's Natural History. Volume 10 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Minerals, &c. &c
Buffon, Georges Louis Leclerc, comte de
Natural history
One of these particular causes proceeds, in some measure, from the
first general cause, and may add something to it. It is certain that
during the time of incadescence, and indeed all the subsequent ages
till that of the refrigeration of the earth, not any of the volatile
matters could reside at the surface, or even in the internal part,
of the globe; they were raised and dispersed in the form of vapours,
and could not deposit themselves but successively in proportion as it
cooled, by which means some of these matters have penetrated through
the clefts and crevices of the earth to great depths, in an infinity of
places; and this is the primitive foundation of volcanos, which are all
found in lofty mountains, where the clefts of the earth are so much the
greater as these points of the globe are more projecting and isolated.
This deposit of the volatile combustible matters of the first ages
will have been greatly augmented by the addition of every combustible
matter which has been subsequently formed. Pyrites, sulphurs, coal,
bitumen, &c. have penetrated into the principal cavities of the earth,
and produced almost every where great masses of inflammable matters,
and often conflagrations, which have been manifested by earthquakes,
erruptions of volcanos, and by the hot springs which flow from
mountains, or run internally in the cavities of the earth. It may,
therefore, be presumed that these subterraneous fires, some of which
burn without explosion, and others with great noise and violence,
somewhat increase the general heat of the globe. Nevertheless this
addition of heat can be only very slight, for it has been observed
that it is nearly as cold on the top of volcanos as on the top of other
mountains of the same height, except at the very time when the volcano
throws out inflamed vapours or burning matters.
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