Buffon's Natural History, Volume 02 (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 02 (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 substances of the first class can never acquire the nature and
properties of the other. Stone will always be as remote from the nature
of flint, as potters earth is from marle; no known agent will ever be
capable of making them quit the combinations peculiar to their nature:
the country which produces stone and marble will remain to do so as
certainly as those wherein there is only flint and granate will never
have either stone or marble.
If we observe the order and distribution of matters in a hill composed
of vitrifiable matters, we shall commonly find, under the first bed
of vegetable earth, a bed of clay, a vitrifiable matter, analogous to
flint, and which, as I have observed, is only a decomposed vitrifiable
sand: this bed of argilaceous earth or sand answers to a bed of gravel
met with in hills composed of calcinable matters: beneath which we meet
with some beds of free-stone scarcely ever more than six inches thick,
and divided into small pieces by perpendicular clefts. Under these
beds are many others of the same matters, and also beds of vitrifiable
sand, the free-stone becomes harder and its blocks encrease in size
in proportion as we descend; underneath these we find a very hard
matter which I have called live rock, or flint in large masses, which
is so hard as to resist the file, graver, and acid spirits, more than
vitrifiable sand, and even powdered glass, on which aqua-fortis seems
to have some effect. If struck by another hard body it emits sparks,
and exhales a very penetrating smell of sulphur. This massy flint, as
I have termed it, is generally found with beds of clay, earth, coals,
and vitrifiable sand, answers to the strata of hard stone and marbles,
which serve as a base to hills composed of calcinable matters.
Water, by flowing through perpendicular clefts, and by penetrating
the strata of these vitrifiable sands, clays, and earths, becomes
impregnated with the fine and most homogeneous parts of these matters,
and forms many different concretions, such as talcs, amianthus's, and
various other substances produced by distillations through vitrifiable
matters.
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