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Hutton, James, 1726-1797

"Theory of the Earth, Volume 1 (of 4)"

If, therefore, it were proved, that
either the one or other of those two substances had been consolidated by
fusion, the other must be acknowledged as having had the same origin;
but now I am to prove, from the natural history of mineral coal, that
pyrites had been there formed by fusion; and then, by means of the
known origin of that sulphureo-metallic substance, we shall extend our
knowledge to the origin of every other mineral body.
The process of this argument is as follows: Every mineral body, I
believe, without exception, will be found so intimately connected with
pyrites, that these two things must be concluded as having been together
in a fluid state, and that, whatever may have been the cause of fluidity
in the one, this must have also caused the fluidity in the other;
consequently, whatever shall be proved with regard to the mineral
operations of pyrites, must be considered as proved of every other
mineral substance. But, from the connection of pyrites with mineral
coal, it is to be proved that the origin of this metallic body had been
fusion; and then it will appear, that all other mineral bodies must have
been more or less in fusion, or that they must have been consolidated
by means of heat, and not by any manner of solution or aqueous
infiltration.


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