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Hutton, James, 1726-1797

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

Il est evident,
que le silex est forme de la pierre puante, parce qu'on remarque ici
les memes phenomenes dont j'ai parle plus haut, c. a. d. les passages
successifs de l'une dans l'autre pierre, tant en montant qu'en
descendant."
There is nothing particular in the siliceous mixture in this species of
lime-stone, except the vein of that substance. It is evident that this
vein, traversing the mountain, had been introduced in the fluid state
of fusion. I do not mean to say, that, in this particular case now
described, the evidence of that truth peculiarly appears; but that, from
the general nature of mineral veins breaking and traversing the solid
strata of the globe, no other conclusion can be formed; and that in
the particulars of this example there is nothing that could lead us to
suppose any other origin to the petrifactions contained in this vein
of stinking lime-stone. It is plain, that our author has imagined to
himself an unknown manner of executing his mineral metamorphoses. He
sees plainly that the common notion of infiltration will not at all
explain the evident confusion of those calcareous and siliceous bodies
which appear to him to be metamorphosing into each other.


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