Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4)Hutton, James
Science
Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4)
Hutton, James
Geology -- Early works to 1800
"J'ai été étonné de trouver au centre d'un énorme massif de granit, que
l'on avoit ouvert avec la poudre pour pratiquer un chemin, des
morceaux, gros comme le poing et au dessous, de spath calcaire blanc,
très-effervescent, en grandes écailles, ou lames entrecroisées. Il
n'occupoit point des cavités particulières, il n'y paroissoit le
produit d'une infiltration qui auroit rempli des cavités, mais il étoit
incorporé avec les feld-spath, le mica, et le quartz, faissoit masse
avec eux, et ne pouvoit se rompre sans les entraîner avec lui."
This great naturalist is convinced that the spar had not been here
introduced by infiltration, although that is the very method which he
employs to form concretions, not only of spar but of crystal, zeolite,
and pyrites, in the closest cavities of the most solid rocks of
basaltes. These four substances in this stone were so mixed together
that nothing but the fusion of the whole mass could explain the state in
which they appeared; but, thinking that such a supposition could not
be allowed, this naturalist, like a man of science when his data fail,
leaves the matter without any interpretation of his own. This however is
what he has not done in the case of basaltes, or that which he mistakes
for proper lavas, as I shall have occasion to show.]
Here is an infinite operation, but an operation which is easily
performed by the natural arrangement of substances acting freely in
a fluid state, and concreting together, each substance, whether more
simple or more compound, directing itself by its internal principle of
attraction, and affecting mechanically those that are concreting around
it.
We see the very same thing happen under our eye, and precisely in the
same manner. When a fluid mass of any mineral or metallic substance is
made to congeal by sudden cooling on the outside, while the mass within
is fluid, a cavity is thus sometimes formed by the contraction of the
contained fluid; and in this cavity are found artificial _druzen_, as
they may be called, being crystallizations similar to those which the
mineral cavities exhibit in such beauty and perfection.
Petrification and consolidation, in some degree, may doubtless be
performed, in certain circumstances, by means of the solution of
calcareous earth; but the examples given by M. de Luc, of those bodies
of lime-stone and agate petrified in the middle of strata of loose or
sandy materials, are certainly inexplicable upon any other principle
except the fusion of those substances with which the bodies are
petrified[35].
[Note 35: Vid. Lettre 28 et Lettre 103. Lettres Physiques et Morales.]
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