Illustrations of the Huttonian Theory of the EarthPlayfair, John
Science
Illustrations of the Huttonian Theory of the Earth
Playfair, John
Geology; Hutton, James, 1726-1797. Theory of the earth
221. According to this theory, veins were filled by the injection of
fluid matter from below; and this account of them, which agrees so
well with the phenomena already described, is confirmed by this, that
nothing of the substances which fill the veins is to be found any where
at the surface. It is not with the veins as with the strata, where, in
the loose sand on the shore, and in the shells and corals accumulated
at the bottom of the sea, we perceive the same materials of which these
strata are composed. The same does not equally hold of metallic veins:
"Look," says Dr Huston, "into the sources of our mineral treasures? Ask
the miner from whence has come the metal in his veins? Not from the
earth or air above, not from the strata which the vein traverses: these
do not contain an atom of the minerals now considered. There is but
one place from whence these minerals may have come; this is the bowels
of the earth; the place of power and expansion; the place from whence
has proceeded that intense heat, by which loose materials have been
consolidated into rocks, as well as that enormous force, by which the
regular strata have been broken and displaced."[117]
[Footnote 117: Theory of the Earth, vol. i. p. 130.]
222. The above is a very just and natural reflection; but if, instead
of interrogating the miner; we consult the Neptunist, we will receive
a very different reply. As this philosopher never embarrasses himself
about preserving a uniformity in the course of nature, he will tell
us, that though it may be true, that neither the air, the upper part
of the earth's surface, nor even the sea, contain at present any thing
like the materials of the veins, yet the time was when these materials
were all mingled together in the chaotic mass, and constituted one
vast fluid, encompassing the earth; from which fluid it was, that the
minerals were precipitated and deposited in the clefts and fissures of
the strata.
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