The Life of Sir Humphry Davy, Bart. LL.D., Volume 2 (of 2)Paris, John Ayrton
History
The Life of Sir Humphry Davy, Bart. LL.D., Volume 2 (of 2)
Paris, John Ayrton
Chemists -- England -- Biography; Davy, Humphry, Sir, 1778-1829
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"I have no objection to the '_refined Plutonic view_,' (of
Professor Playfair and Sir James Hall,) as capable of explaining
many existing phenomena; indeed, you must be aware that I have
myself had recourse to it. What I contend against is, its
application to explain the formations of the secondary rocks, which
I think clearly belong to an order of facts not at all embraced by
it. In the Plutonic system, there is one simple and constant order
assumed, which may be supposed eternal. The surface is constantly
imagined to be disintegrated, destroyed, degraded, and washed into
the bosom of the ocean by water, and as constantly consolidated,
elevated, and regenerated by fire; and the ruins of the old form
the foundations of the new world. It is supposed that there are
always the same types both of dead and living matter,--that the
remains of rocks, of vegetables, and animals of one age are found
imbedded in rocks raised from the bottom of the ocean in another.
Now, to support this view, not only the remains of living beings
which at present people the globe, might be expected to be found in
the oldest secondary strata, but even those of the art of man, the
most powerful and populous of its inhabitants, which is well known
not to be the case. On the contrary, each stratum of the secondary
rocks contains remains of peculiar and mostly now unknown species
of vegetables and animals. In those strata which are deepest, and
which must consequently be supposed to be the earliest deposited,
forms even of vegetable life are rare; shells and vegetable remains
are found in the next order; the bones of fishes and oviparous
reptiles exist in the following class; the remains of birds, with
those of the same genera mentioned before, in the next order; those
of quadrupeds of extinct species in a still more recent class;
and it is only in the loose and slightly consolidated strata of
gravel and sand, and which are usually called diluvian formations,
that the remains of animals, such as now people the globe, are
found, with others belonging to extinct species. But in none of
these formations, whether called secondary, tertial, or diluvial,
have the remains of man, or any of his works, been discovered. It
is, I think, impossible to consider the organic remains found in
any of the earlier secondary strata, the lias-limestone and its
congenerous formations, for instance, without being convinced,
that the beings whose organs they formed belonged to an order of
things entirely different from the present. Gigantic vegetables,
more nearly allied to the palms of the equatorial countries than
to any other plants, can only be imagined to have lived in a very
high temperature; and the immense reptiles, the _Megalosauri_, with
paddles instead of legs, and clothed in mail, in size equal, or
even superior to the whale; and the great amphibia _Plethiosauri_,
with bodies like turtles, but furnished with necks longer than
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