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
The extent of the tract through which these bones are scattered, is a
circumstance truly wonderful. Pallas assures us,[226] that there is not
a river of considerable size in all the north of Asia, from the Tanais,
which runs into the Black Sea, to the Anadyr, which falls into the Gulf
of Kamtchatka, in the sides or bottom of which bones of elephants and
other large animals have not been found. This is especially the case
where the rivers run in plains through gravel, sand, clay, &c.; among
the mountains, the bones are rarely discovered. The extent of the tract
just mentioned exceeds four thousand miles; and how the bones could
be distributed over all that extent, by any means but by the animals
having lived there, it seems impossible to conceive. No torrent nor
inundation could have produced this effect, nor could the bones brought
in that way have been laid together so as to form complete skeletons.
[Footnote 226: De Reliquiis Animalium exoticorum, per Asiam Borealem
repertis.--"Nov. Comment Petrop. tom. xvii. (1772,) p. 576.]
416. One fact recorded by the same author, seems calculated to remove
all uncertainty. It is that of the carcase of a rhinoceros, almost
entire, and covered with the hide, found in the earth in the banks of
the river Wilui, which falls into the Lena below Jakutsk.[227] Some of
the muscles and tendons were actually adhering to the head when Pallas
received it. The head, after being dried in an oven, is still preserved
in the museum at Petersburgh. The preservation of the skin and muscles
of this natural mummy, as Pallas calls it, was no doubt brought
about by its being buried in earth that was in a state of perpetual
congelation; for the place is in the parallel of 64°, where the ground
is never thawed but to a very small depth below the surface.
[Footnote 227: Pallas _ubi supra_, p. 586. Also, Voyages de Pallas,
tom. iv. p. 131.]
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