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
Another general fact concerning these remains, is, that they are found
in all countries whatsoever, but always in the loose or travelled
earth, and never in the genuine strata. Since the year 1696, when the
attention of the curious was called to this subject, by the skeleton
of an elephant dug up in Thuringia, and described by Tentzelius,[212]
there is hardly a country in Europe which has not afforded instances
of the same kind. Fossil bones, particularly grinders and tusks of
elephants, have been found in other places of Germany, in Poland,
France, Italy, Britain, Ireland, and even Iceland.[213] Two countries,
however, afford them in greater abundance by far than any other part of
the known world; namely, the plains of Siberia in the old continent,
and the flat grounds on the banks of the Ohio in the new.[214]
[Footnote 212: Phil. Trans. vol. xix. p. 757.]
[Footnote 213: A grinder of an elephant found in Iceland, is described
by _Bartholinus_, Acta Hafniens. vol. i. p. 83.]
[Footnote 214: The fossil bones on the Ohio are described in two papers
by Mr P. Collinson, Phil. Trans. vol. lvii. p. 464 and 468.]
408. When the bones in Siberia were first discovered, they were
supposed to belong to an animal that lived under ground, to which
they gave the name of the _mammouth_; and the credit bestowed on this
absurd fiction, is a proof of the strong desire which all men feel
of reconciling extraordinary appearances with the regular course of
nature. Much skill, however, in natural history was not required to
discover that many of the bones in question resembled those of the
elephant, particularly the grinders and the tusks of that animal.
Others resembled the bones of the rhinoceros; and a head of that kind,
having the hide preserved upon it, was found in Siberia, and is still
in the imperial cabinet at Petersburgh.
Pallas has described the fossil bones which he found in the museum at
Petersburgh, on his being appointed to the superintendence of it, and
enumerates, not only bones that belong, in his opinion, to the elephant
and rhinoceros, but others that belong to a kind of buffalo, very
different from any now known, and of a size vastly greater.[215] He has
also described, in another very curious memoir, the bones of the same
kind that he met with in his travels through the north-east parts of
Asia.
[Footnote 215: Novi Comment Petrop. tom. xiii. (1768,) p. 436, and tom.
xvii. p. 576, &c.]
The fossil bones found on the banks of the Ohio, resemble in many
things those of Siberia; like them they are contained in the soil or
alluvial earth, and never in the solid strata; like them too they are
no otherwise changed from their natural state, than by being sometimes
slightly calcined at the surface; they are also of great size, and in
great numbers, being probably the remains of several different species.
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