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
[Footnote 71: Phil. Trans. vol. l. p. 688. CAMPER denies that the
remains here mentioned belong to the crocodile, or any amphibious
animal, and refers them to the balænaæ. He passes the same judgment on
those fossil bones from St Peter's Mount, near Maestricht, which have
been supposed to belong to the crocodile; he looks on them as belonging
to whales, though of an unknown species. In this Mount, so famous for
its petrifactions, he finds many specimens of bones, which he thinks
belong to the turtle. Phil. Trans. vol lxxvi. p. 443. The opinion of an
author, so well skilled in comparative anatomy, must be regarded as of
great weight: if it takes from our argument in one part, it adds to it
in another, and the acquisition of the turtle makes up abundantly for
the loss of the crocodile.]
On this subject I cannot help observing, that the accurate comparison
of the animal exuviæ of the mineral kingdom, with their living
archetypes, is not merely a curious inquiry, but is one that may lead
to important consequences, concerning the nature and direction of the
forces which have changed, and are continually changing, the surface of
the earth.
161. These remarks I have thought it proper to add to the proofs of the
composition of the present from former strata, in order to show, that
the great transportation of materials involved in that supposition, is
not only conformable to the hypothesis of the Neptunists concerning
the secondary strata, but is also proved by the most direct evidence,
independently of all hypothesis. All this reasoning regards the ancient
state of the globe. Whether such a travelling of stony bodies makes
a part of the system now actually carrying on, will be considered in
another place.[72]
[Footnote 72: See NOTE XIX.]
NOTE VI. § 13.
_Mr Kirwan's notion of precipitation._
162. The Neptunist who has provided the means of dissolving the
materials of the strata, has only performed half his work, and must
find it a task of equal difficulty to force this powerful menstruum
to part with its solution. Mr Kirwan, aware in some degree of this
difficulty, has attempted to obviate it in a very singular way. First,
he ascribes the solution of all substances in water, or in what he
calls the chaotic fluid, to their being finely pulverised, or created
in a state of the most minute division. Next, as to the deposition, the
solvent being, as he acknowledges, very insufficient in quantity, the
precipitation took place, (he says,) on that account the more rapidly.
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