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Hutton, James, 1726-1797

"Theory of the Earth, Volume 1 (of 4)"

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It will thus appear, that the doctrine which of late has prevailed, of
primitive mountains, or something which should be considered as original
in the construction of this earth, must be given up as a false view of
nature, which has formed the granite upon the same principle with that
of any other consolidated stratum; so far as the collection of different
materials, and the subsequent fusion of the compound mass, are necessary
operations in the preparation of all the solid masses of the earth.
Whatever operations of the globe, therefore, may be concluded from the
composition of granite masses, as well as of the alpine strata, these
must be considered as giving us information with regard to the natural
history of this earth; and they will be considered as important, in
proportion as they disclose to us truths, which from other strata might
not be so evident, or at all made known.
Let us now examine the arguments, which, may be employed in favour of
that supposition of primitive mountains.
The observations, on which naturalists have founded that opinion of
originality in some of the component parts of our earth, are these;
_first_, They observe certain great masses of granite in which
stratification is not to be perceived; this then they say is an original
mass, and it is not to be derived from any natural operation of the
globe; _secondly_, They observe considerable tracts of the earth
composed of matter in the order of stratification as to its general
composition, but not as to its particular position, the vertical
position here prevailing, instead of the horizontal which is proper to
strata formed in water; this, therefore, they also term primitive, and
suppose it to be from another origin than that of the subsidence of
materials moved in the waters of the globe; _lastly_, They observe both
strata and masses of calcareous matter in which they cannot distinguish
any marine body as is usual in other strata of the same substance; and
these calcareous masses being generally connected with their primitive
mountains, they have also included these collections of calcareous
matter, in which marine bodies are not observed, among the primitive
parts which they suppose to be the original construction of this globe.


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