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
134. If indeed this theory of the earth is as well founded as we
suppose it to be, the lapse of time must necessarily remove all
objections to it, and the progress of science will only develope its
evidence more fully. As it stands at present, though true, it must be
still imperfect; and it cannot be doubted, that the great principles
of it, though established on an immoveable basis, must yet undergo
many modifications, requiring to be limited, in one place, or to be
extended, in another. A work of such variety and extent cannot be
carried to perfection by the efforts of an individual. Ages may be
required to fill up the bold outline which Dr Hutton has traced with so
masterly a hand; to detach the parts more completely from the general
mass; to adjust the size and position of the subordinate members; and
to give to the whole piece the exact proportion and true colouring of
nature.
This, however, in length of time, may be expected from the advancement
of science, and from the mutual assistance which parts of knowledge,
seemingly the most remote, often afford to one another. Not only
may the observations of the mineralogist, in tracts yet unexplored,
complete the enumeration of geological facts; and the experiments of
the chemist, on substances not yet subjected to his analysis, afford a
more intimate acquaintance with the nature of fossils, and a measure
of the power of those chemical agents to which this theory ascribes
such vast effects: but also, from other sciences, less directly
connected with the natural history of the earth, much information may
be received. The accurate geographical maps and surveys which are now
making; the foundings; the obsevations of currents; the barometrical
measurements, may all combine to ascertain the reality, and to fix the
quantity of those changes which terrestrial bodies continually undergo.
Every new improvement in science affords the means of delineating more
accurately the face of nature as it now exists, and of transmitting, to
future ages, an account, which may be compared with the face of nature
as it shall then exist. If, therefore, the science of the present times
is destined to survive the physical revolutions of the globe, the
HUTTONIAN THEORY may be confirmed by historical record; and the author
of it will be remembered among the illustrious few, whose systems
have been verified by the observations of succeeding ages, supported
by facts unknown to themselves, and established by the decisions of a
tribunal, slow, but infallible, in distinguishing between truth and
falsehood.
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NOTES AND ADDITIONS.
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NOTES AND ADDITIONS.
NOTE I. § 2.
_Origin of calcareous rocks._
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