Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4)Hutton, James
Science
Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4)
Hutton, James
Geology -- Early works to 1800
In order to understand the system of the heavens, it is necessary to
connect together periods of measured time, and the distinguished places
of revolving bodies. It is thus that system may be observed, or wisdom,
in the proper adapting of powers to an intention. In like manner, we
cannot understand the system of the globe, without seeing that progress
of things which is brought about in time, thus measuring the natural
operations of the earth with those of the heavens. This is properly the
business of the present undertaking.
Our object is to know the time which had elapsed since the foundation of
the present continent had been laid at the bottom of the ocean, to the
present moment in which we speculate on these operations. The space is
long; the data for the calculations are, perhaps, deficient: No matter;
so far as we know our error, or the deficiency in our operation, we
proceed in science, and shall conclude in reason. It is not given to man
to know what things are truly in themselves, but only what those things
are in his thought. We seek not to know the precise measure of any
thing; we only understand the limits of a thing, in knowing what it is
not, either on the one side or the other.
We are investigating the age of the present earth, from the beginning of
that body which was in the bottom of the sea, to the perfection of its
nature, which we consider as in the moment of our existence; and we have
necessarily another aera, which is collateral, or correspondent, in the
progress of those natural events. This is the time required, in the
natural operations of this globe, for the destruction of a former
earth; an earth equally perfect with the present and an earth equally
productive of growing plants and living animals. Now, it must appear,
that, if we had a measure for the one of those corresponding operations,
we would have an equal knowledge of the other.
The formation of a future earth being in the bottom of the ocean, at
depths unfathomable to man, and in regions far beyond the reach of his
observation, here is a part of the process which cannot be taken as a
principle in forming an estimate of the whole. But, in the destruction
of the present earth, we have a process that is performed within the
limits of our observation; therefore, in knowing the measure of this
operation, we shall find the means of calculating what had passed on a
former occasion, as well as what will happen in the composition of a
future earth. Let us, therefore, now attempt to make this estimate of
time and labour.
Public-domain text, read in full here on John Shaqi.
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