Theory of the Earth, With Proofs and Illustrations, Volume 2 (of 4)Hutton, James
Science
Theory of the Earth, With Proofs and Illustrations, Volume 2 (of 4)
Hutton, James
Geology -- Early works to 1800
In the last chapter, I have been using arguments to prove that M. de
Luc has reasoned erroneously, in concluding the future stability of a
continent; and I have been endeavouring to show that our continent
is necessarily wasted in procuring food to plants, or in serving the
various purposes of a system of living animals. We have now in view to
illustrate this theory of the degradation of the surface of the earth;
a theory necessarily leading to that system of the world in which a
provision is made for future continents; and a theory explaining various
natural appearances which otherwise are not to be understood. A door may
thus be opened for the investigation of natural history, particularly
that which traces back, from the present state of things, those
operations of nature which are more immediately connected with what we
take much pleasure to behold, viz. the surface of the earth stored with
such a variety of beautiful plants, and inhabited by such a diversity of
animals, all subservient to the use of man.
There are two ways in which we may look for the transactions of time
past, in the present state of things, upon the surface of this earth,
and read the operations of an ancient date in those which are daily
transacted under our eye. The one of these is to examine the soil, and
to trace the origin of that which we find loose upon the surface of the
earth, or only compacted by the soft and cohesive nature of some of its
materials. In thus studying the soil we shall learn the destruction of
the solid parts; and though, by this means, we cannot form an estimate
of the quantity of this destruction which had been made, we shall, upon
many occasions, see a certain _minimum_ of this quantity which may
perhaps astonish us.
The second method here proposed, is to examine the solid part of the
earth, in order to learn the quantity of matter which had been separated
from this mass. Here also we shall not be able to compute the quantity
of what had been destroyed; but we shall every where find a certain
_minimum_ of this quantity, which will give us an extensive view with
regard to the operation of the elements and seasons upon the surface of
this earth. We shall now examine more particularly those two ways of
judging with regard to the operations of time past, and the changes
which have been made upon the surface of our land, by those active
causes, which, being in the constitution of this earth, must continue to
operate with undiminished power, and tend to preserve the _whole_ amidst
the destruction of its particular parts.
Public-domain text, read in full here on John Shaqi.
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