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
Nothing can be more absurd than to suppose a collection of shells and
corals, amassed about the primitive mountains of the earth, to become
mountains equally solid with the others, upon the removal of the sea; it
would be inconsistent with every principle of sound reasoning to suppose
those masses of loose materials to oppose equal resistance to the
wasting and destroying operations of the surface of the earth, as do
those pretended primitive masses, which might be supposed endued with
natural hardness and solidity; yet, consult the matter of fact, and it
does not appear that there is any difference to be perceived. There are
lofty mountains to be found both of the one kind and the other; both
those different masses yield to the wasting operations of the surface;
and they are both carried away with the descending waters of the earth.
It is not here meant to affirm, that a mass of marble, which is
a calcareous substance, opposes equal resistance, whether to the
operations of dissolution or attrition, as a mass composed of granite or
of quartz; it is only here maintained that there are in the Alps lofty
mountains of marble, as there are in other places lower masses of
granite and its accompanying schistus. But that which is particularly to
be attended to here is this: In all countries of the earth, whether of
primitive masses or those of secondary formation, whether uniform and
homogeneous, or compound and mixed of those two different kinds of
bodies, the system is always the same, of hills and valleys, lakes and
rivers, ravines and streams: no man can say, by looking into the most
perfect map, what is primary or what secondary in the constitution of
the globe. It is the same system of larger rivers branching into lesser
and lesser in a continued series, of smaller rivers in like manner
branching into rivulets, and of rivulets terminating at last into
springs or temporary streams. The principle is universal; and, having
learned the natural history of one river, we know the constitution of
every other upon the face of the earth.
Thus all the surface of this earth is formed according to a regular
system of heights and hollows, hills and valleys, rivulets and rivers,
and these rivers return the waters of the atmosphere into the general
mass, in like manner as the blood, returning to the heart, is conducted
in the veins. But as the solid land, formed at the bottom of the sea or
in the bowels of the earth, could not be there constructed according to
that system of things which we find so widely pursued upon the surface
of the globe, it must be by wasting the solid parts of the land that
this system of the surface has been formed, in like manner as it is by
the operations of the sea that the shape of the land is determined, upon
the shore.
Public-domain text, read in full here on John Shaqi.
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