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
The immediate question now before us is not, If the subterraneous fire,
or elevating power, which we perceive sometimes as operating with such
energy, be the consolidating cause of strata formed at the bottom of the
sea; nor, if that power be the means of making land appear above the
general surface of the water? for, though this be the end we want to
arrive at ultimately, the question at present in agitation respects the
laws of nature, or the generality of particular appearances.
Has the globe within it such an active power as fits it for the
renovation of that part of its constitution which may be subject to
decay? Are those powerful operations of fire, or subterraneous heat,
which so often have filled us with terror and astonishment, to be
considered as having always been? Are they to be concluded as proper to
every part upon the globe, and as continual in the system of this earth?
If these points in question shall be decided in the affirmative, we can
be at no loss in ascertaining the power which has consolidated strata,
nor in explaining the present situation of those bodies, which had their
origin at the bottom of the sea. This, therefore, should be the object
of our pursuit; and in order to have demonstration in a case of physical
inquiry, we must again have recourse to the book of nature.
The general tendency of heat is to produce fluidity and softness; as
that of cold is, on the contrary, to harden soft and fluid bodies. But
this softening power of heat is not uniform in its nature; it is made to
act with very different effect, according to the nature of the substance
to which it is applied. We are but limited in the art of increasing the
heat or the cold of bodies; we find, however, extreme difference in
their substances with respect to fusibility.
A fusible substance, or mineral composition in a fluid state, is emitted
from those places of the earth at which subterraneous fire and expansive
force are manifested in those eruptive operations. In examining these
emitted bodies, men of science find a character for such productions, in
generalising the substance, and understanding the natural constitution
of those bodies. It is in this manner that such a person, finding a
piece of lava in any place of the earth, says with certainty, Here is a
stone which had congealed from a melted state.
Having thus found a distinguishing character for those fused substances
called, in general, Lavas, and having the most visible marks for that
which had been actually a volcano, naturalists, in examining different
countries, have discovered the most undoubted proofs of many ancient
volcanos, which had not been before suspected. Thus, volcanos will
appear to be not a matter of accident, or as only happening in a
particular place, they are general to the globe, so far as there is
no place upon the earth that may not have an eruption of this kind;
although it is by no means necessary for every place to have had those
eruptions.
Public-domain text, read in full here on John Shaqi.
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