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 only question, therefore, which it concerns us to decide at present,
is, Whether those operations of extreme heat, and violent mechanic
force, be only in the system as a matter of accident; or if, on the
contrary, they are operations natural to the globe, and necessary in the
production of such land as this which we inhabit? The answer to this is
plain: These operations of the globe remain at present with undiminished
activity, or in the fullness of their power.
A stream of melted lava flows from the sides of Mount Aetna. Here is a
column of weighty matter raised from a great depth below, to an immense
height above, the level of the sea, and rocks of an enormous size
are projected from its orifice some miles into the air. Every one
acknowledges that here is the liquefying power and expansive force of
subterranean fire, or violent heat. But, that Sicily itself had been
raised from the bottom of the ocean, and that the marble called Sicilian
Jasper, had its solidity upon the same principle with the lava, would
stumble many a naturalist to acknowledge. Nevertheless, I have in my
possession a table of this marble, from which it is demonstrable, that
this calcareous stone had flowed, and been in such a state of fusion and
fluidity as lava.
Here is a comparison formed of two mineral substances, to which it is of
the highest importance to attend. The solidity and present state of the
one of these is commonly thought to be the operation of fire; of the
other, again, it is thought to be that of water. This, however, is not
the case. The immediate state and condition of both these bodies is now
to be considered as equally the effect of fire or heat. The reason of
our forming such a different judgment with regard to these two subjects
is this; we see, in the one case, the more immediate connection of the
cause and the effect, while, in the other, we have only the effects from
whence we are in science to investigate the cause.
But, if it were necessary always to see this immediate connection, in
order to acknowledge the operation of a power which, at present, is
extinguished in the effect, we should lose the benefit of science, or
general principles, from whence particulars may be deduced, and we
should be able to reason no better than the brute. Man is made for
science; he reasons from effects to causes, and from causes to effects;
but he does not always reason without error. In reasoning, therefore,
from appearances which are particular, care must be taken how we
generalise; we should be cautious not to attribute to nature, laws which
may perhaps be only of our own invention.
Public-domain text, read in full here on John Shaqi.
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