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
Let us now consider what power would be required to force up, from the
most unfathomable depth of the ocean, to the Andes or the Alps, a column
of fluid metal and of stone. This power cannot be much less than that
required to elevate the highest land upon the globe. Whether, therefore,
we shall consider the general veins as having been filled by mineral
steams, or by fluid minerals, an elevating power of immense force is
still required, in order to form as well as fill those veins. But such a
power acting under the consolidated masses at the bottom of the sea, is
the only natural means for making those masses land.
If such have been the operations that are necessary for the production
of this land; and if these operations are natural to the globe of this
earth, as being the effect of wisdom in its contrivance, we shall
have reason to look for the actual manifestation of this truth in the
phaenomena of nature, or those appearances which more immediately
discover the actual cause in the perceived effect.
To see the evidence of marble, a body that is solid, having been formed
of loose materials collected at the bottom of the sea, is not always
easy, although it may be made abundantly plain; and to be convinced that
this calcareous stone, which calcines so easily in our fires, should
have been brought into fusion by subterraneous heat, without suffering
calcination, must require a chain of reasoning which every one is not
able to attain[13]. But when fire bursts forth from the bottom of the
sea, and when the land is heaved up and down, so as to demolish cities
in an instant, and split asunder rocks and solid mountains, there
is nobody but must see in this a power, which may be sufficient to
accomplish every view of nature in erecting land, as it is situated in
the place most advantageous for that purpose.
[Note 13: Mr le Chevalier de Dolomieu, in considering the different
effects of heat, has made the following observation; Journal de
Physique, Mai 1792.
Public-domain text, read in full here on John Shaqi.
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