A History of Science — Volume 3Williams, Henry Smith
History
A History of Science — Volume 3
Williams, Henry Smith
Science -- History
From all this, therefore, Hutton reached the conclusion that the
elevation of the bodies of land above the water on the earth's surface
had been effected by the same force which had acted in consolidating the
strata and giving them stability. This force he conceived to be exerted
by the expansion of heated matter.
"We have," he said, "been now supposing that the beginning of our
present earth had been laid in the bottom of the ocean, at the
completion of the former land, but this was only for the sake of
distinctness. The just view is this, that when the former land of the
globe had been complete, so as to begin to waste and be impaired by
the encroachment of the sea, the present land began to appear above the
surface of the ocean. In this manner we suppose a due proportion to be
always preserved of land and water upon the surface of the globe, for
the purpose of a habitable world such as this which we possess. We
thus also allow time and opportunity for the translation of animals and
plants to occupy the earth.
"But if the earth on which we live began to appear in the ocean at
the time when the LAST began to be resolved, it could not be from the
materials of the continent immediately preceding this which we examine
that the present earth has been constructed; for the bottom of the ocean
must have been filled with materials before land could be made to appear
above its surface.
"Let us suppose that the continent which is to succeed our land is at
present beginning to appear above the water in the middle of the Pacific
Ocean; it must be evident that the materials of this great body, which
is formed and ready to be brought forth, must have been collected from
the destruction of an earth which does not now appear. Consequently,
in this true statement of the case there is necessarily required the
destruction of an animal and vegetable earth prior to the former land;
and the materials of that earth which is first in our account must have
been collected at the bottom of the ocean, and begun to be concocted for
the production of the present earth, when the land immediately preceding
the present had arrived at its full extent.
"We have now got to the end of our reasoning; we have no data further
to conclude immediately from that which actually is; but we have got
enough; we have the satisfaction to find that in nature there are
wisdom, system, and consistency. For having in the natural history of
the earth seen a succession of worlds, we may from this conclude that
there is a system in nature; in like manner as, from seeing revolutions
of the planets, it is concluded that there is a system by which they are
intended to continue those revolutions. But if the succession of worlds
is established in the system of nature, it is in vain to look for
anything higher in the origin of the earth. The result, therefore,
of our present inquiry is that we find no vestige of a beginning--no
prospect of an end."
Public-domain text, read in full here on John Shaqi.
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