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 raising up of a continent of land from the bottom of the sea, is an
idea that is too great to be conceived easily in all the parts of its
operations, many of which are perhaps unknown to us; and, without being
properly understood, so great an idea may appear like a thing that is
imaginary. In like manner, the co-relative, or corresponding operation,
the destruction of the land, is an idea that does not easily enter into
the mind of man in its totality, although he is daily witness to part of
the operation. We never see a river in a flood, but we must acknowledge
the carrying away of part of our land, to be sunk at the bottom of the
sea; we never see a storm upon the coast, but we are informed of a
hostile attack of the sea upon our country; attacks which must, in time,
wear away the bulwarks of our soil, and sap the foundations of our
dwellings. Thus, great things are not understood without the analysing
of many operations, and the combination of time with many events
happening in succession.
Let us now consider what is to be the subject of examination, and where
it is that we are to observe those operations which must determine
either the stability or the instability of this land on which we live.
Our land has two extremities; the tops of the mountains, on the one
hand, and the sea-shores, on the other: It is the intermediate space
between these two, that forms the habitation of plants and animals.
While there is a sea-shore and a higher ground there is that which is
required in the system of the world: Take these away, and there would
remain an aqueous globe, in which the world would perish. But, in the
natural operations of the world, the land is perishing continually; and
this is that which now we want to understand.
Upon the one extremity of our land, there is no increase, or there is no
accession of any mineral substance. That place is the mountain-top, on
which nothing is observed but continual decay. The fragments of the
mountain are removed in a gradual succession from the highest station to
the lowest. Being arrived at the shore, and having entered the dominion
of the waves, in which they find perpetual agitation, these hard
fragments, which had eluded the resolving powers natural to the surface
of the earth, are incapable of resisting the powers here employed for
the destruction of the land. By the attrition of one hard body upon
another, the moving stones and rocky shore, are mutually impaired. And
that solid mass, which of itself had potential liability against the
violence of the waves, affords the instruments of its own destruction,
and thus gives occasion to its actual instability.
Public-domain text, read in full here on John Shaqi.
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