A History of Science — Volume 3Williams, Henry Smith
History
A History of Science — Volume 3
Williams, Henry Smith
Science -- History
"There are, in all the regions of the earth, huge masses of calcareous
matter in that crystalline form or sparry state in which, perhaps, no
vestige can be found of any organized body, nor any indication that such
calcareous matter has belonged to animals; but as in other masses this
sparry structure or crystalline state is evidently assumed by the marine
calcareous substances in operations which are natural to the globe,
and which are necessary to the consolidation of the strata, it does not
appear that the sparry masses in which no figured body is formed
have been originally different from other masses, which, being only
crystallized in part, and in part still retaining their original form,
have ample evidence of their marine origin.
"We are led, in this manner, to conclude that all the strata of the
earth, not only those consisting of such calcareous masses, but others
superincumbent upon these, have had their origin at the bottom of the
sea.
"The general amount of our reasoning is this, that nine-tenths, perhaps,
or ninety-nine-hundredths, of this earth, so far as we see, have been
formed by natural operations of the globe in collecting loose materials
and depositing them at the bottom of the sea; consolidating those
collections in various degrees, and either elevating those consolidated
masses above the level on which they were formed or lowering the level
of that sea.
"Let us now consider how far the other proposition of strata being
elevated by the power of heat above the level of the sea may be
confirmed from the examination of natural appearances. The strata formed
at the bottom of the ocean are necessarily horizontal in their position,
or nearly so, and continuous in their horizontal direction or extent.
They may be changed and gradually assume the nature of each other, so
far as concerns the materials of which they are formed, but there cannot
be any sudden change, fracture, or displacement naturally in the body
of a stratum. But if the strata are cemented by the heat of fusion,
and erected with an expansive power acting below, we may expect to find
every species of fracture, dislocation, and contortion in those bodies
and every degree of departure from a horizontal towards a vertical
position.
"The strata of the globe are actually found in every possible position:
for from horizontal they are frequently found vertical; from continuous
they are broken and separated in every possible direction; and from a
plane they are bent and doubled. It is impossible that they could have
originally been formed, by the known laws of nature, in their present
state and position; and the power that has been necessarily required
for their change has not been inferior to that which might have been
required for their elevation from the place in which they have been
formed."(2)
Public-domain text, read in full here on John Shaqi.
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