The Birth-Time of the World and Other Scientific Essays — John Shaqi
The Birth-Time of the World and Other Scientific EssaysJoly, John
Science
The Birth-Time of the World and Other Scientific Essays
Joly, John
Science
The transfer of matter from the exposed land surfaces to the
sub-oceanic slopes of the continents and the increase in the
density of the ocean, must all along have been attended by
isostatic readjustment. We cannot take any other view. On the one
hand the land was being lightened; on the other the sea was
increasing in mass and depth and the flanks of the continents
were being loaded with the matter removed from the land and borne
in solution to the ocean. How important the resulting movements
must have been may be gathered from the fact that the existing
land of the Globe stands at a mean elevation of no more than
2,000 feet above sea level. We have seen that solvent denudation
removed over 1,600 feet of rock. But we have no evidence that on
the whole the elevation of land in the past was ever very
different from what it now is.
We have, then, presented to our view the remarkable fact that
throughout the past, and acting with extreme
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slowness, the land has steadily been melted down into the sea and
as steadily been upraised from the waters. It is possible that
the increased bulk of the ocean has led to a certain diminution
of the exposed land area. The point is a difficult one. One thing
we may without much risk assume. The sub-aereal current of
dissolved matter from the land to the ocean was accompanied by a
sub-crustal flux from the ocean areas to the land areas; the
heated viscous materials creeping from depths far beneath the
ocean floor to depths beneath the roots of the mountains which
arose around the oceans. Such movements took ages for their
accomplishment. Indeed, they have been, probably, continuous all
along and are still proceeding. A low degree of viscosity will
suffice to permit of movements so slow. Superimposed upon these
movements the rhythmic alternations of depression and elevation
of the geosynclines probably resulted in releasing the crust from
local accumulation of strains arising in the more rigid surface
materials. The whole sequence of movements presents an
extraordinary picture of pseudo-vitality--reminding us of the
circulatory and respiratory systems of a vast organism.
All great results in our universe are founded in motions and
forces the most minute. In contemplating the Cause or the Effect
we stand equally impressed with the spectacle presented to us. We
shall now turn from the great effects of denudation upon the
history and evolution of a world and consider for a moment
activities
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so minute in detail that their operations will probably for ever
elude our bodily senses, but which nevertheless have necessarily
affected and modified the great results we have been
considering.
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