Volcanoes: What They are and What They TeachJudd, John W. (John Wesley)
Science
Volcanoes: What They are and What They Teach
Judd, John W. (John Wesley)
Volcanoes
Now the density of the materials which compose the crust of the globe
is very much less than this, varying from about two-and-one-third to
three times that of water. Hence we are compelled to conclude that the
interior portions of the globe are of far greater density than the
exterior portions; that, as a matter of fact, the mass of the globe is
composed of materials having twice the density of the rocks exposed at
the surface.
[Sidenote: DENSITY OF EARTH'S INTERIOR.]
It has been sometimes argued that as all materials under intense
pressure appear to yield to an appreciable extent, and to allow their
particles to be packed into a smaller compass, we may find in this fact
an explanation of the great density of the internal parts of the globe.
It has in fact been suggested that under the enormous pressure which
must be exerted by masses of rock several thousand feet in thickness,
the materials of which our earth is composed may be compelled to pack
themselves into less than one-half the compass which they occupy at the
surface. But the ascription of such almost unlimited compressibility to
solid substances can be supported neither by experiment nor analogy.
Various considerations point to the probability that solid bodies yield
to pressure up to a certain limit and no farther, and that when this
limit is reached an increase in pressure is no longer attended with a
reduction in bulk.
If then we are compelled to reject the idea of the unlimited
compressibility of solid substances, we must conclude that the interior
portions of our globe are composed of _materials of a different kind_
from those which occur in its crust. And this conclusion, as we shall
presently see, is borne out by a number of independent facts.
The study of the materials ejected from volcanic vents proves that even
at very moderate depths there exist substances differing greatly in
density, as well as in chemical composition. The lightest lavas have a
specific gravity of 2·3, the heaviest of over 3. And that materials of
even greater density are sometimes brought by volcanic action from the
earth's interior, we have now the clearest proofs.
[Sidenote: RELATION BETWEEN EARTH AND OTHER PLANETS.]
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