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
_Secondly._ Some physicists have asserted that a globe of liquid
matter radiating its heat into space, would tend to solidify both at
the surface and the centre, at the same time. The consequence of this
action would be the production of a sphere with a solid external shell
and a solid central nucleus, but with an interposed layer in a fluid
or semi-fluid condition. It has been pointed out that if we suppose
the solidification to have gone so far, as to have caused the partial
union of the interior nucleus and the external shell, we may conceive a
condition of things in which the stability and rigidity is sufficient
to satisfy both geologists and astronomers, but that in still
unsolidified pockets or reservoirs, filled with liquefied rock, between
the nucleus and the shell, we should have a competent cause for the
production of the volcanic phenomena of the globe. In this hypothesis,
however, it is assumed that the cooling at the centre and the surface
of the globe would go on at such rates that the reservoirs of liquid
material would be left at a moderate depth from the surface, so that
easy communication could be opened between them and volcanic vents.
[Sidenote: REVIEW OF THE SEVERAL HYPOTHESES.]
_Thirdly._ It has been maintained that the earth may have become
perfectly solid from the centre to the surface. Those who hold this
view endeavour to account for the phenomena of volcanoes in one of two
ways. It may be, they say, that the deep-seated rock-masses, though
actually solid, are in a state of _potential_ liquidity; that though
reduced to a solid state by the intense pressure of the superincumbent
masses, yet such is the condition of unstable equilibrium in the whole
mass, that the comparatively slight movements and changes taking place
at the earth's surface suffice to bring about the liquefaction of
portions of its crust and consequent manifestations of volcanic energy.
But It may be, as other supporters of the doctrine of the earth's
complete solidity have maintained, that the phenomena of volcanoes
have no direct connection with a supposed incandescent condition of
our planet at all, and that there are chemical and mechanical forces
at work within our globe which are quite competent to produce at the
surface all those remarkable phenomena which we identify with volcanic
action.
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