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
By some other theorists, who have felt the full force of this last
objection, an attempt has been made to explain the phenomena of
volcanoes by supposing that the globe is solid from its surface to its
centre, but that the internal portions of the globe are at such a high
temperature that they are only retained in a solid condition by the
enormous pressure to which they are subjected. The central masses of
the globe are thus regarded as being in an _actually_ solid, but in a
_potentially_ liquid condition, and any local relief of pressure is at
once followed by the conversion of solid to liquefied materials, in the
district where the relief takes place, resulting in the manifestation
of volcanic phenomena at the spot. It may be granted that this
hypothesis better accords with the known facts of Vulcanology than any
of those which we have previously described, but it is impossible to
shut our eyes to the fact that not a few serious difficulties still
remain. Thus it is based upon the assumption that the law of the
elevation of the point of fusion by pressure is true at temperatures
and pressures almost infinitely above those at which we are able to
conduct observations; but neither experiment nor analogy warrant this
conclusion, for the former shows that the elevation of the point of
fusion by pressure goes on in a continually diminishing ratio, and the
latter famishes us with the example of volatile liquids which, above
their critical points, obstinately remain in a gaseous condition under
the highest pressures. Nor is it easy upon this hypothesis to account
for the very irregular distribution of temperatures within the earth's
crust, as demonstrated by observations in mines, wells, and borings.
The hypothesis further requires the assumption that, at such very
moderate depths as are required for the reservoirs of volcanoes, the
effects of pressure and temperature on the condition of rock-materials
are so nicely balanced that the smallest changes at the surface lead to
a disturbance of the equilibrium.
[Sidenote: DIFFICULTIES NOT YET EXPLAINED.]
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