The Life of Sir Humphry Davy, Bart. LL.D., Volume 2 (of 2)Paris, John Ayrton
History
The Life of Sir Humphry Davy, Bart. LL.D., Volume 2 (of 2)
Paris, John Ayrton
Chemists -- England -- Biography; Davy, Humphry, Sir, 1778-1829
"If the idea of Lemery were correct, that the action of sulphur on
iron may be a cause of volcanic fires, sulphate of iron ought to
be the great product of the volcano; which is known not to be the
case; and the heat produced by the action of sulphur on the common
metals is quite inadequate to account for the appearances. When
it is considered that volcanic fires occur and intermit with all
the phenomena that indicate intense chemical action, it seems not
unreasonable to refer them to chemical causes. But for phenomena
upon such a scale, an immense mass of matter must be in activity,
and the products of the volcano ought to give an idea of the
nature of the substances primarily active. Now, what are these
products? Mixtures of the earths in an oxidated and fused state,
and intensely ignited; water and saline substances, such as might
be furnished by the sea and air, altered in such a manner as might
be expected from the formation of fixed oxidated matter. But it may
be said, if the oxidation of the metals of the earths be the causes
of the phenomena, some of these substances ought occasionally to
be found in the lava, or the combustion ought to be increased
at the moment the materials passed into the atmosphere. But the
reply to this objection is, that it is evident that the changes
which occasion volcanic fires take place in immense subterranean
cavities; and that the access of air to the acting substances
occurs long before they reach the exterior surface.
"There is no question but that the ground under the solfaterra
is hollow; and there is scarcely any reason to doubt of a
subterraneous communication between this crater and that of
Vesuvius: whenever Vesuvius is in an active state, the solfaterra
is comparatively tranquil. I examined the bocca of the solfaterra
on the 21st of February 1820, two days before the activity of
Vesuvius was at its height: the columns of steam which usually
arise in large quantities when Vesuvius is tranquil, were now
scarcely visible, and a piece of paper thrown into the aperture
did not rise again; so that there was every reason to suppose
the existence of a descending current of air. The subterraneous
thunder heard at such great distances under Vesuvius is almost a
demonstration of the existence of great cavities below filled with
aëriform matter: and the same excavations which, in the active
state of the volcano, throw out, during so great a length of time,
immense volumes of steam, must, there is every reason to believe,
in its quiet state, become filled with atmospheric air.[115]
[115] "Vesuvius is a mountain admirably fitted, from its form and
situation, for experiments on the effect of its attraction on
the pendulum: and it would be easy in this way to determine the
problem of its cavities. On Etna the problem might be solved on a
larger scale."
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