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
If, however, careful and exact observations, like those carried on
at Stromboli, compel us to reject the popular notions concerning
the supposed resemblance between volcanic action and the combustion
of sulphur or other substances, they nevertheless suggest analogies
with certain other simple and well-known operations. And in pursuing
these analogies, we are led to the recognition of some admirable
illustrations both of the attendant phenomena and of the true cause of
volcanic outbursts.
No one can look down on the mass of seething material in violent
agitation within the fissures at the bottom of the crater of Stromboli,
without being forcibly reminded of the appearances presented by liquids
in a state of boiling or ebullition. The glowing material seems to be
agitated by two kinds of movements, the one whirling or rotatory, the
other vertical or up-and-down in its direction. The fluid mass in this
way appears to be gradually impelled upwards, till it approaches the
lips of the aperture, when vast bubbles are formed upon its surface,
and to the sudden bursting of these the phenomena of the eruption are
due.
Now if we take a tall narrow vessel and fill it with porridge or
some similar substance of imperfect fluidity, we shall be able, by
placing it over a fire, to imitate very closely indeed the appearances
presented in the crater of Stromboli. As the temperature of the mass
rises, steam is generated within it, and in the efforts of this steam
to escape, the substance is set in violent movement. These movements of
the mass are partly rotatory and partly vertical in their direction; as
fresh steam is generated in the mass its surface is gradually raised,
while an escape of the steam is immediately followed by a fall of the
surface. Thus an up-and-down movement of the liquid is maintained, but
as the generation of steam goes on faster than it can escape through
the viscid mass, there is a constant tendency in the latter to rise
towards the mouth of the vessel. At last, as we know, if heat continues
to be applied to the vessel, the fluid contents will be forced up to
its edge and a catastrophe will occur; the steam being suddenly and
violently liberated from the bubbles formed on the surface of the mass,
and a considerable quantity of the material forcibly expelled from
the vessel. The suddenness and violence of this catastrophe is easily
accounted for, if we bear in mind that the escaping steam acts after
the manner of a compressed spring which is suddenly released. Steam
is first formed at the bottom of the vessel which is in contact with
the fire; but here it is under the pressure of the whole mass of the
liquid, and moreover, the viscidity of the substance tends to retard
the union of the steam bubbles and their rise to the surface of the
mass. But when the pressure is relieved by the bursting of bubbles at
the surface, the whole of the generated steam tends to escape suddenly.
[Sidenote: ESCAPE OF STEAM-BUBBLES FROM LAVA.]
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