The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
History
The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
Astronomy; Earth (Planet); Natural history
At many volcanic vents the eruptive energy manifests itself with
more or less regularity. At Stromboli, which is constantly in an
active state, the explosions occur at intervals varying from three or
four to ten minutes and upward. A similar rhythmical movement has
been often observed during the eruptions at other vents which are
not constantly active. Volcano, for example, during its eruption of
September, 1873, displayed a succession of explosions which followed
each other at intervals of from twenty to thirty minutes. At Etna and
Vesuvius a similar rhythmical series of convulsive efforts has often
been observed during the course of an eruption. Among the volcanoes
of the Andes a periodic discharge of steam has been observed; Mr.
Whymper noticed outrushes of steam to proceed at intervals of from
twenty to thirty minutes from the summit of Sangai, while during his
inspection of the great crater of Cotopaxi, this volcano was seen to
blow off steam at intervals of about half an hour. At the eruption of
the Japanese volcano, Oshima, in 1877, Mr. Milne observed that the
explosions occurred nearly every two seconds, with occasional pauses
of 15 or 20 seconds. Kilauea, in Hawaii, seems to show a regular
system of grand eruptive periods. Dana has pointed out that outbreaks
of lava have taken place from that volcano at intervals of from eight
to nine years, this being the time required to fill the crater up to
the point of outbreak, or to a depth of 400 or 500 feet.
The approach of an eruption is not always indicated by any
premonitory symptoms, for many tremendous explosions are recorded to
have taken place in different parts of the world without perceptible
warning. Much in this respect would appear to depend upon the
condition of liquidity of the lava, and the amount of resistance
offered by it to the passage of the escaping vapors through its mass.
In Hawaii, where the lavas are remarkably liquid, vast outpourings of
them have taken place quietly without earthquakes during the present
century. But even there the great eruption of 1868 was accompanied by
violent earthquakes.
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