The Boy Travellers in the Far East, Part Third: Adventures of Two Youths in a Journey to Ceylon and India; With Descriptions of Borneo, the Philippine Islands and BurmahKnox, Thomas Wallace
General
The Boy Travellers in the Far East, Part Third: Adventures of Two Youths in a Journey to Ceylon and India; With Descriptions of Borneo, the Philippine Islands and Burmah
Knox, Thomas Wallace
East Indies -- Description and travel -- Juvenile literature
Frank asked the Doctor what was the cause of an earthquake, and whether
the movements of the ground were always the same.
"The cause is difficult to get at," Doctor Bronson answered, "although
the wisest men in all ages have studied the phenomenon, and endeavored
to make a satisfactory theory for it. The ancient philosophers supposed
that the winds became imprisoned in the earth, and, in their struggles
to escape, gave rise to the upheaval of the land and the general
convulsions. In the last century a French scientist contended that large
quantities of bituminous and sulphurous matter became suddenly inflamed,
and broke forth in violent fermentations. The still more modern theory
is that the surface of the earth is only a thin crust over a mass of
melted matter; that we live on the outside of a ball of liquid fire,
which is liable to explode at any time, and put an end to us and all
around. It is argued that the volcanoes now in activity are the outlets
for this internal fire, and the occasional eruptions and earthquakes
are the result of the fire seeking vent, in consequence of the clogging
of the subterranean passages."
Frank thought the theory was not very comforting, and on the whole he
preferred the older one. Fred agreed with him, and then the Doctor
continued:
"The movements of the ground are not always the same in earthquakes;
sometimes there will be only a single shock, or more frequently two
about twenty seconds or even a minute apart, and again there will be a
succession of shocks lasting for hours, or even days, at irregular
intervals. The latter is oftener the case in South America than in other
parts of the world; there the ground keeps up a rocking more or less
continual for hours, and the later shocks are generally more violent
than the earlier ones. Usually, however, the earthquake comes without
warning, and is over in less than a minute, but in that space of time
the destruction may be terrible.
[Illustration: DESTRUCTION OF MESSINA IN 1783.]
Public-domain text, read in full here on John Shaqi.
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