Earth Features and Their Meaning: An Introduction to Geology for the Student and the General ReaderHobbs, William Herbert
Science
Earth Features and Their Meaning: An Introduction to Geology for the Student and the General Reader
Hobbs, William Herbert
Geology; Physical geography
During the grander or catastrophic earthquakes, the changes are
indeed terrifying, and have usually been accompanied by losses to
life and property, which are only to be compared with those of great
conflagrations or of inundations on thickly populated plains. The
conflagration has all too frequently been an aftermath of the great
historic earthquakes. The earthquake of December 28, 1908, in southern
Italy, destroyed almost the entire population of a great city, and left
of its massive buildings only a confused heap of rubble (Fig. 49). Two
years later a heavy earthquake resulted in great damage to cities in
Costa Rica (Fig. 50), while two years earlier our own country was first
really awakened to the danger in which it stands from these convulsive
earth throes; though, as we shall see, these dangers can be largely met
through proper methods of construction.
[Illustration:
FIG. 50.—Ruins of the Carnegie Palace of Peace at Cartago, Costa Rica,
destroyed when almost completed by the great earthquake of May 4, 1910
(after a photograph by Rear-Admiral Singer, U.S.N.).]
Earthquakes are usually preceded for a brief instant by subterranean
rumblings whose intensity appears to bear no relation to the shocks
which follow. The ground then rocks in wavelike motions, which, if of
large amplitude, may induce nausea, prevent animals from keeping upon
their feet, and wreck all structures not specially adapted to withstand
them. Heavy bodies are sometimes thrown up from the ground (Fig. 51),
and at other times similar heavy masses are, apparently because of
their inertia, more deeply imbedded in the earth. Thus gravestones and
heavy stone posts are often sunk more deeply in the ground and are
surrounded by a hollow and perhaps by small open cracks in the surface
(Fig. 52). When bodies are thrown upward, it would imply that a quick
upward movement of the ground had been suddenly arrested, while the
burial of heavy bodies in the earth is probably due to a movement which
begins suddenly and is less abruptly terminated.
[Illustration: FIG. 51.—Bowlders thrown into the air and overturned
during the Assam earthquake of 1897 (after R. D. Oldham).]
[Illustration:
FIG. 52.—Heavy post sunk deeper into the ground during the Charleston
earthquake of August 31, 1886 (after Dutton).]
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