A seismograph is used to measure
the vibrations of the earth and to locate the source of earth vibrations.
Phenomena capable of being detected by a seismograph include earthquakes,
volcanic eruptions, explosions such as bombs, powerful winds, violent storms
at sea and even, in urban areas, traffic.
Thanks to the seismograph whole
populations can be warned and prepared for a variety of natural disasters.
Seismic observatories around the world, have provided information increasing
our knowledge of the earth's structure.
The
seismograph operates on one of two basically simple mechanisms which are
devices responsive to strain and pendulums. The earliest form of seismograph
known was been used to measure the thickness
of the ice sheets covering the polar regions of the earth and, when used in
conjunction with artificial explosions created under special test conditions,
seismographs can help geologists trace oil fields.
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