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In 1870s the
English geologist John Milne designed
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a forerunner of modern
seismographs.
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A simple
pendulum and a needle suspended above
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a smoked-glass
plate allowed to distinguish
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primary and
secondary earthquake waves and,
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basing on
their timing, to derive an accurate
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statement
about location of an earthquake source.
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The modern
seismograph was invented in the early
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20th
century by the Russian Prince Boris Golitzyn,
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who improved
similar instruments of the 1890's.
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