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It was only
in the 1930's that Charles F. Richter, a
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California
seismologist, introduced the concept
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of earthquake
magnitude.
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His original
definition held only for California
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earthquakes
occurring within 600 km of a
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particular
type of seismograph (the Woods-
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Anderson
torsion instrument).
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Richter's
original magnitude scale (ML) was then
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extended to
observations of earthquakes of any
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distance and
of focal depths ranging between 0
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and 700 km.
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