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Published October 1948 | Published
Journal Article Open

Minimal recorded earthquakes

Abstract

The magnitude of an earthquake was originally defined (Richter, 1935) as the common logarithm of the maximum displacement, expressed in microns, of the trace written by a standard torsion seismometer at an epicentral distance of 100 kilometers. When this trace amplitude is one micron the magnitude is accordingly zero.

Additional Information

Copyright © 1948, by the Seismological Society of America. Manuscript received for publication March 3, 1948.

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Created:
August 19, 2023
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October 26, 2023