An instrumental earthquake magnitude scale
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In the course of historical or statistical study of earthquakes in any
given region it is frequently desirable to have a scale for rating these
shocks in terms of their original energy, independently of the effects
which may be produced at any particular point of observation. On the
suggestion of Mr. H. O. Wood, it is here proposed to refer to such a
scale as a "magnitude" scale. This terminology is offered in distinction
from the name "intensity" scale, now in general use for such scales as
the Rossi-Forel and Mercalli-Cancani scales, which refer primarily to the
local intensity of shock manifestation.
[1] H. O. Wood. Concerning the perceptibility of weak earthquakes and their dynamical measurement , 1914, Bulletin of the Seismological Society of America.
[2] R. Oldham. The Depth of Origin of Earthquakes , 1926, Quarterly Journal of the Geological Society of London.
[3] C. Richter,et al. Recent earthquakes near Whittier, California , 1931 .
[4] B. Gutenberg,et al. The earthquake in Santa Monica Bay, California, on August 30, 1930 , 1932 .