An instrumental earthquake magnitude scale

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 .