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The Richter scale [1] (/ ˈ r ɪ k t É™r /), also called the Richter magnitude scale, Richter's magnitude scale, and the Gutenberg–Richter scale, [2] is a measure of the strength of earthquakes, developed by Charles Richter in collaboration with Beno Gutenberg, and presented in Richter's landmark 1935 paper, where he called it the "magnitude scale". [3]
Second, Richter arbitrarily defined the zero point of the scale to be where an earthquake at a distance of 100 km makes a maximum horizontal displacement of 0.001 millimeters (1 μm, or 0.00004 in.) on a seismogram recorded with a Wood-Anderson torsion seismograph. [14]
The relationship between earthquake magnitude and frequency was first proposed by Charles Francis Richter and Beno Gutenberg in a 1944 paper studying earthquakes in California, [2] [3] and generalised in a worldwide study in 1949. [4]
In two most recent investigations using statistically stable samples for Italian earthquakes (approximately 100,000 events over the period 1981–2002 in the Richter local [M L ] magnitude range of 3.5–5.8) [5] and for Indian earthquakes exemplified by an aftershock sequence of 121 events with M s (surface wave magnitude) > 4.0 in 2001 in the Bhuj area of northwestern India, [4] the latest ...
A pie chart comparing the seismic moment release of the three largest earthquakes for the hundred-year period from 1906 to 2005 with that for all earthquakes of magnitudes <6, 6 to 7, 7 to 8, and >8 for the same period. The 2011 Japan quake would be roughly similar to Sumatra.
M L Richter scale M s Surface-wave magnitude scale M n Nuttli magnitude scale—a version of the Richter scale specifically for use in eastern North America [ 22 ]
Two scales were developed, one based on surface waves, , and one on body waves, . Surface waves with a period near 20 s generally produce the largest amplitudes on a standard long-period seismograph, and so the amplitude of these waves is used to determine M s {\displaystyle M_{s}} , using an equation similar to that used for M L {\displaystyle ...
M L This is the only deadly Australian earthquake recorded to date – February 8, 1990 15:15 local time Bohol Sea, Philippines; see 1990 Bohol Sea earthquake. 9.755 124.694 6 6.8 M w [90] [91] June 14, 1990: 15:41 local time Panay Island, Philippines see 1990 Panay earthquake: 11.34 122.10 8 7.1 M w – June 21, 1990: 00:30 local time
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