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The Richter scale [1] (/ ˈ r ɪ k t ər /), 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]
The original "body-wave magnitude" – mB or m B (uppercase "B") – was developed by Gutenberg 1945c and Gutenberg & Richter 1956 [25] to overcome the distance and magnitude limitations of the M L scale inherent in the use of surface waves. mB is based on the P and S waves, measured over a longer period, and does not saturate until around M 8.
To understand the magnitude scales based on M o detailed background of M wg and M w scales is given below. M w scale. Hiroo Kanamori [50] defined a magnitude scale (Log W 0 = 1.5 M w + 11.8, where W 0 is the minimum strain energy) for great earthquakes using Gutenberg Richter Eq. (1).
The earthquake, measuring 2.1ML on the Richter scale, hit Morvern in the Highlands just before 3.30pm. It was felt by islanders on Lismore, Inner Hebrides, and by villagers in Mallaig and Morar ...
Earthquakes of magnitude 8.0 and greater from 1900 to 2018. ... Unless otherwise noted, magnitudes are reported on the Moment magnitude scale (M w). Country/Territory
The following are examples of commonly used logarithmic scales, where a larger quantity results in a higher value: Richter magnitude scale and moment magnitude scale (MMS) for strength of earthquakes and movement in the Earth; A logarithmic scale makes it easy to compare values that cover a large range, such as in this map.
1979 Imperial Valley earthquake – magnitude 6.4 earthquake with an epicenter less than 1 km inside Mexico – significant damage and injuries on both sides of the border (60 in the US) 2010 Baja California earthquake (Mexico near S California) – magnitude 7.2 earthquake, 4 fatalities and 100 injuries, none in the United States
Seismic intensity scales categorize the intensity or severity of ground shaking (quaking) at a given location, such as resulting from an earthquake.They are distinguished from seismic magnitude scales, which measure the magnitude or overall strength of an earthquake, which may, or perhaps may not, cause perceptible shaking.