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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]
All magnitude scales retain the logarithmic scale as devised by Charles Richter, and are adjusted so the mid-range approximately correlates with the original "Richter" scale. [8] Most magnitude scales are based on measurements of only part of an earthquake's seismic wave-train, and therefore are incomplete.
This scale is also known as the Richter scale, but news media sometimes use that term indiscriminately to refer to other similar scales.) The local magnitude scale was developed on the basis of shallow (~15 km (9 mi) deep), moderate-sized earthquakes at a distance of approximately 100 to 600 km (62 to 373 mi), conditions where the surface waves ...
The 1906 earthquake preceded the development of the Richter scale by three decades. The most widely accepted estimate for the magnitude of the quake on the modern moment magnitude scale is 7.9; [1] values from 7.7 to as high as 8.3 have been proposed. [8]
New models show a generalization of the original Gutenberg–Richter model. Among these is the one released by Oscar Sotolongo-Costa and A. Posadas in 2004, [14] of which R. Silva et al. presented the following modified form in 2006, [15]
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 ...
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.
Earthquakes (6.0+ M w) between 1900 and 2017 Earthquakes are caused by movements within the Earth's crust and uppermost mantle.They range from weak events detectable only by seismometers, to sudden and violent events lasting many minutes which have caused some of the greatest disasters in human history.