The Richter magnitude scale is a measure of the strength of earthquakes. It was developed by Charles F. Richter and presented in his landmark 1935 paper. The scale was later revised and renamed the local magnitude scale, denoted as ML or ML. Most seismological authorities now use other scales to report earthquake magnitudes.
About Richter magnitude scale in brief

The magnitude of a given earthquake can be determined by the intensity of the shaking in that area, as well as the depth of the earthquake and the amount of water in the area at the time of the quake. It can also be calculated by comparing the shaking to a logarithmic scale, where each step represents a tenfold increase of magnitude, similar to the magnitude scale used by astronomers for star brightness. In 1956, Gutenberg and Richter labelled it ‘local magnitude’ with the symbol ML’ to distinguish it from two other scales they had developed, the surface wave magnitude and body wave magnitude scales. The MMS and MMS measure the energy released by an earthquake; another scale,. classifies their effects by their effect on their environment, but not noticeable to catastrophic to catastrophic, by their classifies them as ‘less noticeable’ or ‘more intense’ than Richter’s scale. The ‘MMS’ scale was replaced in the 1970s by the moment. magnitude scale ; for earthquakes measured for magnitude over Mw 8, they are frequently reported by the press as Richter magnitudes, even when they are not.
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This page is based on the article Richter magnitude scale published in Wikipedia (as of Jan. 03, 2021) and was automatically summarized using artificial intelligence.






