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Turkey cooking time what is an earthquake diagram. The richter scale also called the richter magnitude scale or richters magnitude scale is a measure of the strength of earthquakes developed by charles f. Earthquakes below magnitude 75 seldom cause tsunamis. From 1935 until 1970 the earthquake magnitude scale was the richter scale a mathematical formula invented by caltech seismologist charles richter to compare quake sizes.
The scientific study of earthquakes is called seismology. This was later revised and renamed the local magnitude scale denoted as ml or m l. The largest known quake in the united states struck prince william sound alaska on march 28 1964 and measured magnitude 92.
The richter scale m l is what most people have heard about but in practice it is not commonly used anymore except for small earthquakes recorded locally for which ml and short period surface wave magnitude mblg are the only magnitudes that can be measured. Richter and presented in his landmark 1935 paper where he called it the magnitude scale. Understanding plate tectonics helps to explain the cause.
The types and nature of these waves are described in the section seismic wavesbecause the size of earthquakes varies enormously it is necessary for purposes of comparison to compress the range of wave amplitudes. For all other earthquakes the moment magnitude mw scale is a more accurate measure of the earthquake size. Magnitude is the most common measure of an earthquakes size according to the usgs.
It is used for observations near the earthquake epicentre where the. Surface wave magnitude ms is based on the maximum amplitude of the surface wave having a period of 20 2 s. A submarine undersea or underwater earthquake is an earthquake that occurs underwater at the bottom of a body of water especially an oceanthey are the leading cause of tsunamisthe magnitude can be measured scientifically by the use of the moment magnitude scale and the intensity can be assigned using the mercalli intensity scale.
Earthquake magnitude is a measure of the size or amplitude of the seismic waves generated by an earthquake source and recorded by seismographs. Usually not felt but can be recorded by seismograph. Often felt but.
Estimated number each year. Because of various shortcomings of the m l scale most.