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The scale was replaced in the 1970s by the moment magnitude scale (MMS, symbol Mw ); for earthquakes adequately measured by the Richter scale, numerical values are approximately the same.
The Richter scale measures the largest wiggle (amplitude) on the recording, but other magnitude scales measure different parts of the earthquake. The USGS currently reports earthquake magnitudes using the Moment Magnitude scale, though many other magnitudes are calculated for research and comparison purposes.
The first widely-used method, the Richter scale, was developed by Charles F. Richter in 1934. It used a formula based on the amplitude of the largest wave recorded on a specific type of seismometer and the distance between the earthquake and the seismometer.
The Modified Mercalli Intensity (MMI) Scale assigns intensities as Although numerous intensity scales have been developed over the last several hundred years to evaluate the effects of earthquakes, the one currently used in the United States is the Modified Mercalli Intensity (MMI) Scale.
Richter scale (ML), quantitative measure of an earthquakes magnitude (size), devised in 1935 by American seismologists Charles F. Richter and Beno Gutenberg. The earthquakes magnitude is determined using the logarithm of the amplitude (height) of the largest seismic wave calibrated to a scale by a seismograph.