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seismic moment

geophysics
Also known as: M0

Quick Summary

The moment magnitude scale (MW) is a quantitative measure of an earthquake's size, developed to more accurately assess the total energy released. Unlike older scales like the Richter scale, which rely on seismic wave amplitudes, moment magnitude is tied to the earthquake's seismic moment (M0).12

The seismic moment is calculated using the fault's geometry and the displacement across its surface. Specifically, it's the product of the fault area, the average slip on the fault, and the rigidity of the rocks involved: M0 = DA\u03bc. This method avoids "magnitude saturation," allowing for reliable measurement of even the largest and most destructive earthquakes.1

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