Description

The Moment Magnitude Scale (MMS) has superceded the Richter Scale (RS) to describe the energy release during an earthquake. It is based on the seismic "moment" of the earthquake. It was developed in 1979 by Hanks and Kanamori at the California Institute of Technology.


 

If the seismic moment is known in dyne•centimeters:

 

MMS =

= (0.667 * LOG10(moment in dyne•cm)) - 10.7

 

where:

• The seismic moment values are very, very large.

• A dyne•centimeter is 0.0000001 Newton•meter (10^(-7))

 

When comparing 2 earthquakes, the difference in energy between the 2 is:

 

energy in MMS2 vs MMS1 =

= 10^((1.5 * MMS2) - (1.5 * (MMS)))

 

Limitations:

• The MMS is better than the Richter scale for describing large earthquakes. The MMS and Richer scale are comparable for moderate earthquakes.

• The MMS has problems with small earthquakes and is not used for earthquakes with a magnitude < 3.5 RS.

 


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