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Richter scale: Difference between revisions

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:<math display="block">M_\mathrm{L} = \log_{10} A - \log_{10} A_\mathrm{0}(\delta) = \log_{10} [A / A_\mathrm{0}(\delta)],\ </math>
 
where {{mvar|A}} is the maximum excursion of the Wood–Anderson[[Wood-Anderson seismograph]], the empirical function {{mvar|A<sub>0</sub>}} depends only on the [[epicentral distance]] of the station, <math>\delta</math>. In practice, readings from all observing stations are averaged after adjustment with station-specific corrections to obtain the {{M|L}} value.<ref name="Ellsworth" />
Because of the logarithmic basis of the scale, each whole number increase in magnitude represents a tenfold increase in measured amplitude; in terms of energy, each whole number increase corresponds to an increase of about 31.6 times the amount of energy released, and each increase of 0.2 corresponds to approximately a doubling of the energy released.