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If an Earthquake Has a Total Horizontal Displacement of S M=S2(12πtan1dD)M = \frac { S } { 2 } \left( 1 - \frac { 2 } { \pi } \tan ^ { - 1 } \frac { d } { D } \right)

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If an earthquake has a total horizontal displacement of S meters along its fault line, then the horizontal movement M of a point on the surface of Earth d kilometers from the fault line can be estimated using the formula M=S2(12πtan1dD) M = \frac { S } { 2 } \left( 1 - \frac { 2 } { \pi } \tan ^ { - 1 } \frac { d } { D } \right) where D is the depth (in kilometers) below the surface of the focal point of the earthquake. For the San Francisco earthquake of 1906, S was 4 meters and D was 3.08 kilometers. Approximate M for d = 6 kilometers. Round the answer to the nearest hundredth.


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