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When an earthquake occurs, seismologists create graphics of focal mechanisms, informally referred to as beach balls, to show the faulting motions that produce the earthquake. The focal mechanisms are based on the direction of the first arriving P wave. Lets investigate the patterns of P-wave arrivals that result from different faulting mechanisms by first considering a strike-slip earthquake. When an earthquake occurs, seismic waves radiate away from the epicenter in all directions. The parallel green lines in the northwest and southeast quadrants have been compressed during the earthquake and the Northeast and southwest quads were stretched. This applies also to vertical faults. Lets look at the Pwaves moving away from the epicenter. We will inset slinkies to demonstrate and exaggerate the compression/dilatation features. Northwest and Southeast of the epicenter the rock is compressed and the first arriving P waves at those stations are pushes away from the epicenter. Northeast and S