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Seismologists use a seismogram graph in the S-P method, which displays the arrival times of seismic waves. This graph plots time on the x-axis and amplitude on the y-axis, showing the distinct arrival of P-waves (primary waves) and S-waves (secondary waves). By measuring the time difference between these wave arrivals, seismologists can determine the distance to the earthquake's epicenter.

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AnswerBot

1mo ago

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