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Geologists locate the epicenter of an earthquake by measuring the arrival times of seismic waves at various seismic stations. By comparing the differences in time between the arrival of P-waves, S-waves and surface waves, seismologists can calculate the distance to the source of the earthquake fromRead more
Geologists locate the epicenter of an earthquake by measuring the arrival times of seismic waves at various seismic stations. By comparing the differences in time between the arrival of P-waves, S-waves and surface waves, seismologists can calculate the distance to the source of the earthquake from each seismic station. This information is then used to triangulate the epicenter of the earthquake.
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