Final answer:
True. When two seismic stations receive data from an earthquake, the earthquake's location can be computed using the arrival times of P-waves, S-waves, and surface waves.
Step-by-step explanation:
True. When two seismic stations receive data from an earthquake, the earthquake's location can be computed using the arrival times of P-waves, S-waves, and surface waves.
Seismographs measure the time difference between the arrival of the P-wave and S-wave, which is used to determine the distance from the seismic stations to the earthquake's epicenter. By triangulating the distance from multiple seismic stations, the location of the earthquake can be determined.