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When the rocks finally give way and slip, this sudden movement generates seismic waves. There are several types of seismic waves, but the two main ones are **P-waves** (primary waves) and **S-waves** (secondary waves). P-waves are the fastest and can travel through solids, liquids, and gases. S-waves are slower and can only travel through solids. By analyzing the arrival times of these waves at different seismograph stations, scientists can pinpoint the location and magnitude of an earthquake.
