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A seismic wave is identified by the way it moves and the order it comes in when an earthquake strikes. Primary waves (or P waves) are the first waves to arrive and move in an Accordion-like motion. Secondary waves (or S waves) come before the P waves and either move side to side and/or up and down. Surface waves are created when P and S waves reach the surface of the earth and produce the most destruction. They move like P and S waves, but the movements are magnified. They come after the S waves.

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