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These P waves are able to travel through both solid rock, such as granite mountains, and liquid material, such as volcanic magma or the water of the oceans. The slower wave auspices of the body of sway is called the unessential or S wave. As an S wave propagates, it shears the bankrupt sideways at right angles to the direction of travel.
If a is sheared sideways or twisted, it will not spring back, hence S waves cannot propagate in the liquid parts of the earth, such as oceans and lakes.
The actual speed of P and S seismic waves depends on the density and elastic properties of the rocks and blot through which they pass. In most earthquakes, the P waves are felt first. The effect is similar to a sonic boom that bumps and rattles windows. Some anothers later, the S waves arrive with their up-and-down and side-to-side motion, shaking the ground surface vertically and horizontally.
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