Seismic wave, vibration generated by an earthquake, explosion, or similar energetic source and propagated within the Earth or along its surface. Seismic waves are produced by earthquakes in the Earth’s crust.

They usually result from an earthquake, volcanic eruption or other explosion. The diagram below is an example of the paths P-waves generated by an earthquake near Earth's surface would follow. As they travel through rock, the waves move tiny rock particles back and forth -- pushing them apart and then back together -- in line with the direction the wave is traveling.
Structure of the Earth. They can cause damage to structures on the Earth’s surface, as well as tsunamis. Earthquakes generate four principal types of elastic waves; two, known as body waves, travel within the Earth, whereas the other two, called surface Seismic waves can be distinguished by a number of properties including the speed the waves travel, ... We can solve these equations or an appropriate approximation to them to compute the paths that seismic waves follow in Earth. They can pass through solids, liquids and gases easily.

The Earth is almost a sphere.
Primary waves (or P waves) are the fastest moving waves, traveling at 1 to 5 miles per second (1.6 to 8 kilometers per second). Seismic waves. Seismic waves travel through the layers of the Earth.


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