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Fluids (gases and liquids) cannot transmit P waves.

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Earthquake waves that travel through Earth's interior are called body waves.

Earthquake body waves are divided into two types called primary (P) waves and secondary (S) waves.

Most earthquakes are produced by the rapid release of elastic energy stored in rock that has been subjected to great stress.

In 1935, Charles Richter, a California seismologist, devised a simple procedure that is now used throughout the world to measure the size of an earthquake, the Richter Magnitude.