Elastic rebound is the process by which rocks store energy that eventually releases as an earthquake.
The incidence of earthquakes is explained by the elastic-rebound theory. Earthquakes are produced when bending rocks fail and release their stored stress energy. In geology, the study of how energy is released following an earthquake is known as elastic-rebound theory. Along the fault line, the crust ruptures; the quick motion releases the built-up energy, and the rocks almost immediately return to their previous shape. Elastic rebound is the ability of the deformed rock to restore its original shape in a new position as a result of the slide along a fault (i.e., earthquake). Elastic rebound describes the process by which a rock that has been deformed by an earthquake's sliding along a fault can return to its former shape.
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