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The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earths crust and cause the shaking that we feel.
seismology, scientific discipline that is concerned with the study of earthquakes and of the propagation of seismic waves within the Earth. A branch of geophysics, it has provided much information about the composition and state of the planets interior.
earthquake. / rthkwāk / A sudden movement of the Earths lithosphere (its crust and upper mantle). Earthquakes are caused by the release of built-up stress within rocks along geologic faults or by the movement of magma in volcanic areas. They are usually followed by aftershocks.
Earthquakes are usually caused when underground rock suddenly breaks and there is rapid motion along a fault. This sudden release of energy causes the seismic waves that make the ground shake.
Earthquakes are the result of sudden movement along faults within the Earth. The movement releases stored-up elastic strain energy in the form of seismic waves, which propagate through the Earth and cause the ground surface to shake.
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earthquake, any sudden shaking of the ground caused by the passage of seismic waves through Earths rocks. Seismic waves are produced when some form of energy stored in Earths crust is suddenly released, usually when masses of rock straining against one another suddenly fracture and slip.

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