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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.
Earthquakes are rupturing processes in the Earths crust that lead to vibrations on the surface layer of the planet. Most of the damaging earthquakes so far have been tectonic in origin (tectonic quakes).
The location on the surface directly above the focus of an earthquake is called the epicenter.
The location below the earths surface where the earthquake starts is called the hypocenter, and the location directly above it on the surface of the earth is called the epicenter. Sometimes an earthquake has foreshocks. These are smaller earthquakes that happen in the same place as the larger earthquake that follows.
An earthquake is what happens when two blocks of the earth suddenly slip past one another. The surface where they slip is called the fault or fault plane.
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An earthquake is the sudden release of strain energy in the Earths crust, resulting in waves of shaking that radiate outwards from the earthquake source. When stresses in the crust exceed the strength of the rock, it breaks along lines of weakness, either a pre-existing or new fault plane.
Triangulation can be used to locate an earthquake. The seismometers are shown as green dots. The calculated distance from each seismometer to the earthquake is shown as a circle. The location where all the circles intersect is the location of the earthquake epicenter.
Earthquakes are highly destructive natural disasters, leading to significant loss of life and extensive damage to property on a global scale each year.

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