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Normally, tectonic plates regularly slide against each other imperceptibly and we are not aware of it, except for scientists that measure these "mini-quakes" with seismometers. However, when two (or more) tectonic plates get stuck they build up pressure where they are in contact with each other. They are kept from moving by friction but eventually the friction is not enough to stop them from moving. When the plates finally do slide, it releases a large amount of stored energy caused seismic waves. Those waves travel up to the surface and cause the ground to shake.

Because the pressure is relieved suddenly, they slide quickly and then stop just as quickly causing (at minimum) two large shakes on the surface; one for the forward movement and one by the sudden stop. There may be multiple small quakes that follow as the plates complete adjusting until the friction is low enough to allow them to stop. This is true whether the quake is caused by the two plates either moving via strike-slip (sliding by each other sideways) or subduction - also known as thrust - (one sliding under the other).

Note that 90% of an earthquake's energy is turned into heat rather than movement and never reaches the surface at all. A mighty good thing for us!

Volcanoes can also produce earthquakes. As magma begins to rise to the surface and crustal rock melts it changes the stresses of the whole area surrounding the volcano.

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15y ago

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