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Tectonic earthquakes occur at plate tectonic boundaries. Tectonic plates are constantly moving slowly, but sometimes friction between them causes them lock together and become unable to move. The rest of the plates carry on moving, which leads to increased pressure on the locked section. Eventually, the locked section succumbs to the pressure, and the plates move past each other rapidly. This movement causes a tectonic earthquake. The waves of released energy move through the Earth's crust and cause the shaking we feel at an earthquake site.A tectonic earthquake occurs where tectonic plates meet, an area known as the boundary. When two plates push into each other, they form a convergent plate boundary.



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