Earthquakes are violent shaking from the planet's surface, according to AccuWeather. They're caused by movement from Earth's outermost layer, the crust.
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The crust is broken up into pieces called tectonic plates that are always on the move, though usually in ways we cannot feel. When the plates hit a roadblock, stress builds and leads to cracks in the Earth called faults.
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In time, the energy from within builds to the breaking point. That sudden release leads to an earthquake.
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The shaking begins at a central region called the epicenter and spreads far and wide. An earthquake can then be followed by additional shaking known as an aftershock.
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