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Strike-slip faults are a type of tectonic boundary where two blocks of Earth’s crust move horizontally past one another, rather than pulling apart or colliding. The motion is lateral - side-to-side - driven by stress that builds up over years or centuries and is released suddenly during an earthquake. In most earthquakes, this movement occurs below the surface, along a fault plane that may be several miles deep. Even when the ground above shakes violently, the surface itself often remains intact
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