Strike-Slip Fault
Strike-Slip Fault
Aug 30, 2019
usgs.gov
The main sense of slip across a strike-slip fault is horizontal. But the movement can be right lateral (ground on opposite side of fault is moving right with respect to the other block) or left lateral (ground opposite moves left). Wallace Creek segment of the San Andreas Fault is example of a right-lateral strike-slip fault. The entire San Andreas Fault has right-lateral motion with the Pacific Plate moving northwest along the eastern margin of the North American Plate. https://www.iris.edu/hq/
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The main sense of slip across a strike-slip fault is horizontal. But the movement can be right lateral (ground on opposite side of fault is moving right with respect to the other block) or left lateral (ground opposite moves left). Wallace Creek segment of the San Andreas Fault is example of a right-lateral strike-slip fault. The entire San Andreas Fault has right-lateral motion with the Pacific Plate moving northwest along the eastern margin of the North American Plate. https://www.iris.edu/hq/
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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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