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Faults
Fractures in the Earth's crust along which there has been significant displacement as a result of rock-mass movement.
Beds
Horizontal layers of sedimentary rock that display a planar or nearly planar bedding surface, indicating periods of deposition over time.
Strike-Slip Fault
A fault in which the relative movement is essentially horizontal, parallel to the strike of the fault surface.
Normal Fault
A fault in which the hanging wall moves down relative to the footwall.
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