The San Andreas Fault is an example of a strike-slip fault.
Two blocks gliding past one another on a fault plane is called a strike-slip fault. A right lateral fault is exemplified by the San Andreas Fault. When viewed from either side, a right-lateral strike-slip fault has the far block displaced to the right.
A fault is a crack or region of cracks that separate two rock blocks.
A dip-slip fault known as a normal fault occurs when the block above the fault has slid lower in relation to the block below. Reverse (thrust) faults are dip-slip faults in which the higher block travels up and over the lower block above the fault plane. This kind of faulting frequently occurs in compressed areas.
To learn more about geologic faults:
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