San Andreas Fault

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The San Andreas Fault is a continental transform fault that extends roughly 1,200 kilometers (750 mi) through California . [1] It forms the tectonic boundary between the Pacific Plate and the North American Plate , and its motion is right-lateral strike-slip (horizontal). The fault divides into three segments, each with different characteristics and a different degree of earthquake risk. The slip rate along the fault ranges from 20 to 35 mm (0.79 to 1.38 in)/yr. [1]


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