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High Quality Content by WIKIPEDIA articles! High Quality Content by WIKIPEDIA articles! The San Andreas Fault is a continental transform fault that runs a length of roughly 800 miles (1,300 km) through California in the United States, and through Baja California in Mexico. The fault's motion is right-lateral strike-slip (horizontal motion). It forms the tectonic boundary between the Pacific Plate and the North American Plate. The fault was first identified in Northern California by UC Berkeley geology professor Andrew Lawson in 1895 and named by him after a small lake which lies in a linear…mehr

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High Quality Content by WIKIPEDIA articles! High Quality Content by WIKIPEDIA articles! The San Andreas Fault is a continental transform fault that runs a length of roughly 800 miles (1,300 km) through California in the United States, and through Baja California in Mexico. The fault's motion is right-lateral strike-slip (horizontal motion). It forms the tectonic boundary between the Pacific Plate and the North American Plate. The fault was first identified in Northern California by UC Berkeley geology professor Andrew Lawson in 1895 and named by him after a small lake which lies in a linear valley formed by the fault just south of San Francisco, the Laguna de San Andreas. After the 1906 San Francisco Earthquake, Lawson also discovered that the San Andreas Fault stretched southward into Southern California.