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  2. San Andreas Fault - Wikipedia

    • The San Andreas Fault is a continental right-lateral strike-slip transform fault that extends roughly 1,200 kilometers (750 mi) through the U.S. state of California. It forms part of the tectonic boundary between the Pacific Plate and the North American Plate. Traditionally, for scientific purposes, the fault has been classified into three main segments (northern, central, and … See more

    Fault zones

    The northern segment of the fault runs from Hollister, through the Santa Cruz Mountains, epicenter of the
    The … See more

    Plate boundaries

    The Pacific Plate, to the west of the fault, is moving in a northwest direction while the North American Plate to the east is moving toward the southwest, but relatively southeast under the influence of plate tectonics. … See more

    Formation

    The San Andreas began to form in the mid Cenozoic about 30 Mya (million years ago). At this time, a spreading center between the Pacific Plate and the Farallon Plate (which is now mostly subducted, with remnants including the … See more

     
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  2. The San Andreas Fault is a major geological feature in California. Here are some key points about its history12345:
    • Born about 30 million years ago when the Pacific Plate and the North America plate first met.
    • First identified in 1895 by Professor Andrew Lawson of UC Berkeley.
    • Has horizontally slipped a total of about 300-350 km (186-220 mi) since it began moving.
    • Revealed by the 1906 San Francisco earthquake, establishing the concept of strike-slip movement on a major crustal fracture.
    Learn more:
    The San Andreas Fault was born about 30 million years ago in California, when the Pacific Plate and the North America plate first met. Before then, another oceanic plate, the Farallon plate, was disappearing beneath North America at a subduction zone, another type of plate boundary.
    www.livescience.com/45294-san-andreas-fault.html
    The SAF is about 28 million years old. It 'began' when the East Pacific Rise, the boundary between the Farallon and Pacific Plates, subducted under the North American Plate near what is now Los Angeles. Spreading northwest and southeast, The SAF gradually grew, and it still growing.
    sanandreasfault.org/Information.html
    The fault was first identified in 1895 by Professor Andrew Lawson of UC Berkeley. In the wake of the 1906 San Francisco earthquake, Lawson was tasked with deciphering the origin of the earthquake. He began by surveying and mapping offsets (such as fences or roads that had been sliced in half) along surface ruptures.
    en.wikipedia.org/wiki/San_Andreas_Fault
    Scientists have a good big picture understanding of the San Andreas Fault Zone (SAFZ). The SAFZ started moving about 28-30 million years ago and has horizontally slipped (transform motion) a total of about 300-350 km (186-220 mi) since it began moving.
    www.usgs.gov/programs/earthquake-hazards/scien…
    The long and active San Andreas fault was revealed by the San Francisco earthquake of 1906. Strike-slip movement on a major crustal fracture was first established by that event. The elastic rebound theory was developed in an analysis of this earthquake.
    pubs.geoscienceworld.org/gsa/gsabulletin/article-a…
     
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