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- 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:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.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.htmlThe 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.htmlThe 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_FaultScientists 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… - People also ask
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