The San Andreas Fault is a famous tectonic feature in California known as a site of plate slippage. It is classified as a transform fault, where two tectonic plates move horizontally past each other. This movement often leads to significant seismic activity, including earthquakes. ;
The San Andreas Fault is known as a site of plate slippage, specifically as a transform fault where two tectonic plates move horizontally past each other, causing significant seismic activity. This fault is critical in understanding earthquake dynamics in California.
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