Fault friction refers to the frictional resistance that occurs along a fault plane, which is a surface where two blocks of the Earth's crust have moved relative to each other. This concept is crucial in understanding the mechanics of earthquakes and fault movement. When stress builds up in the Earth's crust due to tectonic forces, it can eventually exceed the frictional strength of the rocks along a fault, leading to slippage and, ultimately, an earthquake.
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