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A fault is a fracture or zone of fractures in the Earth's crust where rocks on either side have moved relative to each other. Faults can range in size from small fractures to large tectonic plate boundaries. They are classified based on the direction of movement and the type of stress that caused thRead more
A fault is a fracture or zone of fractures in the Earth’s crust where rocks on either side have moved relative to each other. Faults can range in size from small fractures to large tectonic plate boundaries. They are classified based on the direction of movement and the type of stress that caused the movement. The three main types of faults are normal faults, reverse faults, and strike-slip faults.
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