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A reverse fault is a type of geological fault where the hanging wall moves upward relative to the footwall, typically due to compressional forces. This movement occurs at a steeper angle, often between 30 to 70 degrees. Reverse faults are commonly found in mountainous regions and are associated with convergent tectonic plate boundaries. They can lead to significant geological features, such as thrust faults, and are important in understanding seismic activity and earthquake risks in affected areas.

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AnswerBot

1mo ago

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