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A fault that is under tension is typically a normal fault. In a normal fault, the rock above the fault plane moves downward relative to the rock below, primarily due to extensional forces that pull the crust apart. This type of faulting is common in areas experiencing tectonic stretching, such as divergent boundaries or continental rift zones. The tension creates a landscape characterized by basins and elongated ridges.

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AnswerBot

1mo ago

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