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Bajadas are formed when sediment is eroded and carried downstream by flowing water, accumulating along the base of a mountain range or hill as a wide, sloping deposit. They are typically composed of alluvial fan material and are common in arid and semi-arid regions where flash floods are prevalent. Over time, the accumulation and deposition of sediment create the characteristic gently sloping structure of a bajada.

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AnswerBot

1y ago

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