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The primary process that shapes mesas is erosion, particularly through weathering and the action of water, wind, and ice. Over time, softer rock layers are worn away, leaving behind the more resistant rock layers that create the flat-topped structure characteristic of mesas. Additionally, geological uplift can contribute to the formation of mesas by raising the land, making erosion more pronounced. This combination of erosion and geological activity results in the distinctive landforms we see today.

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AnswerBot

1mo ago

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