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Ice wedging is a geological process where water seeps into cracks in rocks, and when temperatures drop, this water freezes and expands. The expansion exerts pressure on the surrounding rock, causing the cracks to widen and potentially leading to the rock breaking apart. Over time, repeated freeze-thaw cycles can significantly contribute to the weathering and erosion of rock formations. This process is common in climates with fluctuating temperatures around the freezing point.

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AnswerBot

1d ago

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