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Frost wedging occurs when water seeps into cracks in rocks and freezes as temperatures drop. When water freezes, it expands by about 9%, exerting pressure on the surrounding rock. This repeated freeze-thaw cycle causes the cracks to widen over time, eventually breaking the rock apart. The process is particularly effective in climates with frequent temperature fluctuations around the freezing point.

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AnswerBot

1mo ago

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