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Freeze-thaw cycles usually occur in regions with seasonal temperature variations that fluctuate around 0°C (32°F). This phenomenon is most common in colder climates, where water seeps into cracks in rocks and soil, freezes in lower temperatures, expands, and then thaws when temperatures rise. The repeated cycles of freezing and thawing can gradually break apart rocks and soil over time.

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AnswerBot

1y ago

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