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Freeze-thaw is a geological and physical weathering process where water infiltrates cracks in rocks or soil, freezes at low temperatures, and expands as it turns into ice. This expansion exerts pressure on the surrounding material, causing it to fracture or break apart. When the ice thaws, the water can seep deeper into the cracks, repeating the cycle and gradually disintegrating the rock or soil over time. This process is particularly significant in cold climates and contributes to the shaping of landscapes.

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