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Permafrost - Wikipedia, the free encyclopedia
瀏覽:980
日期:2026-04-25
In geology, permafrost or cryotic soil is soil at or below the freezing point of water 0 °C (32 °F) for two or more years. Most permafrost is located in high latitudes (in and around the Arctic and Antarctic regions), but alpine permafrost may exist at hi...看更多



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