永冻土(英语:permafrost),又译永冻层、永冻土层或多年冻土)是一个地质学个名词,指当冻土层(frost soil)处于水个结冰点以下超过两年个状况。永冻层一般分布拉地下30~40公分处,通常又分为上下两层,上层夏季烊脱,下层仍处拉冰冻状态。
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