| 单词 | gelifluction |
| 释义 | gelifluction [¦jel·ǝ¦flǝk·shǝn] GEOLOGY The slow, continuous downslope movement of rock debris and water-saturated soil that occurs above frozen ground, as in most polar regions and in many high mountain ranges. Also known as congelifluction; gelisolifluction. |
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