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水滴和凍結形成的冰峰 来自维基百科，自由的百科全书
冰锥（英语：icicle）也称冰柱、冰挂、冰凌、冰溜子[1]等。是雪融化在房檐或其他高处滴水渐渐凝成的尖椎形冰柱。[2]冰锥形成的物理原因一般是雪在阳光照射下因为周围环境温度升高而融化成水，在高处低落的时候，水的下层部分因脱离融点温度而又凝结成冰。
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