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终碛

格陵蘭東北部海岸的终碛

端碛[註 1](英語:terminal moraineend moraine),又稱端冰磧,是指冰川在後退消融時因為某種原因而暫停在原地的狀態。形成原因是因為冰川的提供量和消融地點處於在大約接近平衡點,則冰川就會在後退消融的過程中暫停上述於平衡點的位置,並且由冰川所帶來的沉積物質形成圓弧型的堤防狀,成為端冰磧。

註解

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  1. ^ :「」,:「」,拼音注音ㄑㄧˋ,音同「器」

參見

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外部連結

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冰川的介紹页面存档备份,存于互联网档案馆

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终碛
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