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Glaciers

A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, seracs, and other distinguishing features. They also abrade rock and debris from their substrate to create landforms such as cirques and moraines. Glaciers form only on land and are distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water.

Contributors in Glaciers

Glaciers

海平面

Water bodies; Glaciers

全球海平面政權的海水可用數量的變化引起的波動。最大變化是引起的水被添加到,或從冰川中刪除。

總站

Water bodies; Glaciers

低大部分邊距、 結束或下肢的冰川。

碎片錐

Water bodies; Glaciers

圓錐或的一堆碎片覆蓋冰,保護不融化的冰夠厚的沉積物覆蓋。

新月體過切

Water bodies; Glaciers

任何彎曲的標記或骨折產生的拔毛或鑿的冰川在床。大比顫振標記,通常這些有溝槽的角點了冰川。

條紋

Water bodies; Glaciers

多個一般並行、 線性槽刻由岩石中的冰川到哪些它流動的基岩床被凍結。

冰川流

Water bodies; Glaciers

冰的冰川,通常是在向下和向外的方向,引起的重力的運動。正常流動率是在每日的腳。'快速' 流率 (即 潮) 在 10 秒或每日腳數百個。

分流

Water bodies; Glaciers

源自冰川的主幹的冰川冰的舌頭。這可能會導致從微分熔化更改漸變的冰川的一部分。

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