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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

冰水沉積平原

Water bodies; Glaciers

廣泛、 低邊坡角的沖積平原組成極度侵蝕、 排序已經運靠冰雪融水的沉積物 (稱為沙石)。沖積扇平原冰川腳下開始,並可能延長英里。通常情況下,沉積物變得細細微性與冰川總站的距離增加。 ...

冰川槽

Water bodies; Glaciers

線性的抑鬱症,英寸到英里長,脫除的岩石或沉積物由冰川的侵蝕作用。

大陸冰川

Water bodies; Glaciers

大陸範圍內積累的從一個中心的積累,通常在各個方向傳播的冰川冰和常年積雪的厚,次大陸。

飄忽不定

Water bodies; Glaciers

未指定的形狀和大小,岩石由冰河或冰山運輸從它的起源的一個顯著距離及存放于冰的融化。遊動範圍從卵石大小到比一座房子,通常具有不同組成,基岩或沉積物的沉積。 ...

聚集區

Water bodies; Glaciers

終年覆蓋著雪的冰川的一部分。也被稱為終年被。

冰川

Water bodies; Glaciers

冰、 雪、 岩石、 泥沙、 液態水來源於土地和南下影響其自身的重量和重心 ; 下的邊坡大,常年積累冰動態河。按其大小、 位置和熱制度分為兩冰川。 ...

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