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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

mass budget

Water bodies; Glaciers

A measure of the change in mass of a glacier at a certain point for a specific period of time. The balance between accumulation and ablation.

glacial lake

Water bodies; Glaciers

An accumulation of standing liquid water on (supraglacial), in (englacial), or under (subglacial) a glacier.

drift

Water bodies; Glaciers

A collective term used to describe all types of glacier sedimentary deposits, regardless of the size or amount of sorting. The term includes all sediment that is transported by a glacier, whether it ...

end moraine

Water bodies; Glaciers

A cross-valley, ridge-like accumulation of glacial sediment that forms at the farthest point reached by the terminus of an advancing glacier.

remnant

Water bodies; Glaciers

An isolated melting mass of glacier ice, that has become detached from its source and the remainder of the glacier. Some remnants cover many square miles.

ice-cored moraine

Water bodies; Glaciers

A moraine ridge consisting of a drape of sediment overlying a mass of stagnant ice.

outwash plain

Water bodies; Glaciers

A broad, low-slope angle alluvial plain composed of glacially eroded, sorted sediment (termed outwash), that has been transported by meltwater. The alluvial plain begins at the foot of a glacier and ...

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