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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

SPETSBÅGE

Water bodies; Glaciers

En arcuatus, konvex, down-glaciären-pekar band eller vågformigheten som bildar på ytan av en glaciär på basen av en icefall. Två typer av ogives uppstår: våg ogives, som vågor på varierande höjd och ...

Nunatak

Water bodies; Glaciers

En bergstopp eller ås som Petar genom yta ett ice-fält eller en glaciär. Det kan skilja intill dalglaciärer (grönländska).

Tarn

Water bodies; Glaciers

En sjö som utvecklas i handfatet av en cirque, allmänt efter smältning av glaciären.

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