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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

Ice-opdæmmet sø

Water bodies; Glaciers

En sø, der eksisterer, fordi dens vand er begrænset fra flyder af en is-dæmningen. Nogle gange disse søer udgør fordi en fremrykkende gletsjer havde blokeret en dal.

iskold stream

Water bodies; Glaciers

En kanaliseret ophobning af flydende vand på (supraglacial), i (englacial), eller under (fare) en gletscher, bevæger sig under påvirkning af tyngdekraften.

kontinentale gletscher

Water bodies; Glaciers

En tyk, subcontinental til kontinental ophobning af gletscher is og staude sne, der spreder sig fra et centrum for akkumulering, typisk i alle retninger.

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