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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

Tarna

Water bodies; Glaciers

Ezeru, kas attīsta cirque baseinā kopumā pēc ledāja kušanas.

ogive

Water bodies; Glaciers

Arcuate, izliekta, norādot uz leju ledāju joslu vai bedrīti, kas veido ledāja pakājē icefall virsmas. Divu veidu zeltpleksti notikt: vilnis zeltpleksti, kurā ir dažādu augstumu un band zeltpleksti, ...

ledāja groove

Water bodies; Glaciers

Lineārā depresija, collas jūdžu garumā, ražo, atdalot no akmens vai nogulumu erozijas darbība ir kā rāpdamies pa ledāju.

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