A glacier is a large mass of ice that moves slowly over land due to its own weight.
Glaciers form from the compaction and recrystallization of snow over time, which eventually turns into ice.
Glacial erosion includes processes such as plucking, where rocks are lifted and carried away by the glacier, and abrasion, where the glacier grinds and polishes the underlying rock.
Glacial erosion creates landforms such as U-shaped valleys, fjords, and truncated spurs.
As glaciers melt, they deposit sediment in the form of moraines (ridges of till), drumlins (elongated hills), and eskers (long ridges of gravel).
Distinctive glacial landforms include cirques (bowl-shaped depressions), aretes (narrow ridges), horns (sharp peaks), and erratic boulders (large rocks transported and deposited by glaciers).
Climate change has led to the retreat of glaciers and the formation of glacial lakes, as well as changes in the distribution of plant and animal species in glacial regions.
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