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In a valley glacier the ice flows downslope from the zone of accumulation, while for a continental glacier the ice flows laterally outward and away from the zone of accumulation. A subpolar glacier includes both temperate and polar ice, depending on the depth beneath the surface and position along the length of the glacier. In a similar way, the thermal regime of a glacier is often described by its basal temperature.
Understanding the Context
Glacier, any large mass of perennial ice that originates on land by the recrystallization of snow or other forms of solid precipitation and that shows evidence of past or present flow. With over 700 miles of trails, Glacier is a paradise for adventurous visitors seeking a landscape steeped in human culture. Relive the days of old through historic chalets, lodges, and the famous Going-to-the-Sun Road. What is a glacier?
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A glacier is a large, perennial accumulation of crystalline ice, snow, rock, sediment, and often liquid water that originates on land and moves down slope under the influence of its own weight and gravity. Typically, glaciers exist and may even form in areas where: A glacier is a huge mass of many years of snow, ice, rock, sediment, and water. It originates on land and moves down slope under the influence of its own weight and gravity. In geography and geology, a glacier is a large, persistent body of ice that forms on land and moves slowly due to its own weight and internal deformation. Glaciers form in regions where the accumulation of snow and ice exceeds melting and sublimation over long time scales, typically centuries.