glacier ice accumulation wikipedia - EAS
- From Wikipedia, the free encyclopedia The accumulation zone is found at the highest altitude of the glacier, where accumulation of material is greater than ablation. On a glacier, the accumulation zone is the area above the firn line, where snowfall accumulates and exceeds the losses from ablation, (melting, evaporation, and sublimation).en.wikipedia.org/wiki/Accumulation_zone
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See all on Wikipediahttps://en.wikipedia.org/wiki/Glacier_ice_accumulationGlacier ice accumulation occurs through accumulation of snow and other frozen precipitation, as well as through other means including rime ice (freezing of water vapor on the glacier surface), avalanching from hanging glaciers on cliffs and mountainsides above, and re-freezing of glacier
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See moreGlaciologists subdivide glaciers into glacier accumulation zones, based on the melting and refreezing occurring. These zones include the dry snow zone, in which the ice entirely retains subfreezing temperatures and no melting occurs. Dry
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Wikipedia text under CC-BY-SA licenseWas this helpful?Thanks! Give more feedback- https://en.wikipedia.org/wiki/Glacier
A glacier is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. Glaciers slowly deform and flow under stresses induced by their weight, creating crevasses, seracs, and other distinguishing features. They also abrade rock and debris from their substrate to create landf…
Wikipedia · Text under CC-BY-SA license - https://en.wikipedia.org/wiki/Glacier_National_Park_(U.S.)
Glacier National Park is an American national park located in northwestern Montana, on the Canada–United States border, adjacent to the Canadian provinces of Alberta and British Columbia.The park encompasses more than 1 million acres (4,000 km 2) and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), more than 130 named lakes, more …
- Area: 1,013,322 acres (4,100.77 km²)
- Nearest city: Columbia Falls, Montana
- Established: May 11, 1910
- https://en.wikipedia.org/wiki/IceSee more on en.wikipedia.orgAs a naturally occurring crystalline inorganic solid with an ordered structure, ice is considered to be a mineral. It possesses a regular crystalline structure based on the molecule of water, which consists of a single oxygen atom covalently bonded to two hydrogen atoms, or H–O–H. However, many of the physical properties of wat…
- Refractive index (n): 1.309
- Density (ρ): 0.9167–0.9168 g/cm³
- Tensile strength (σ): 5 to 18 kg-force/cm²
- https://en.wikipedia.org/wiki/Accumulation_zone
On a glacier, the accumulation zone is the area above the firn line, where snowfall accumulates and exceeds the losses from ablation, (melting, evaporation, and sublimation). The annual equilibrium line separates the accumulation and ablation zone annually. The accumulation zone is also defined as the part of a glacier's surface, usually at higher elevations, on which there is net …
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- https://en.wikipedia.org/wiki/Accumulation
Glacier ice accumulation, an element in the glacier mass balance formula Metabolic trapping , a localization mechanism of the synthesized radiocompounds in human body Tree accumulation , in computer science, the process of accumulating …
- https://sco.wikipedia.org/wiki/Glacier
A glacier is a persistent body o dense ice that is constantly movin unner its ain wicht; it forms whaur the accumulation o snaw exceeds its ablation (melting an sublimation) ower many years, eften centuries . Glacier. Taen frae "https://sco.wikipedia.org/w/index.php?title=Glacier&oldid=743651". Categeries:
- https://en.citizendium.org/wiki/Glacier
A glacier is a natural body of ice formed by the accumulation, compaction, and recrystallization of snow that thick enough to flow. It is a dynamic system involving the accumulation and transportation of ice. A mass of ice must move or flow to be considered a glacier.
- https://thereaderwiki.com/en/Glacier
The upper part of a glacier, where accumulation exceeds ablation, is called the accumulation zone. The equilibrium line separates the ablation zone and the accumulation zone; it is the contour where the amount of new snow gained by accumulation is equal to the amount of ice lost through ablation.
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