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in New Zealand ]] Glacier morphology, or the form a Glacier takes, is influenced by Temperature , Precipitation , Topography , and other factors. Types of glaciers range from massive Ice Sheet s, such as the Greenland Ice Sheet or those in Antarctica, to small Cirque Glacier s perched on a mountain. Glaciers types can be grouped into two main categories, based on whether or not ice flow is constrained by the underlying Bedrock Topography . UNCONSTRAINED ice cap in Iceland ]] Ice Sheet s and Ice Cap s cover vast areas and are unconstrained by the underlying topography. The main distinction between the two is area, with ice caps covering areas less than 50,000 square kilometers, while ice sheets span larger areas.1 Ice sheets and ice caps can be classified further. Ice domes Ice Dome s located in the Accumulation zone in the higher altitude portions. Ice streams Ice Stream s rapidly channel ice flow out to the sea or Ocean , where it may feed into an Ice Shelf . At the margin between ice and water, Ice Calving takes place, with Iceberg s breaking off. Ice streams are bounded on the sides by areas of slowly moving ice.2 Outlet glaciers Outlet Glacier s are channels of ice that flow out of an ice sheet, but are constrained on the sides with exposed bedrock. CONSTRAINED Icefield An Icefield covers a relatively large area, usually located in mountainous terrain. The underlying topography controls or influences the form that an icefield takes. Often, Nunatak s poke through the surface of icefields. Examples of icefields include the Columbia Icefield in the Canadian Rockies and Patagonia Icefield in Argentina . Valley glaciers Valley Glacier s, which provide drainage for icefields, are also constrained by underlying topography. Ice-free exposed bedrock and slopes often surround valley glaciers, providing snow and ice from above to accumulate on the glacier via Avalanche s. Cirque glaciers in the State of Washington ]] Cirque Glacier s form in Cirque , bowl-shaped depressions on the side of mountains. In these depressions, Snow persists through summer months, and is transformed into Glacier ice. Snow may be situated on the Leeward slope of a mountain, where it is sheltered. REFERENCES |
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