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  2. Glacier morphology - Wikipedia

    en.wikipedia.org/wiki/Glacier_morphology

    Lower Curtis Glacier is a cirque glacier in the North Cascades in the U.S. state of Washington. Cirque glaciers are glaciers that appear in bowl-shaped valley hollows. [4] [12] Snow easily settles in the topographic structure; it is turned to ice as more snow falls and is subsequently compressed. [12]

  3. Glacial landform - Wikipedia

    en.wikipedia.org/wiki/Glacial_landform

    Apart from the landforms left behind by glaciers, glaciers themselves are striking features of the terrain, particularly in the polar regions of Earth. Notable examples include valley glaciers where glacial flow is restricted by the valley walls, crevasses in the upper section of glacial ice, and icefalls—the ice equivalent of waterfalls.

  4. Ice-sheet model - Wikipedia

    en.wikipedia.org/wiki/Ice-sheet_model

    The Parallel Ice Sheet Model is an open-sourced 3D ice sheet model capable of high resolution. [26] PISM is written in C++ and Python, and takes NetCDF files as input for the model. [ 27 ] PISM uses a "SIA+SSA hybrid" model, using both the shallow shelf approximation and shallow ice approximation models as stress balance models and does not ...

  5. Vernagtferner - Wikipedia

    en.wikipedia.org/wiki/Vernagtferner

    The diagrams on the right demonstrate the data collected by the Commission for Glaciology of the BAdW since 1965 on the growth of the Vernagtferner glacier. The upper diagram shows the glacier's area, with the ablation and accumulation areas (nutrient and supply areas) displayed in different colors.

  6. Quaternary glaciation - Wikipedia

    en.wikipedia.org/wiki/Quaternary_glaciation

    The reason is that a continental glacier completely disrupts the preglacial drainage system. The surface over which the glacier moved was scoured and eroded by the ice, leaving many closed, undrained depressions in the bedrock. These depressions filled with water and became lakes. A diagram of the formation of the Great Lakes

  7. Ice sheet - Wikipedia

    en.wikipedia.org/wiki/Ice_sheet

    Greenland ice sheet as seen from space. An ice sheet is a body of ice which covers a land area of continental size - meaning that it exceeds 50,000 km 2. [4] The currently existing two ice sheets in Greenland and Antarctica have a much greater area than this minimum definition, measuring at 1.7 million km 2 and 14 million km 2, respectively.

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  9. Esker - Wikipedia

    en.wikipedia.org/wiki/Esker

    Diagram illustrating (i) tunnel in glacier before retreat of ice, forming (ii) meandering esker in The Ice Melts: Deposition, p. 6 of "Pennsylvania and the Ice Age" published 1999 by PA DCNR Bureau of Topographic and Geologic Survey; The Bridgenorth Esker: geomorphology and sedimentology