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  2. File:Glacier diagram.svg - Wikipedia

    en.wikipedia.org/wiki/File:Glacier_diagram.svg

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  3. Glacier morphology - Wikipedia

    en.wikipedia.org/wiki/Glacier_morphology

    Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. [1] The goal of glacial morphology is to gain a better understanding of glaciated landscapes and the way they are shaped. [ 2 ]

  4. Glacial landform - Wikipedia

    en.wikipedia.org/wiki/Glacial_landform

    Erosional landforms. As the glaciers expand, due to their accumulating weight of snow and ice they crush, abrade, and scour surfaces such as rocks and bedrock.The resulting erosional landforms include striations, cirques, glacial horns, arêtes, trim lines, U-shaped valleys, roches moutonnées, overdeepenings and hanging valleys.

  5. 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 ...

  6. Glacier - Wikipedia

    en.wikipedia.org/wiki/Glacier

    A glacier that fills a valley is called a valley glacier, or alternatively, an alpine glacier or mountain glacier. [14] A large body of glacial ice astride a mountain, mountain range, or volcano is termed an ice cap or ice field. [15] Ice caps have an area less than 50,000 km 2 (19,000 sq mi) by definition.

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  8. Moulin (geomorphology) - Wikipedia

    en.wikipedia.org/wiki/Moulin_(geomorphology)

    They can be up to 10 meters wide and are typically found on ice sheets and flat areas of a glacier in a region of transverse crevasses. Moulins can reach the bottom of the glacier, hundreds of meters deep, [3] [4] [5] or may only reach the depth of common crevasse formation (about 10–40 m) where the stream flows englacially. [6]

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