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  2. 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.

  3. Paternoster lake - Wikipedia

    en.wikipedia.org/wiki/Paternoster_lake

    A paternoster lake is one of a series of glacial lakes connected by a single stream or a braided stream system. The name comes from the word Paternoster , another name for the Lord's Prayer derived from the Latin words for the prayer's opening words, "Our Father"; Paternoster lakes are so called because of their resemblance to rosary beads ...

  4. Kame - Wikipedia

    en.wikipedia.org/wiki/Kame

    A kame, or knob, is a glacial landform, an irregularly shaped hill or mound composed of sand, gravel and till that accumulates in a depression on a retreating glacier, and is then deposited on the land surface with further melting of the glacier.

  5. Bergschrund - Wikipedia

    en.wikipedia.org/wiki/Bergschrund

    Cross section of a cirque glacier showing the bergschrund A bergschrund—the long crack at the foot of the mountain slope—in the Ötztal Alps Open bergschrunds at Mont Dolent. A bergschrund (from the German for mountain cleft) is a crevasse that forms where moving glacier ice separates from the stagnant ice or firn above. [1]

  6. U-shaped valley - Wikipedia

    en.wikipedia.org/wiki/U-shaped_valley

    The glacier visible at the head of the valley is the last remnant of the formerly much more extensive glacier which carved it. U-shaped valley with lake in Myklebustdalen, Nordfjord, Sogn og Fjordane, Norway. U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation.

  7. 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 ]

  8. Category:Glacial landforms - Wikipedia

    en.wikipedia.org/wiki/Category:Glacial_landforms

    Pages in category "Glacial landforms" The following 56 pages are in this category, out of 56 total. This list may not reflect recent changes. ...

  9. List of glaciers in India - Wikipedia

    en.wikipedia.org/wiki/List_of_glaciers_in_India

    The Himalayan region of India is home to some of the most notable glaciers in the world, including the Siachen Glacier, the second-largest non-polar glacier on Earth and the largest glacier in India. The following is a list of the most important glaciers in India .