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  2. Glacial motion - Wikipedia

    en.wikipedia.org/wiki/Glacial_motion

    At some point, if an Alpine glacier becomes too thin it will stop moving. This will result in the end of any basal erosion. The stream issuing from the glacier will then become clearer as glacial flour diminishes. Lakes and ponds can also be caused by glacial movement. Kettle lakes form when a retreating glacier leaves behind an underground ...

  3. Glacier - Wikipedia

    en.wikipedia.org/wiki/Glacier

    A glacier (US: / ˈ ɡ l eɪ ʃ ər /; UK: / ˈ ɡ l æ s i ər, ˈ ɡ l eɪ s i ər /) is a persistent body of dense ice that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries.

  4. Glaciology - Wikipedia

    en.wikipedia.org/wiki/Glaciology

    A glacier is an extended mass of ice formed from snow falling and accumulating over a long period of time; glaciers move very slowly, either descending from high mountains, as in valley glaciers, or moving outward from centers of accumulation, as in continental glaciers.

  5. Glacial stream - Wikipedia

    en.wikipedia.org/wiki/Glacial_stream

    A glacier stream is a channelized area that is formed by a glacier in which liquid water accumulates and flows. [1] Glacial streams are also commonly referred to as "glacier stream" or/and "glacial meltwater stream". The movement of the water is influenced and directed by gravity and the melting of ice. [1]

  6. Why this spectacular glacier is surging in Alaska - AOL

    www.aol.com/why-spectacular-glacier-surging...

    Alaska's mighty Muldrow Glacier is moving 50 to 100 times faster than normal. It's a major surge. Large parts of the 39-mile-long "river of ice" are progressing some 30 to 60 feet per day, as ...

  7. Glacier terminus - Wikipedia

    en.wikipedia.org/wiki/Glacier_terminus

    The difference in location of a glacier terminus as measured from this fixed position at different time intervals provides a record of the glacier's change. A similar way of tracking glacier change is comparing photographs of the glacier's position at different times. [2] The form of a glacier terminus is determined by many factors.

  8. Basal sliding - Wikipedia

    en.wikipedia.org/wiki/Basal_sliding

    Basal sliding is the act of a glacier sliding over the bed due to meltwater under the ice acting as a lubricant.This movement very much depends on the temperature of the area, the slope of the glacier, the bed roughness, the amount of meltwater from the glacier, and the glacier's size.

  9. Tourists are rushing to see glaciers before they disappear ...

    www.aol.com/news/tourists-rushing-see-glaciers...

    Now, as the glacier melts, a wall might last maybe two or three weeks before climbers need to move to a different section. “I can’t get over how fast it’s disappearing,” he said.