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  2. Glacial motion - Wikipedia

    en.wikipedia.org/wiki/Glacial_motion

    If a glacier's terminus moves forward faster than it melts, the net result is advance. Glacier retreat occurs when more material ablates from the terminus than is replenished by flow into that region. Glaciologists consider that trends in mass balance for glaciers are more fundamental than the advance or retreat of the termini of individual ...

  3. Glacier morphology - Wikipedia

    en.wikipedia.org/wiki/Glacier_morphology

    Outlet glaciers are often found in valleys, and they originate from major ice sheets and ice caps. [4] They move in a singular direction that is determined by the underlying landscape. [12] Outlet glaciers drain inland glaciers through gaps found in the surrounding topography. [4]

  4. Glacier - Wikipedia

    en.wikipedia.org/wiki/Glacier

    A glacier originates at a location called its glacier head and terminates at its glacier foot, snout, or terminus. Glaciers are broken into zones based on surface snowpack and melt conditions. [ 22 ] The ablation zone is the region where there is a net loss in glacier mass.

  5. 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.

  6. 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]

  7. 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.

  8. 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.

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