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  2. Fluvioglacial landform - Wikipedia

    en.wikipedia.org/wiki/Fluvioglacial_landform

    Kettles, or kettle holes, are impressions left in a glacial outwash plain by remnant ice of a retreating glacier. [32] As a glacier retreats, chunks of ice may break off in a process known as ice calving or glacier calving. As sediment-heavy glacial meltwater flows past the stationary ice block, the increased friction between the ice and ...

  3. Retreat of glaciers since 1850 - Wikipedia

    en.wikipedia.org/wiki/Retreat_of_glaciers_since_1850

    Satellite images and aerial photographs from the 1950s and 1970s show that the front of the glacier had remained in the same place for decades. In 2001 the glacier began retreating rapidly, and by 2005 the glacier had retreated a total of 7.2 km (4.5 mi), accelerating from 20 m (66 ft) per day to 35 m (115 ft) per day during that period. [117]

  4. Proglacial lake - Wikipedia

    en.wikipedia.org/wiki/Proglacial_lake

    Tarn—a proglacial lake impounded by the terminal moraine of the retreating Schoolroom Glacier in Grand Teton National Park, Wyoming In geology, a proglacial lake is a lake formed either by the damming action of a moraine during the retreat of a melting glacier , a glacial ice dam, or by meltwater trapped against an ice sheet due to isostatic ...

  5. 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 ...

  6. Paraglacial - Wikipedia

    en.wikipedia.org/wiki/Paraglacial

    Rates of landscape change and sediment output from the system are typically elevated during paraglacial landscape response. When a large mass of ice melts, the newly exposed landscape is free of vegetation and is generally unstable. Often, the retreating glacier is providing the area with high stream discharge, further increasing erosion.

  7. Kettle (landform) - Wikipedia

    en.wikipedia.org/wiki/Kettle_(landform)

    A kettle (also known as a kettle hole, kettlehole, or pothole) is a depression or hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased ...