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  2. Retreat of glaciers since 1850 - Wikipedia

    en.wikipedia.org/wiki/Retreat_of_glaciers_since_1850

    Melting of mountain glaciers from 1994 to 2017 (6.1 trillion tonnes) constituted about 22% of Earth's ice loss during that period. [7]Excluding peripheral glaciers of ice sheets, the total cumulated global glacial losses over the 26 years from 1993 to 2018 were likely 5500 gigatons, or 210 gigatons per yr. [1]: 1275

  3. Glacier - Wikipedia

    en.wikipedia.org/wiki/Glacier

    The ice of a polar glacier is always below the freezing threshold from the surface to its base, although the surface snowpack may experience seasonal melting. A subpolar glacier includes both temperate and polar ice, depending on the depth beneath the surface and position along the length of the glacier. In a similar way, the thermal regime of ...

  4. List of glaciers - Wikipedia

    en.wikipedia.org/wiki/List_of_glaciers

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

  5. Holocene glacial retreat - Wikipedia

    en.wikipedia.org/wiki/Holocene_glacial_retreat

    Terminal moraines formed 5.7 thousand years ago in the San Rafael Glacier, and around 4.96 thousand years ago, they formed in the nearby Colonia Glacier. [8] In the Southern Patagonian Icefield located in Argentina and Chile, some glaciers have actually been advancing to their peak extents as recently as the 19th century as evidenced by ...

  6. Meltwater - Wikipedia

    en.wikipedia.org/wiki/Meltwater

    Meltwater (or melt water) is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltwater is often found during early spring when snow packs and frozen rivers melt with rising temperatures, and in the ablation zone of glaciers where the rate of snow cover is reducing.

  7. Glaciology - Wikipedia

    en.wikipedia.org/wiki/Glaciology

    During times in which the volume input to the glacier by precipitation is equivalent to the ice volume lost from calving, evaporation, and melting, the glacier has a steady-state condition. Some glaciers show periods where the glacier is advancing at an extreme rate, that is typically 100 times faster than what is considered normal, it is ...

  8. Last Glacial Period - Wikipedia

    en.wikipedia.org/wiki/Last_Glacial_Period

    A chronology of climatic events of importance for the Last Glacial Period, about the last 120,000 years The Last Glacial Period caused a much lower global sea level.. The Last Glacial Period (LGP), also known as the Last glacial cycle, occurred from the end of the Last Interglacial to the beginning of the Holocene, c. 115,000 – c. 11,700 years ago, and thus corresponds to most of the ...

  9. Ice melting - Wikipedia

    en.wikipedia.org/wiki/Ice_melting

    Ice melting may refer to: Ice melt; Retreat of glaciers since 1850; Arctic sea ice decline This page was last edited on 2 ...