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  2. Laurentide ice sheet - Wikipedia

    en.wikipedia.org/wiki/Laurentide_ice_sheet

    The Laurentide ice sheet (LIS) was a massive sheet of ice that covered millions of square miles, including most of Canada and a large portion of the Northern United States, multiple times during the Quaternary glaciation epochs, from 2.58 million years ago to the present.

  3. Huge glacier melt and fast rising seas amid hottest eight ...

    www.aol.com/huge-glacier-melt-fast-rising...

    Glacier melt records were shattered in the European Alps, with average loss of three to four metres of ice thickness throughout the mountain range – substantially more than the previous record ...

  4. Post-glacial rebound - Wikipedia

    en.wikipedia.org/wiki/Post-glacial_rebound

    Changes in the elevation of Lake Superior due to glaciation and post-glacial rebound. During the last glacial period, much of northern Europe, Asia, North America, Greenland and Antarctica were covered by ice sheets, which reached up to three kilometres thick during the glacial maximum about 20,000 years ago.

  5. Last Glacial Maximum - Wikipedia

    en.wikipedia.org/wiki/Last_Glacial_Maximum

    [68] [69] [70] At its peak, the Laurentide Ice Sheet reached 3.2 km in height around Keewatin Dome and about 1.7-2.1 km along the Plains divide. [71] In addition to the large Cordilleran Ice Sheet in Canada and Montana, alpine glaciers advanced and (in some locations) ice caps covered much of the Rocky and Sierra Nevada Mountains further south ...

  6. Greenland glaciers melt five times faster than 20 years ago - AOL

    www.aol.com/news/greenland-glaciers-melt-five...

    Global warming has increased the speed at which glaciers in Greenland are melting by fivefold over the last 20 years, scientists from the University of Copenhagen said on Friday. Greenland's ice ...

  7. Deglaciation - Wikipedia

    en.wikipedia.org/wiki/Deglaciation

    Deglaciation is the transition from full glacial conditions during ice ages, to warm interglacials, characterized by global warming and sea level rise due to change in continental ice volume. [1] Thus, it refers to the retreat of a glacier, an ice sheet or frozen surface layer, and the resulting exposure of the Earth's surface.

  8. Scientists discover why the Andes are rising as glaciers melt

    www.aol.com/news/scientists-discover-why-the...

    The glaciers on the Andes mountain range are melting quickly - at some of the fastest rates on the planet - and the ground beneath them is rising up rapidly too. Scientists discover why the Andes ...

  9. Retreat of glaciers since 1850 - Wikipedia

    en.wikipedia.org/wiki/Retreat_of_glaciers_since_1850

    The White Chuck Glacier (near Glacier Peak) is a particularly dramatic example. The glacier area shrank from 3.1 km 2 (1.2 sq mi) in 1958 to 0.9 km 2 (0.35 sq mi) by 2002. Between 1850 and 1950, the Boulder Glacier on the southeast flank of Mount Baker retreated 8,700 feet (2,700 m). William Long of the United States Forest Service observed the ...