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  2. Laurentide ice sheet - Wikipedia

    en.wikipedia.org/wiki/Laurentide_ice_sheet

    Laurentide ice sheet. The maximum extent of glacial ice in the north polar area during the Pleistocene period included the vast Laurentide ice sheet in eastern North America. The Laurentide ice sheet 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 ...

  3. Ice sheet - Wikipedia

    en.wikipedia.org/wiki/Ice_sheet

    Greenland ice sheet as seen from space. An ice sheet is a body of ice which covers a land area of continental size - meaning that it exceeds 50,000 km 2. [4] The currently existing two ice sheets in Greenland and Antarctica have a much greater area than this minimum definition, measuring at 1.7 million km 2 and 14 million km 2, respectively.

  4. Antarctic ice sheet - Wikipedia

    en.wikipedia.org/wiki/Antarctic_ice_sheet

    The Antarctic ice sheet is a continental glacier covering 98% of the Antarctic continent, with an area of 14 million square kilometres (5.4 million square miles) and an average thickness of over 2 kilometres (1.2 mi). It is the largest of Earth's two current ice sheets, containing 26.5 million cubic kilometres (6,400,000 cubic miles) of ice ...

  5. Greenland ice sheet - Wikipedia

    en.wikipedia.org/wiki/Greenland_ice_sheet

    The Greenland ice sheet is an ice sheet which forms the second largest body of ice in the world. It is an average of 1.67 km (1.0 mi) thick, and over 3 km (1.9 mi) thick at its maximum. [ 2 ] It is almost 2,900 kilometres (1,800 mi) long in a north–south direction, with a maximum width of 1,100 kilometres (680 mi) at a latitude of 77°N, near ...

  6. West Antarctic Ice Sheet - Wikipedia

    en.wikipedia.org/wiki/West_Antarctic_Ice_Sheet

    Like the other ice sheets, West Antarctic Ice Sheet had undergone significant changes in size during its history. Until around 400,000 years ago, the state of WAIS was largely governed by the effects of solar variation on heat content of the Southern Ocean , and it waxed and waned in accordance with a 41,000-year-long cycle. [ 31 ]

  7. Deglaciation - Wikipedia

    en.wikipedia.org/wiki/Deglaciation

    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. Ross Ice Shelf - Wikipedia

    en.wikipedia.org/wiki/Ross_Ice_Shelf

    The Ross Ice Shelf is one of many such shelves. It reaches into Antarctica from the north, and covers an area of about 520,000 km 2 (200,000 sq mi), nearly the size of France. [2][3] The ice mass is about 800 km (500 mi) wide and 970 km (600 mi) long. In some places, namely its southern areas, the ice shelf can be almost 750 m (2,450 ft) thick.

  9. Keewatin ice sheet - Wikipedia

    en.wikipedia.org/wiki/Keewatin_ice_sheet

    Manitoba. Centered on the Kivalliq Region, Nunavut, Canada (known as the Keewatin Region, Northwest Territories, until 1999) (ca 102 W, 63 N) the ice sheet covered up to 2,500,000 km 2 (970,000 sq mi) the Last Glacial Maximum. At its greatest reach, (14*146=2044 N-S by 12*146=1752 E-W) the northern edge abutted the Greenland ice sheet in Baffin ...

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