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  2. Geology of Antarctica - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Antarctica

    Study of the geology of Antarctica is hampered by the widespread ice cover The bedrock topography of Antarctica (with the ice cover digitally removed), critical to understanding the motion of the continental ice sheets Antarctica without its ice cover. This map does not consider that sea level would rise because of the melted ice, or that the ...

  3. McMurdo Dry Valleys - Wikipedia

    en.wikipedia.org/wiki/McMurdo_Dry_Valleys

    The Dry Valleys are so named because of their extremely low humidity and lack of snow or ice cover. They are also dry because, in this location, the mountains are sufficiently high that they block seaward-flowing ice from the East Antarctic Ice Sheet from reaching the Ross Sea. At 4,800 square kilometres (1,900 sq mi), the valleys constitute ...

  4. Geography of Antarctica - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Antarctica

    USGS TerraWeb: Satellite Image Map of Antarctica (archived 1 March 2005) United States Antarctic Resource Center (USARC) Archived 28 August 2008 at the Wayback Machine; BEDMAP (archived 25 January 2005) Antarctic Digital Database (Topographic data for Antarctica, including web map browser) Landsat Image Mosaic of Antarctica (LIMA; USGS web pages)

  5. Scientists create most detailed map of Antarctica ever - AOL

    www.aol.com/news/scientists-create-most-detailed...

    <p>Chances are you make it through most days without sparing a thought for Antarctica. At just over 5.4 million square miles, it's a massive chunk of land that is nearly twice the size of ...

  6. Antarctic oasis - Wikipedia

    en.wikipedia.org/wiki/Antarctic_oasis

    In Antarctica there are, in addition to mountaintops and nunataks, other natural snow- and ice-free areas often referred to as "Antarctic oases" or "dry valleys". [1] [2] These areas are surrounded by the Antarctic ice sheet or, in coastal areas, are situated between the ice sheet and the Antarctic ice shelves.

  7. Smith Island (South Shetland Islands) - Wikipedia

    en.wikipedia.org/wiki/Smith_Island_(South...

    Antarctica: Livingston Island and Greenwich, Robert, Snow and Smith Islands. Scale 1:120000 topographic map. Troyan: Manfred Wörner Foundation, 2010. ISBN 978-954-92032-9-5 (First edition 2009. ISBN 978-954-92032-6-4) South Shetland Islands: Smith and Low Islands. Scale 1:150000 topographic map No. 13677. British Antarctic Survey, 2009.

  8. Byers Peninsula - Wikipedia

    en.wikipedia.org/wiki/Byers_Peninsula

    Byers Peninsula is a mainly ice-free peninsula forming the west end of Livingston Island in the South Shetland Islands of Antarctica. It occupies 60 km 2 (23 sq mi), [ 1 ] borders Ivanov Beach to the northeast and is separated from Rotch Dome on the east by the ridge of Urvich Wall .

  9. Veleka Ridge - Wikipedia

    en.wikipedia.org/wiki/Veleka_Ridge

    Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Veleka Ridge is a predominantly ice-free ridge extending 3 km between Charity Glacier in the north and Botev Point in the south, and 1.3 km wide, in the southwest extremity of Friesland Ridge, Tangra Mountains on Livingston Island in the South Shetland Islands ...