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- Antarctica is divided into West Antarctica and East Antarctica by the Transantarctic Mountains, which stretch from Victoria Land to the Ross Sea.
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5 days ago · East Antarctica lies mostly in the east longitudes and is larger than West Antarctica, which lies wholly in the west longitudes. East and West Antarctica are separated by the approximately 2,100-mile- (about 3,400-km-) long Transantarctic Mountains.
- Physical Geography
Antarctica, with an average elevation of about 7,200 feet...
- Antarctica Summary
Antarctica approximates a circular form, except for the...
- Polar, Ice, Climate
Antarctica - Polar, Ice, Climate: The unique weather and...
- Discovery of The Antarctic Poles
Antarctica - Exploration, Ice, Wildlife: National and...
- History
Antarctica - Exploration, Wildlife, Ice: Many nations were...
- National Rivalries, Claims
Antarctica - National Rivalries, Claims: The early...
- Plant Life
Antarctica - Flora, Fauna, Ecosystems: The cold desert...
- The Antarctic Treaty
Antarctica - Treaty, Continent, Wildlife: With the ending of...
- Animal Life
Antarctica - Penguins, Seals, Whales: The native land fauna...
- Biological Resources
Antarctica - Wildlife, Marine Life, Ecosystems: Marine...
- Physical Geography
May 14, 2024 · These mountains form a flat-topped massif that rises gently from beneath the ice sheet to the south, and to the north drops 3,000 feet into a valley between two major ridge systems.
2 days ago · Antarctica is divided into West Antarctica and East Antarctica by the Transantarctic Mountains, which stretch from Victoria Land to the Ross Sea. [17] [18] The vast majority of Antarctica is covered by the Antarctic ice sheet , which averages 1.9 km (1.2 mi) in thickness. [19]
May 18, 2024 · 18 May, 2024 News stories. Comprehensive digital maps of Antarctica are now available to all, following the latest update of the Antarctic Digital Database. A new map viewer brings together all of the Antarctic Digital Database datasets, alongside further useful information, and displays them together in an open-access interactive website.
3 hours ago · The mountain was likely formed in an area where two tectonic plates collided, creating a zone of uplift and compression. This process pushed the rock upwards, forming a high-elevation mountain range. Over time, the forces of erosion, especially glacial erosion, then shaped the mountain into its distinctive pyramidal form.
May 15, 2024 · about 99% thick continental ice sheet and 1% barren rock, with average elevations between 2,000 and 4,000 m; mountain ranges up to nearly 5,000 m; ice-free coastal areas include parts of southern Victoria Land, Wilkes Land, the Antarctic Peninsula area, and parts of Ross Island on McMurdo Sound; glaciers form ice shelves along about half of the ...
2 days ago · Pre-satellite era observations of Antarctic glaciers are rare. A unique record of aerial expedition images of East Antarctic outlet glaciers since the 1930s reveal long-term stability and moderate ...
