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Ice streams are a type of glacier [1] and many of them have "glacier" in their name, e.g. Pine Island Glacier. Ice shelves are listed separately in the List of Antarctic ice shelves . For the purposes of these lists, the Antarctic is defined as any latitude further south than 60° (the continental limit according to the Antarctic Treaty System ).
Lambert Glacier is a major glacier in East Antarctica. At about 80 km (50 mi) wide, over 400 km (250 mi) long, and about 2,500 m (8,200 ft) deep, it is the world's largest glacier. At about 80 km (50 mi) wide, over 400 km (250 mi) long, and about 2,500 m (8,200 ft) deep, it is the world's largest glacier.
This is a list of glaciers in the Antarctic with a name starting with the letters I–Z. This list does not include ice sheets , ice caps or ice fields , such as the Antarctic ice sheet , but includes glacial features that are defined by their flow, rather than general bodies of ice.
Pages in category "Lists of glaciers of Antarctica" The following 25 pages are in this category, out of 25 total. This list may not reflect recent changes. A.
The majority of Europe's glaciers are found in the Alps, Caucasus and the Scandinavian Mountains (mostly Norway) as well as in Iceland. Iceland has the largest glacier in Europe, Vatnajökull Glacier, that covers between 8,100 and 8,300 km 2 in area and 3,100 km 3 in volume. Norway alone has more than 2500 glaciers (including very small ones ...
Antarctica is the southernmost continent on Earth. While Antarctica has never had a permanent human population, it has been explored by various groups, and many locations on and around the continent have been described. This page lists notable places in and immediately surrounding the Antarctic continent, including geographic features, bodies ...
Antarctica glacier stubs (8 C, 94 P) Pages in category "Glaciers of Antarctica" The following 11 pages are in this category, out of 11 total.
The Amundsen Glacier) is a major Antarctic glacier, about 7 to 11 km (4 to 6 nmi) wide and 150 km (80 nmi) It originates on the Antarctic Plateau where it drains the area to the south and west of Nilsen Plateau, then descends through the Queen Maud Mountains to enter the Ross Ice Shelf just west of the MacDonald Nunataks.