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The Alph River is a small river in Antarctica, running into Walcott Bay, Victoria Land. It is in an ice-free region at the west of the Koettlitz Glacier, Scott Coast. The Alph emerges from Trough Lake and flows through Walcott Lake, Howchin Lake, and Alph Lake. It ends in a subglacial flow beneath Koettlitz Glacier to McMurdo Sound. Jemmi Creek
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). [2]
The Antarctic Ice Sheet is drained to the sea by several ice streams. The largest in East Antarctica is Lambert Glacier.In West Antarctica the large Pine Island and Thwaites Glaciers are currently the most out of balance, with a total net mass loss of 85 gigatonnes (84 billion long tons; 94 billion short tons) per year measured in 2006.
McMurdo Dry Valleys, Landsat 7 imagery acquired on December 18, 1999 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
Using satellite observations and ice-penetrating radar, scientists are now getting a glimpse of Antarctica's lost world. Ancient landscape formed by rivers revealed deep under Antarctic ice Skip ...
The Onyx River is an Antarctic meltwater stream which flows westward through the Wright Valley from Wright Lower Glacier and Lake Brownworth at the foot of the glacier to Lake Vanda, during the few months of the Antarctic summer. At 32 kilometres (20 mi) in length, it is the longest river in Antarctica.
Pages in category "Rivers of Antarctica" The following 11 pages are in this category, out of 11 total. This list may not reflect recent changes. ...
The Drygalski Ice Tongue is stable by the standards of Antarctica's icefloes, and stretches 70 kilometres (43 mi) out to sea from the David Glacier, reaching the sea from a valley in the Prince Albert Mountains of Victoria Land. The Drygalski Ice Tongue ranges from 14 to 24 kilometres (9 to 15 mi) wide.