Shackleton Glacier is a major Antarctic glacier that descends from the East Antarctic Ice Sheet on the Antarctic Plateau and flows north through the Queen Maud Mountains to the Ross Ice Shelf, ending between Mount Speed and Waldron Spurs. It runs more than 60 nautical miles, about 110 kilometers, long and 5 to 10 nautical miles wide, fed by tributary glaciers including the Zaneveld, Logie, McGregor, and Yeats, and features such as the Swithinbank Moraine and the Gemini Nunataks along its course. It was discovered during the United States Antarctic Service expedition of 1939 to 1941 and named by the Advisory Committee on Antarctic Names for the explorer Sir Ernest Shackleton, and it has since been used as a landing site for United States Navy aircraft. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
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Caused By
Wikidata P31 formation-type mapped to formative process Glaciation via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Shackleton Glacier
In Discipline
Wikidata P31 formation-type mapped to discipline Glaciology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Shackleton Glacier
In the Other Atlases
- Also in Geography Atlas: Antarctica, found in there.
Sources
Shackleton Glacier (Wikipedia)
Lead sectionQuote, Lead section
Shackleton Glacier (84°35′S 176°20′W) is a major Antarctic glacier, over 60 nautical miles (110 km; 69 mi) long and from 5 to 10 nautical miles (9.3 to 18.5 km; 5.8 to 11.5 mi) wide, descending from the Antarctic Plateau from the vicinity of Roberts Massif and flowing north through the Queen Maud Mountains to enter...
View the Source Wikidata: Shackleton Glacier
Wikidata Q2944385, class allow-list match (w-wdresolver-0926)View the Source Reader Challenges (0)
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