Rennick Glacier is a major outlet glacier of the East Antarctic Ice Sheet, flowing north from the polar plateau west of the Mesa Range to Rennick Bay on the Southern Ocean. It is one of Antarctica largest glaciers, stretching nearly 200 nautical miles and varying from 20 to 30 nautical miles wide before narrowing to about 10 nautical miles near the coast. Its seaward end was first photographed during the US Navy 1946-47 Operation Highjump, and its upper reaches were explored by the US Victoria Land Traverse in February 1960, whose party was evacuated from the glacier by a Navy aircraft piloted by Lieutenant Commander Robert L. Dale. It takes its name from Rennick Bay, where it reaches the sea. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
Facts
Classification
Protected StatusInternational Treaty Protected Area 1 Connections
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: Rennick 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: Rennick Glacier
In the Other Atlases
Found In
Also in Geography Atlas: where this subject is found.
Sources
1. Secretariat of the Antarctic Treaty: Protocol on Environmental Protection to the Antarctic Treaty
Secretariat of the Antarctic TreatyArticle 2Quote, Article 2
It designates Antarctica as a “natural reserve, devoted to peace and science” (Art. 2).
View the Source Rennick Glacier (Wikipedia)
Lead sectionQuote, Lead section
Rennick Glacier (70°30′S 160°45′E) is a broad glacier, nearly 200 nautical miles (370 km; 230 mi) long, which is one of the largest in Antarctica.
View the Source Wikidata: Rennick Glacier
Wikidata Q7313329, class allow-list match (w-wdresolver-0926)View the Source Reader Challenges (0)
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