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Geological Formation

Dålk Glacier

Glaciers and Ice Formations

Dålk Glacier is a glacier in Antarctica, about 15 kilometers long, draining into the southeast part of Prydz Bay between the Larsemann Hills and Steinnes. It was mapped by Norwegian cartographers from aerial photographs taken during the Lars Christensen Expedition of 1936 and 1937, and it was named by John H. Roscoe in a 1952 study of features identified from U.S. Navy Operation Highjump photographs, after the nearby Dålk Island at the glacier's terminus. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Connections

Caused By

Glaciation, Processes

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: Dålk Glacier

In Discipline

Glaciology, Disciplines

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: Dålk Glacier
Sources
Dålk Glacier (Wikipedia)
Lead section
Quote, Lead section
Dålk Glacier (69°26′S 76°27′E) is a glacier, 8 nautical miles (15 km) long, draining into the southeast part of Prydz Bay between the Larsemann Hills and Steinnes.
View the Source
Wikidata: Dålk Glacier
Wikidata Q5320165, class allow-list match (w-wdresolver-0926)View the Source
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