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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/

Facts
Classification
Protected Status
International Treaty Protected Area 1
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

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
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Found In

Also in Geography Atlas: where this subject is found.

Source GeoNames: GeoNames search results for Dålk GlacierSearch result row
Quote, Search result row
Dålk Glacier -69.4261111 76.4722222 Antarctica glacier(s)
Sources
1. Secretariat of the Antarctic Treaty: Protocol on Environmental Protection to the Antarctic Treaty
Secretariat of the Antarctic TreatyArticle 2
Quote, Article 2
It designates Antarctica as a “natural reserve, devoted to peace and science” (Art. 2).
View the Source
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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