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Geological Formation

Flogeken Glacier

Glaciers and Ice Formations

Flogeken Glacier is a deeply entrenched glacier in the Muhlig-Hofmann Mountains of Queen Maud Land, Antarctica, flowing northwest between Mount Grytoyr and the Langfloget Cliff. It was mapped by Norwegian cartographers from surveys and air photographs taken during the Sixth Norwegian Antarctic Expedition of 1956 to 1960, which named it Flogeken, meaning the rock wall spoke. 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: Flogeken 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: Flogeken 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 2
Quote, Article 2
It designates Antarctica as a “natural reserve, devoted to peace and science” (Art. 2).
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Flogeken Glacier (Wikipedia)
Lead section
Quote, Lead section
Flogeken Glacier (72°4′S 4°25′E) is a deeply entrenched glacier, flowing northwest between Mount Grytoyr and Langfloget Cliff, in the Mühlig-Hofmann Mountains of Queen Maud Land, Antarctica. it was mapped by Norwegian cartographers from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956-60) and named Flogeken (the rock wall spoke).
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Wikidata: Flogeken Glacier
Wikidata Q5459984, class allow-list match (w-wdresolver-0926)View the Source
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