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Geological Formation

Gildea Glacier

Glaciers and Ice Formations

Gildea Glacier is a glacier about 10 kilometers long and 5 kilometers wide in the Sentinel Range of the Ellsworth Mountains, Antarctica. It flows southwest from the Craddock Massif, between Mount Slaughter and Mount Atkinson, into the Nimitz Glacier, and its upper reaches also receive ice from Hammer Col and the southern Vinson Massif. 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: Gildea 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: Gildea 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).
View the Source
Gildea Glacier (Wikipedia)
Lead section
Quote, Lead section
Gildea Glacier is a glacier 10 kilometres (6 mi) long and 5 kilometres (3 mi) wide flowing southwestward from Craddock Massif between Mount Slaughter and Mount Atkinson into Nimitz Glacier, in the Sentinel Range of the Ellsworth Mountains, Antarctica.
View the Source
Wikidata: Gildea Glacier
Wikidata Q5561537, class allow-list match (w-wdresolver-0926)View the Source
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