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Geological Formation

Cumpston Glacier

Glaciers and Ice Formations

Cumpston Glacier is a small glacier on the east coast of Graham Land in Antarctica, draining into Mill Inlet between the neighboring Breitfuss and Quartermain glaciers. It was named by the UK Antarctic Place-Names Committee for J.S. Cumpston, an Australian historian of Antarctic exploration. Detailed information on its length and date of discovery remains sparse in published sources. 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: Cumpston 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: Cumpston 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
Cumpston Glacier (Wikipedia)
Lead section
Quote, Lead section
Cumpston Glacier is a small glacier on the east coast of Graham Land, draining between Breitfuss Glacier and Quartermain Glacier into the head of Mill Inlet.
View the Source
Wikidata: Cumpston Glacier
Wikidata Q5194170, class allow-list match (w-wdresolver-0926)View the Source
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