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Geological Formation

Balch Glacier

Glaciers and Ice Formations

Balch Glacier is a glacier about 9 nautical miles long on the east coast of Graham Land, Antarctica, flowing southeast into Mill Inlet south of Gould Glacier and reaching a maximum elevation of about 267 meters. It was surveyed by the Falkland Islands Dependencies Survey in 1946 and 1947 and named for Edwin S. Balch, an American historian of Antarctic exploration. 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: Balch 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: Balch Glacier
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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
Balch Glacier (Wikipedia)
Lead section
Quote, Lead section
Balch Glacier (66°50′S 64°48′W) is a glacier 9 nautical miles (17 km) long, on the east coast of Graham Land, flowing southeast into Mill Inlet, to the south of Gould Glacier.
View the Source
Wikidata: Balch Glacier
Wikidata Q4850237, class allow-list match (w-wdresolver-0926)View the Source
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