Gough Glacier is an Antarctic glacier about 25 nautical miles long, flowing from the northern slopes of the Prince Olav Mountains and the base of the Lillie Range northward to the Ross Ice Shelf, between the Gabbro Hills and the Bravo Hills. It was named by the southern party of the New Zealand Geological Survey Antarctic Expedition of 1963 and 1964 for A. L. Gough, the party's surveyor. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
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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: Gough 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: Gough Glacier
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Gough Glacier (Wikipedia)
Lead sectionQuote, Lead section
Gough Glacier (84°42′S 171°35′W) is an Antarctic glacier about 25 nautical miles (50 km) long, flowing from the northern slopes of the Prince Olav Mountains and the base of the Lillie Range and trending northward to the Ross Ice Shelf, between the Gabbro Hills and the Bravo Hills.
Wikidata: Gough Glacier
Wikidata Q5588187, class allow-list match (w-wdresolver-0926)View the Source Reader Challenges (0)
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