Liv Glacier
glacier in Antarctica

Liv Glacier (84°55′S 168°0′W) is a steep valley glacier, 40 nautical miles (74 km; 46 mi) long, emerging from the Antarctic Plateau just southeast of Barnum Peak and draining north through the Queen Maud Mountains to enter Ross Ice Shelf between Mayer Crags and Duncan Mountains. It was discovered in 1911 by Roald Amundsen, who named it for the daughter of Fridtjof Nansen.
Richard E. Byrd chose this glacier as his route to the Polar Plateau on 28 November 1929 when he flew from Little America to the South Pole.
Location
According to Sailing Directions for Antarctica (1960), "The Liv Glacier (85° S. 168° W.) reaches the Ross Ice Shelf on the western side of the Duncan Mountains. It is about 7 miles wide and trends southward about 40 miles to the polar plateau. The Fisher Mountains rise prominently forming the western wall, and the massif of Mount Fridtjof Nansen, about 13,156 feet high, forms the eastern flank of the Liv Glacier. The northern slopes of this sandstone and granite massif were investigated by Gould in 1929, and coal beds found. Many tributary or dendritic glaciers feed the Liv Glacier from the heights of the bordering mountains."
The head of Liv Glacier is on the East Antarctic Ice Sheet, where it passes through Hump Passage.
The glacier flow north, and near its head is joined by the LaVergne Glacier.
It turn northeast, and flows on both sides past McKinley Nunatak, June Nunatak and Aviator Nunatak.
The public source identifies “Liv Glacier” as glacier in Antarctica. This brief keeps that definition visible, then builds a research path around Glacier, glacier and Antarctica.
Why this record matters
A short description can identify a subject without explaining its stakes. For “Liv Glacier”, the useful work is to connect “glacier in Antarctica” to the records capable of establishing context and consequence.
Vocabulary and entity names are the principal evidence signals here, because they determine the precision of every later search. The source revision retrieved here is dated Jul 3, 2026. The linked authority identifier is Q6654157. Authority coordinates are -84.917, -168.000. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1911, 1929 and 1960.
A concise general-reference account can conceal disagreements about scope, terminology or the weight assigned to individual sources. The lead is largely declarative, so disagreement and counter-evidence require a deliberate search beyond the opening account. Authority statements aid reconciliation but still require their own references, qualifiers and ranks to be checked.
How to read it
Use the entry as an orientation point, then follow its citations and revision history. Names, dates and institutional relationships should be checked against the original record.
- Subject orientation
- Search vocabulary
- Locating named sources
The closest primary source, responsible institution and strongest cited specialist reference.
Three-step research path
- Establish the record: confirm the title “Liv Glacier”, its source revision and the description used here.
- Expand the search: follow Liv Glacier primary sources, Liv Glacier archive and Glacier research across catalogues and specialist indexes.
- Test the account: compare the strongest cited source with the responsible institution’s current record and note any disagreement.
Questions for further research
- Which source most directly establishes the central claim about “Liv Glacier”?
- Which cited source is closest to the event, object or claim?
- Which institution is responsible for the underlying evidence?
Search terms from this dossier
This entry incorporates text from “Liv Glacier” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.