Nimrod Glacier
glacier in Antarctica

The Nimrod Glacier (82°21′S 163°00′E) is a major glacier about 85 nautical miles (157 km; 98 mi) long, flowing from the polar plateau in a northerly direction through the Transantarctic Mountains into the Ross Ice Shelf, Antarctica.
Location
The Nimrod Glacier flows north between the Geologists and Miller Ranges, then northeasterly between the Churchill Mountains and Queen Elizabeth Range, and finally spills into Shackleton Inlet and the Ross Ice Shelf between Capes Wilson and Lyttelton.
It was photographed from the air by USN Operation Highjump, 1946–47. The name, given by US-ACAN, is in association with Shackleton Inlet and is for the Nimrod, the ship of the British Antarctic Expedition (1907–09) under Ernest Shackleton.
The mouth of the glacier is southeast of the Starshot Glacier and the Nursery Glacier.
It is north of Robb Glacier.
Icefalls
Worsley Icefalls
82°57′S 155°00′E
Icefalls near the head of Nimrod Glacier.
Seen by the northern party of the NZGSAE (1961-62) and presumbably named for Frank Worsley, member of the British Trans-Antarctic Expedition, 1914-16, and Shackleton-Rowett Antarctic Expedition, 1921-22.
Cooper Icefalls
82°31′S 160°00′E.
The main icefalls of the Nimrod Glacier, in the vicinity of Kon-Tiki Nunatak.
Named by the southern party of the NZGSAE (1960-61) for Christopher Neville Cooper, a member of the expedition, and also a member of the New Zealand Alpine Club Antarctic Expedition, 1959-60.
The public source identifies “Nimrod Glacier” as glacier in Antarctica. This brief keeps that definition visible, then builds a research path around Nimrod, Glacier and glacier.
Why this record matters
A short description can identify a subject without explaining its stakes. For “Nimrod 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 Q3108304. Authority coordinates are -81.350, 163.000. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1946, 1907, 1961 and 1914.
Overview language is designed for orientation and should not be treated as a substitute for the evidence cited beneath it. 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 “Nimrod Glacier”, its source revision and the description used here.
- Expand the search: follow Nimrod Glacier primary sources, Nimrod Glacier archive and Nimrod 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 “Nimrod Glacier”?
- What terminology or title could unlock a more precise catalogue search?
- Which institution is responsible for the underlying evidence?
Search terms from this dossier
This entry incorporates text from “Nimrod 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.