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Russell West Glacier

glacier in Antarctica

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General referenceInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionJul 3, 2026
Entity authorityQ7381866
Source-derived summary

Russell West Glacier (63°40′S 58°50′W) is a glacier, 11 nautical miles (20 km; 13 mi) long and 4 nautical miles (7.4 km; 4.6 mi) wide, which lies immediately north of Detroit Plateau and flows from Mount Canicula westward into Bone Bay, on the north side of Trinity Peninsula. This glacier together with Russell East Glacier, which flows eastward into Prince Gustav Channel on the south side of Trinity Peninsula, form a through glacier across the north part of Antarctic Peninsula.

Location

Russell West Glacier flows west into the northwest shore of the western end of the Trinity Peninsula, which forms the tip of the Antarctic Peninsula.

Its mouth is in Bone Bay on the Bransfield Strait, northeast of Charcot Bay, east of the Orléans Strait, south of Astrolabe Island and southwest of Lafond Bay.

It is bounded to the southwest by the Gavin Ice Piedmont.

The head of the glacier is between Allen Knoll and Sirius Knoll.

At its mouth it passes Wimple Dome to the north.

Copernix satellite view

Mapping and name

Russell West Glacier was first surveyed in 1946 by the Falkland Islands Dependencies Survey (FIDS).

It was named by the UK Antarctic Place-Names Committee (UK-APC) for Victor Ian Russell, surveyor and leader of the FIDS base at Hope Bay in 1946.

Russell was head of the Hope Bay station in 1946 and 1947.

Editorial summary

The public source identifies “Russell West Glacier” as glacier in Antarctica. This brief keeps that definition visible, then builds a research path around Russell, West and Glacier.

Editorial reviewA practical starting point whose main value is the path it opens into stronger specialist and primary sources. The current lead gives the account dated anchors—1946, 1947—that can be checked directly. The selected authority fields contribute no independent date. Its value is orientation rather than verdict, with Russell, West and Glacier providing the first useful test.
Editorial analysis

Why this record matters

A short description can identify a subject without explaining its stakes. For “Russell West Glacier”, the useful work is to connect “glacier in Antarctica” to the records capable of establishing context and consequence.

Evidence profile

Named sources, stable identifiers and responsible institutions provide the strongest route from overview to verifiable evidence. The source revision retrieved here is dated Jul 3, 2026. The linked authority identifier is Q7381866. Authority coordinates are -63.667, -58.833. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1946 and 1947.

Critical limits

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.

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Three-step research path

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  2. Expand the search: follow Russell West Glacier primary sources, Russell West Glacier archive and Russell research across catalogues and specialist indexes.
  3. Test the account: compare the strongest cited source with the responsible institution’s current record and note any disagreement.

Questions for further research

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Source & attribution

This entry incorporates text from Russell West 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.