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Canyon 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 authorityQ5034206
Source-derived summary

Canyon Glacier (83°57′S 175°25′E) is a narrow glacier, 35 nautical miles (65 km; 40 mi) long, flowing to the Ross Ice Shelf. It drains the northwest slopes of Mount Wexler and moves northward between steep canyon walls of the Separation Range and Hughes Range to join the ice shelf immediately west of Giovinco Ice Piedmont. The glacier was observed from nearby Mount Patrick by the New Zealand Alpine Club Antarctic Expedition (1959–60) who gave the descriptive name.

Location

The Canyon Glacier rises to the north of the Pain Névé, below Mount Wexler in the Hughes Range to the east. The Commonwealth Range is to the west, including Mount Hermanson and Gray Peak, which overlook the upper reaches. The Canyon Glacier flows north and is joined by the Cunningham Glacier from the left (west). It continues north past the Separation Range along its west side.

At its mouth it passes the Nadeau Bluff and the Giovinco Ice Piedmont to the east and Mount Cope to its west.

Features

Cunningham Glacier

84°16′S 173°45′E.

A tributary glacier flowing northeast to enter Canyon Glacier 5 nautical miles (9.3 km; 5.8 mi) north of Gray Peak.

Named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Willard E. Cunningham, Jr., cook at McMurdo Station, winter 1960; at South Pole Station, winter 1963.

Editorial summary

Begin with the source’s own compact description: “Canyon Glacier” is glacier in Antarctica. The dossier treats that line as a proposition to test through Canyon, Glacier and glacier, not as a finished interpretation.

Editorial reviewA dependable orientation record for establishing vocabulary, names and a first evidence trail. The current lead gives the account dated anchors—1959, 1960, 1963—that can be checked directly. The selected authority fields contribute no independent date. For this dossier, Canyon, Glacier and glacier is the immediate research focus.
Editorial analysis

Why this record matters

The phrase “glacier in Antarctica” supplies a clear boundary for inquiry. It also exposes the unanswered questions: who defined that boundary, when it became stable and which sources sit outside it.

Evidence profile

The citation trail is more important than the brevity of the summary: it shows where individual claims can be examined in context. The source revision retrieved here is dated Jul 3, 2026. The linked authority identifier is Q5034206. Authority coordinates are -83.950, 175.417. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1959, 1960 and 1963.

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 Canyon Glacier primary sources, Canyon Glacier archive and Canyon 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.

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Source & attribution

This entry incorporates text from Canyon 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.