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Dennistoun 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 authorityQ1189637 ↗
Source-derived summary

The Dennistoun Glacier (71°11′S 168°0′E) is a glacier, 50 nautical miles (93 km; 58 mi) long, draining the northern slopes of Mount Black Prince, Mount Royalist and Mount Adam in the Admiralty Mountains of Victoria Land, Antarctica.

It flows northwest between the Lyttelton Range and Dunedin Range, turning east on rounding the latter range to enter the sea south of Cape Scott.

Exploration and naming

The coastal extremity of the Dennistoun Glacier was charted in 1911–12 by the Northern Party, led by Victor Campbell, of the British Antarctic Expedition, 1910–13 (BrAE).

The glacier is named after Jim Dennistoun, a New Zealand alpinist who was in charge of the mules on board the Terra Nova on her way to Antarctica. The entire extent of the glacier was mapped by the United States Geological Survey from surveys and United States Navy aerial photography, 1960–63.

The name Fowlie Glacier, which in fact refers to a tributary glacier, has sometimes been inadvertently misapplied to this feature.

Location

The Dennistoun Glacier rises in the Admiralty Mountains between the Lyttelton Range and the Dunedin Range.

The Anare Pass is to its west, forming a route to the Ebbe Glacier.

The Dennistoun Glacier flows north and then east, fed by the Rowles Glacier and Lann Glacier from the southeast.

It passes the Hedgpeth Heights and Quam Heights to the north in the Anare Mountains.

Editorial summary

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

Editorial reviewA dependable orientation record for establishing vocabulary, names and a first evidence trail. The current lead gives the account dated anchors—1911, 1910, 1960—that can be checked directly. The selected authority fields contribute no independent date. Its value is orientation rather than verdict, with Dennistoun, Glacier 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 “Dennistoun 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 Q1189637. Authority coordinates are -71.183, 168.000. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1911, 1910 and 1960.

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Source & attribution

This entry incorporates text from “Dennistoun 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.