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Cumulus Hills

hills in Antarctica

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General referenceInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionAug 11, 2026
Entity authorityQ5194190
Source-derived summary

The Cumulus Hills (85°20′S 175°0′W) are several groups of largely barren hills in Antarctica. Divided by the Logie Glacier, they are bounded by Shackleton Glacier on the west, McGregor Glacier on the north and Zaneveld Glacier on the south.

Discovery and naming

The exposed rock in this area was observed on a number of occasions to give rise to the formation of cumulus clouds, considered to be very rare at this elevation.

The hills were named by the Southern Party of the New Zealand Geological Survey Antarctic Expedition (1961–62) because of these clouds.

Features

The Cumulus Hills are bounded by the Shackleton Glacier to the west, Zaneveld Glacier to the south and McGregor Glacier and Gatlin Glacier to the north.

There is a large snowfield to the east.

From south to north, features include Schroeder Hill, Wiest Bluff, Vickers Nunatak and Ellis Bluff, all south of Logie Glacier, which flows west into Shackleton Glacier.

North of this are Landry Bluff, separated by Brunner Glacier from Halfmoon Bluff, Gillespie Glacier, Shenk Peak, Mount Kenyon, La Prade Valley, Rougier Hill and Cheu Valley.

To the east of Gatlin Glacier is Red Raider Rampart.

Schroeder Hill

85°23′S 175°12′W.

A rock prominence, 2,680 metres (8,790 ft) high, standing 3.5 nautical miles (6.5 km; 4.0 mi) southeast of Ellis Bluff.

Editorial summary

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

Editorial reviewA concise reference frame for defining the subject, testing terminology and identifying the institution closest to the evidence. The current lead gives the account dated anchors—1961—that can be checked directly. The selected authority fields contribute no independent date. For this dossier, Cumulus, Hills and hills is the immediate research focus.
Editorial analysis

Why this record matters

The phrase “hills 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

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 Aug 11, 2026. The linked authority identifier is Q5194190. Authority coordinates are -85.333, -175.000. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1961.

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.

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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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  2. Expand the search: follow Cumulus Hills primary sources, Cumulus Hills archive and Cumulus 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 Cumulus Hills” 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.