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Mount Dechen

hill in New Zealand

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General referenceInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionAug 15, 2026
Entity authorityQ31663382
Source-derived summary

Mount Dechen is a 2,643-metre-elevation (8,671-foot) mountain in the West Coast Region of New Zealand.

Description

Mount Dechen is located in the Southern Alps of the South Island. Precipitation runoff from the mountain drains east into the Landsborough River, southwest into the headwaters of the Ōtoko River, and north into the headwaters of the Edison River. Topographic relief is significant as the summit rises 1,700 metres (5,577 feet) above the Ōtoko Valley in four kilometres, and 2,220 metres (7,283 feet) above the Landsborough Valley in four kilometres. The nearest higher peak is Mount Ward, nine kilometres to the southeast. The mountain's toponym was applied by Julius von Haast to honour his geology teacher, Ernst Heinrich Karl von Dechen (1800–1889).

Climbing

The first ascent of the summit was made in March 1935 by Marjorie Edgar-Jones, Gladys Acton-Adams, Frank Alack, and Tom Christie.

Climbing routes with the first ascents:

South Ridge – Marjorie Edgar-Jones, Gladys Acton-Adams, Frank Alack, Tom Christie – (1935)

East Face – Norman Hardie, Jim McFarlane – (1947)

North East Ridge – Trevor McCann, Maurie Bishop – (1952)

Ōtoko Couloir – Dick Tornquist, Vic McGregor, Alex Parton, John Luxton, Tim Barfoot, George Hunter – (1961)

Climate

Based on the Köppen climate classification, Mount Dechen is located in a marine west coast (Cfb) climate zone, with a subpolar oceanic climate (Cfc) at the summit. Prevailing westerly winds blow moist air from the Tasman Sea onto the mountains, where the air is forced upward by the mountains (orographic lift), causing moisture to fall in the form of rain or snow. This climate supports the Dechen and McCardell glaciers on the slopes of the peak.

Editorial summary

Begin with the source’s own compact description: “Mount Dechen” is hill in New Zealand. The dossier treats that line as a proposition to test through Mount, Dechen and hill, 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—1800, 1889, 1935, 1947—that can be checked directly. The selected authority fields contribute no independent date. For this dossier, Mount, Dechen and hill is the immediate research focus.
Editorial analysis

Why this record matters

The phrase “hill in New Zealand” 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 15, 2026. The linked authority identifier is Q31663382. Authority coordinates are -43.797, 169.756. None of the 1 selected statements returned an explicit reference. The first chronological checks are 1800, 1889, 1935 and 1947.

Critical limits

A concise general-reference account can conceal disagreements about scope, terminology or the weight assigned to individual sources. 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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Source & attribution

This entry incorporates text from Mount Dechen” 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.