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Newall Glacier

glacier of the Asgard Range

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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 authorityQ7016555
Source-derived summary

The Newall Glacier (77°30′S 162°50′E) is a glacier in the east part of the Asgard Range of Victoria Land,

It flows east between Mount Newall and Mount Weyant into the Wilson Piedmont Glacier.

The Newall Glacier was mapped by the N.Z. Northern Survey Party of the CTAE, 1956-58, who named it after nearby Mount Newall.

Location

The Newall Glacier forms to the east of the Lacroix Glacier, which flows south into Taylor Valley.

It flows northeast, past the head of Suess Glacier, past Mount Valkyrie to the west and Mount Weyant to the east.

It turns east and is joined by the Loftus Glacier below Mount Newall.

It continues east past the head of Commonwealth Glacier and joins with Wright Lower Glacier as it flows into Wilson Piedmont Glacier.

Features

Features, from southwest to northeast, include Lyons Cone, Twickler Cone, Unwin Ledge, Hothern Cliffs, Mount Hall, Loftus Glacier, Mount Weyant, Mount Saga, Hetha Peak, Commanda Glacier and Repeater Glacier.

Lyons Cone

77.631911°S 162.504109°E / -77.631911; 162.504109.

A cone shaped peak 2.4 nautical miles (4.4 km; 2.8 mi) north-northeast of the Matterhorn, rising to 1,850 metres (6,070 ft) high on the ridge separating the heads of Lacroix Glacier, Newall Glacier, and Suess Glacier.

Named by the United States Advisory Committee on Antarctic Names (US-ACAN) after William Berry Lyons, American geochemist, veteran of expeditions to the Himalayas, Greenland, Iceland, and Antarctica, 1980-97; chief scientist, McMurdo Dry Valleys Long-Term Ecological Research (LTER) field team, 1993-97.

Editorial summary

The public source identifies “Newall Glacier” as glacier of the Asgard Range. This brief keeps that definition visible, then builds a research path around Newall, 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—1956, 1980, 1993—that can be checked directly. The selected authority fields contribute no independent date. Its value is orientation rather than verdict, with Newall, 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 “Newall Glacier”, the useful work is to connect “glacier of the Asgard Range” to the records capable of establishing context and consequence.

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 Jul 3, 2026. The linked authority identifier is Q7016555. Authority coordinates are -77.500, 162.833. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1956, 1980 and 1993.

Critical limits

The absence of detail may reflect summary conventions rather than a lack of surviving documentation. 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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Source & attribution

This entry incorporates text from Newall 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.