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Tucker Glacier

glacier in Victoria Land, east 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 authorityQ2459130
Source-derived summary

Tucker Glacier (72°32′S 169°15′E) is a major valley glacier of Victoria Land, Antarctica, about 90 nautical miles (170 km; 100 mi) long, flowing southeast between the Admiralty Mountains and the Victory Mountains to the Ross Sea. There is a snow saddle at the glacier's head, just west of Homerun Range, from which the Ebbe Glacier flows northwestward.

Exploration and naming

Explored by New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1957–58, and named by them after Tucker Inlet, the ice-filled coastal indentation at the mouth of this glacier named by Captain James Clark Ross in 1841.

Geography

The upper reaches of the Tucker Glacier south of the Homerun Range saddle with the Greenwell Glacier and Jutland Glacier, in the Lillie Glacier basin.

The Tucker Glacier is fed by the Rastorfer Glacier from the left (north) and then by the Leander Glacier after it has been joined by the Church Glacier.

South of the McGregor Range the Man-O-War Glacier enters from the northeast, combined with the Freimanis Glacier from the east.

Tributaries of the Man-O-War Glacier include the Massey Glacier, Deming Glacier and Fitch Glacier.

Tributaries of the Tucker Glacier from the Admiralty Mountains to the east below the Freimants Glacier include the Tocci Glacier, Helman Glacier, Tyler Glacier, Staircase Glacier, Kelly Glacier and Towles Glacier.

To the south of the Pemmican Step, the Montecchi Glacier enters from the west.

South of that the Pearl Harbor Glacier enters the Tucker Glacier from the west, flowing to the north of the Cartographers Range.

Editorial summary

“Tucker Glacier” enters the record as glacier in Victoria Land, east Antarctica. Crown Archives preserves that source wording while asking what Tucker, Glacier and glacier can confirm, complicate or overturn.

Editorial reviewA practical starting point whose main value is the path it opens into stronger specialist and primary sources. The current lead gives the account dated anchors—1957, 1841—that can be checked directly. The selected authority fields contribute no independent date. Its strongest next move is a source search built around Tucker, Glacier and glacier.
Editorial analysis

Why this record matters

“Tucker Glacier” is worth following because a concise public description often conceals a longer documentary argument. Here, Tucker, Glacier and glacier provides the most credible route into that argument.

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 Q2459130. Authority coordinates are -72.533, 169.250. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1957 and 1841.

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 Tucker 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.