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Wilson Piedmont 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 authorityQ3761722
Source-derived summary

Wilson Piedmont Glacier (77°15′S 163°10′E) is a large piedmont glacier extending from Granite Harbour to Marble Point on the coast of Victoria Land.

Discovery and name

The Wilson Piedmont Glacier was discovered by the Discovery expedition, 1901–1904. The British Antarctic Expedition, 1910–1913, named the feature for Dr. Edward A. Wilson, surgeon and artist with Scott's first expedition and chief of the scientific staff with the second. Wilson lost his life on the way back from the South Pole with Scott.

Glaciology

The Wilson Piedmont Glacier extends along the coastal plain of the west coast of the Ross Sea from Granite Harbor south to McMurdo Sound.

Most of its input is from direct precipitation, but it receives some inflows from alpine glaciers.

It has a broad dome with a divide near the McMurdo Dry Valleys.

Most ice flows east to the Ross Sea, where the glacier terminates and comes afloat in the sea along its eastern margin.

Some ice flows west and contributes to the Wright Lower Glacier and the Victoria Lower Glacier.

Editorial summary

This brief starts where responsible research should: with the source description of “Wilson Piedmont Glacier” as glacier in Antarctica. Everything that follows is an evidence route, not borrowed authority.

Editorial reviewA dependable orientation record for establishing vocabulary, names and a first evidence trail. The current lead gives the account dated anchors—1901, 1904, 1910, 1913—that can be checked directly. The selected authority fields contribute no independent date. The account is most persuasive where Wilson, Piedmont and Glacier can be independently traced.
Editorial analysis

Why this record matters

The subject matters to the general reference register because the source frames it as glacier in Antarctica. Its deeper value depends on whether names, dates, institutions and citations support that framing.

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 Q3761722. Authority coordinates are -77.250, 163.167. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1901, 1904, 1910 and 1913.

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.

How to read it

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.

Best used for
  • Subject orientation
  • Search vocabulary
  • Locating named sources
Verify next

The closest primary source, responsible institution and strongest cited specialist reference.

Three-step research path

  1. Establish the record: confirm the title “Wilson Piedmont Glacier”, its source revision and the description used here.
  2. Expand the search: follow Wilson Piedmont Glacier primary sources, Wilson Piedmont Glacier archive and Wilson 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.

Questions for further research

  1. Which source most directly establishes the central claim about “Wilson Piedmont Glacier”?
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  3. Which cited source is closest to the event, object or claim?
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Source & attribution

This entry incorporates text from Wilson Piedmont 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.