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Gould 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 revisionMar 11, 2026
Entity authorityQ5588274 ↗
Source-derived summary

Gould Glacier () is a glacier, 12 miles (19 km) long, on the east coast of Graham Land, Antarctica, flowing south-east into Mill Inlet, to the west of Aagaard Glacier. It was first surveyed by the Falkland Islands Dependencies Survey in 1946–47, and named "East Gould Glacier". Together with "West Gould Glacier" it was reported to fill a transverse depression across Graham Land, but further survey in 1957 showed that there is no close topographical alignment between the two. The name Gould Glacier, after Rupert T. Gould, a British polar historian and cartographer, is now only applied to this glacier, and the west glacier is now called Erskine Glacier.

References

This article incorporates public domain material from "Gould Glacier". Geographic Names Information System. United States Geological Survey.

Editorial summary

“Gould Glacier” enters the record as glacier in Antarctica. Crown Archives preserves that source wording while asking what Gould, 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—1946, 1957—that can be checked directly. The selected authority fields contribute no independent date. Its strongest next move is a source search built around Gould, Glacier and glacier.
Editorial analysis

Why this record matters

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

Evidence profile

The citation trail is more important than the brevity of the summary: it shows where individual claims can be examined in context. The source revision retrieved here is dated Mar 11, 2026. The linked authority identifier is Q5588274. Authority coordinates are -66.783, -64.650. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1946 and 1957.

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.

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

Three-step research path

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

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Source & attribution

This entry incorporates text from “Gould 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.