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Umiamako Glacier

glacier in Greenland

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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 authorityQ7881562 ↗
Source-derived summary

Umiamako Glacier (Danish: Umiammakku Isbræ), is a glacier in Avannaata, Greenland.

Geography

It is a marine terminating glacier outlet of the Greenland Ice Sheet. Its terminus is in the Karrat Fjord, Nordost Bay, Baffin Bay, North Atlantic Ocean.

The Umiamako Glacier flows roughly southwestwards, bending to an almost north–south direction shortly before its terminus. It is surrounded by some of the highest mountains in west Greenland.

Editorial summary

Begin with the source’s own compact description: “Umiamako Glacier” is glacier in Greenland. The dossier treats that line as a proposition to test through Umiamako, Glacier and glacier, not as a finished interpretation.

Editorial reviewA concise reference frame for defining the subject, testing terminology and identifying the institution closest to the evidence. The current 66-word lead offers orientation but no explicit four-digit date, so chronology should not be assumed. The selected authority fields contribute no independent date. For this dossier, Umiamako, Glacier and glacier is the immediate research focus.
Editorial analysis

Why this record matters

The phrase “glacier in Greenland” 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

Named sources, stable identifiers and responsible institutions provide the strongest route from overview to verifiable evidence. The source revision retrieved here is dated Jul 3, 2026. The linked authority identifier is Q7881562. Authority coordinates are 71.711, -52.449. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank.

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.

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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Verify next

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

Three-step research path

  1. Establish the record: confirm the title “Umiamako Glacier”, its source revision and the description used here.
  2. Expand the search: follow Umiamako Glacier primary sources, Umiamako Glacier archive and Umiamako 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 “Umiamako Glacier”?
  2. Which cited source is closest to the event, object or claim?
  3. What terminology or title could unlock a more precise catalogue search?
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Source & attribution

This entry incorporates text from “Umiamako 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.