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Armira 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 authorityQ4793588 ↗
Source-derived summary

Armira Glacier (Bulgarian: ледник Армира, romanized: lednik Armira, IPA: [ˈlɛdnik ɐrˈmirɐ]) is a 1.6 nautical miles (3.0 km; 1.8 mi) long glacier on Smith Island in the South Shetland Islands, Antarctica draining the southeast slopes of Imeon Range southeast of Slaveykov Peak and east of Neofit Peak. It is situated southwest of Dragoman Glacier and northeast of Gramada Glacier, and flows southeastward into Yarebitsa Cove on Osmar Strait. Bulgarian early mapping in 2009. The glacier is named after Armira River in southeastern Bulgaria.

See also

List of glaciers in the Antarctic

Glaciology

Maps

Chart of South Shetland including Coronation Island, &c. from the exploration of the sloop Dove in the years 1821 and 1822 by George Powell Commander of the same. Scale ca. 1:200000. London: Laurie, 1822.

L.L. Ivanov.

Editorial summary

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

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—2009, 1821, 1822—that can be checked directly. The selected authority fields contribute no independent date. For this dossier, Armira, Glacier and glacier is the immediate research focus.
Editorial analysis

Why this record matters

The phrase “glacier in Antarctica” 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 Q4793588. Authority coordinates are -63.024, -62.550. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 2009, 1821 and 1822.

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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  2. Expand the search: follow Armira Glacier primary sources, Armira Glacier archive and Armira 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.

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Source & attribution

This entry incorporates text from “Armira 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.