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Tundzha 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 authorityQ7852918 ↗
Source-derived summary

Tundzha Glacier (Bulgarian: ледник Тунджа, romanized: lednik Tundzha, IPA: [ˈlɛdnik ˈtund͡ʒɐ]) is a glacier on Livingston Island in the South Shetland Islands, Antarctica situated east-southeast of Berkovitsa Glacier, west of Saedinenie Snowfield, northwest of Pimpirev Glacier, north of Kamchiya Glacier, and east-northeast of Verila Glacier. It is bounded by Snow Peak to the west, Teres Ridge to the east and the glacial divide between the Drake Passage and Bransfield Strait to the south. The glacier extends 7.5 nautical miles (13.9 km; 8.6 mi) in east-west direction and 2.4 nautical miles (4.4 km; 2.8 mi) in the north-south direction, and drains northwards into Hero Bay between Avitohol Point and Siddins Point.

The feature was named after the Tundzha River in Bulgaria.

Location

The midpoint of the glacier is located at 62°35′40″S 60°30′30″W (Bulgarian mapping in 2009).

See also

List of glaciers in the Antarctic

Glaciology

Maps

L.L. Ivanov et al. Antarctica: Livingston Island and Greenwich Island, South Shetland Islands. Scale 1:100000 topographic map. Sofia: Antarctic Place-names Commission of Bulgaria, 2005.

L.L. Ivanov.

Editorial summary

Begin with the source’s own compact description: “Tundzha Glacier” is glacier in Antarctica. The dossier treats that line as a proposition to test through Tundzha, 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, 2005—that can be checked directly. The selected authority fields contribute no independent date. For this dossier, Tundzha, 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 Q7852918. Authority coordinates are -62.594, -60.508. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 2009 and 2005.

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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  2. Expand the search: follow Tundzha Glacier primary sources, Tundzha Glacier archive and Tundzha research across catalogues and specialist indexes.
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Source & attribution

This entry incorporates text from “Tundzha 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.