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Conger 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 6, 2026
Entity authorityQ5160456 ↗
Source-derived summary

Conger Glacier (66°2′S 103°33′E) is a glacier 5 nautical miles (9 km) east of Glenzer Glacier, flowing north into the eastern part of the Shackleton Ice Shelf. It was mapped by Gardner Dean Blodgett (1955) from air photos taken by U.S. Navy Operation Highjump (1946–47). It was named by the Advisory Committee on Antarctic Names for Richard R. Conger, chief photographer's mate with U.S. Navy Operation Windmill (1947–48), who assisted in establishing astronomical control stations along the coast from Wilhelm II Coast to Budd Coast.

On 25 March 2022, it was reported that Conger Ice Shelf had collapsed around ten days earlier, as evidenced by satellite data. The collapse had not been anticipated by experts, although a gradual shrinking of the glacier had been observed since the mid-2000s, and a more rapid one since early 2020. Whether the collapse was related to the preceding abnormally high temperatures in the area was not immediately clear. An ice shelf is a large floating platform of ice that forms where a glacier or ice sheet flows down to a coastline and onto the ocean surface; it stops a glacier from rapidly flowing into an ocean.

See also

List of glaciers in the Antarctic

Glaciology

References

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

Editorial summary

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

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—1955, 1946, 1947, 2022—that can be checked directly. The selected authority fields contribute no independent date. The account is most persuasive where Conger, Glacier 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

Named sources, stable identifiers and responsible institutions provide the strongest route from overview to verifiable evidence. The source revision retrieved here is dated Jul 6, 2026. The linked authority identifier is Q5160456. Authority coordinates are -66.033, 103.550. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1955, 1946, 1947 and 2022.

Critical limits

The absence of detail may reflect summary conventions rather than a lack of surviving documentation. The source lead contains qualifying language; that uncertainty should survive quotation, summary and reuse. 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 Conger Glacier primary sources, Conger Glacier archive and Conger research across catalogues and specialist indexes.
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Source & attribution

This entry incorporates text from “Conger 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.