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Drygalski Glacier (Antarctica)

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 revisionAug 27, 2026
Entity authorityQ3108290
Source-derived summary

Drygalski Glacier (64°43′S 60°44′W) is a broad glacier, 18 nautical miles (33 km; 21 mi) long which flows southeast

from Herbert Plateau through a rectangular re-entrant to a point immediately north of Sentinel Nunatak on the east coast of Graham Land, Antarctica.

Location

Drygalski Glacier is on the Nordenskjöld Coast of the Antarctic Peninsula.

It is east of the Forbidden Plateau, southeast of the Herbert Plateau, southwest of the Detroit Plateau and northeast of the Weddell Sea.

The Foster Plateau, Anderson Peak and Seal Nunataks are to the south.

Discovery and name

Drygalski Glacier was discovered in 1902 by the Swedish Antarctic Expedition (SwedAE), under Otto Nordenskiöld, and named "Drygalski Bay" after Professor Erich von Drygalski.

The feature was determined to be a glacier by the Falkland Islands Dependencies Survey (FIDS) in 1947.

Upper features

Features around the head of the glacier include:

Foster Plateau

64°43′S 61°25′W.

A plateau, about 80 square miles (210 km2) in area, lying between Drygalski Glacier and Hektoria Glacier.

Photographed by the Falkland Islands and Dependencies Aerial Survey Expedition (FIDASE) in 1956-57 and mapped from these photos by the Falkland Islands Dependencies Survey (FIDS).

Named by the UK Antarctic Place-Names Committee (UK-APC) in 1960 for Richard A. Foster, FIDS leader of the Danco Island station in 1956 and 1957.

Fender Buttress

64°34′S 61°04′W.

A rock buttress rising to more than 1,600 metres (5,200 ft) high, projecting from the south side of Herbert Plateau into the head of Drygalski Glacier.

Editorial summary

The public source identifies “Drygalski Glacier (Antarctica)” as glacier in Antarctica. This brief keeps that definition visible, then builds a research path around Drygalski, Glacier and Antarctica.

Editorial reviewA dependable orientation record for establishing vocabulary, names and a first evidence trail. The current lead gives the account dated anchors—1902, 1947, 1956, 1960—that can be checked directly. The selected authority fields contribute no independent date. Its value is orientation rather than verdict, with Drygalski, Glacier and Antarctica providing the first useful test.
Editorial analysis

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A short description can identify a subject without explaining its stakes. For “Drygalski Glacier (Antarctica)”, the useful work is to connect “glacier in Antarctica” to the records capable of establishing context and consequence.

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 Aug 27, 2026. The linked authority identifier is Q3108290. Authority coordinates are -64.717, -60.733. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1902, 1947, 1956 and 1960.

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Source & attribution

This entry incorporates text from Drygalski Glacier (Antarctica)” 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.