Drygalski Glacier (Antarctica)
glacier in Antarctica

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.
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.
Why this record matters
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.
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.
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.
- Subject orientation
- Search vocabulary
- Locating named sources
The closest primary source, responsible institution and strongest cited specialist reference.
Three-step research path
- Establish the record: confirm the title “Drygalski Glacier (Antarctica)”, its source revision and the description used here.
- Expand the search: follow Drygalski Glacier (Antarctica) primary sources, Drygalski Glacier (Antarctica) archive and Drygalski research across catalogues and specialist indexes.
- Test the account: compare the strongest cited source with the responsible institution’s current record and note any disagreement.
Questions for further research
- Which source most directly establishes the central claim about “Drygalski Glacier (Antarctica)”?
- Which institution is responsible for the underlying evidence?
- What terminology or title could unlock a more precise catalogue search?
Search terms from this dossier
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.