Antarctic Plateau margin
E1281230
UNEXPLORED
The Antarctic Plateau margin is the transitional region where the high, icy interior of Antarctica descends toward the surrounding coastal mountain ranges and ice shelves.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Antarctic Plateau margin canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T17657259 — resolving that mention is where its identity was fixed. The disambiguator weighed these candidate entities and picked the highlighted one (or “None”, minting a new entity). This is how homonymy is resolved: the same surface form can point to different entities.
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Antarctic Plateau margin Context triple: [Mühlig-Hofmann Mountains, locatedOn, Antarctic Plateau margin]
-
A.
Antarctic Plate boundary region
The Antarctic Plate boundary region is a geologically active zone encircling Antarctica where the Antarctic Plate interacts with neighboring tectonic plates, giving rise to features such as mid-ocean ridges, fracture zones, and subduction-related structures.
-
B.
East Antarctic margin of the Southern Ocean
The East Antarctic margin of the Southern Ocean is the remote, ice-dominated oceanic boundary fringing East Antarctica, characterized by extensive continental shelves, strong katabatic winds, and crucial roles in global ocean circulation and climate.
-
C.
South American–Scotia plate boundary zone
The South American–Scotia plate boundary zone is a complex tectonic region in the South Atlantic where the South American Plate interacts with the Scotia Plate through a network of microplates, transform faults, and subduction-related structures.
-
D.
Amery Ice Shelf region
The Amery Ice Shelf region is a vast coastal area of East Antarctica dominated by one of the continent’s largest ice shelves, where thick glacial ice flows from the interior into the Southern Ocean.
-
E.
South Sandwich microplate
The South Sandwich microplate is a small tectonic plate in the South Atlantic associated with the South Sandwich Islands and an active subduction zone and volcanic arc east of the Scotia Plate.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: Antarctic Plateau margin Target entity description: The Antarctic Plateau margin is the transitional region where the high, icy interior of Antarctica descends toward the surrounding coastal mountain ranges and ice shelves.
-
A.
Antarctic Plate boundary region
The Antarctic Plate boundary region is a geologically active zone encircling Antarctica where the Antarctic Plate interacts with neighboring tectonic plates, giving rise to features such as mid-ocean ridges, fracture zones, and subduction-related structures.
-
B.
East Antarctic margin of the Southern Ocean
The East Antarctic margin of the Southern Ocean is the remote, ice-dominated oceanic boundary fringing East Antarctica, characterized by extensive continental shelves, strong katabatic winds, and crucial roles in global ocean circulation and climate.
-
C.
South American–Scotia plate boundary zone
The South American–Scotia plate boundary zone is a complex tectonic region in the South Atlantic where the South American Plate interacts with the Scotia Plate through a network of microplates, transform faults, and subduction-related structures.
-
D.
Amery Ice Shelf region
The Amery Ice Shelf region is a vast coastal area of East Antarctica dominated by one of the continent’s largest ice shelves, where thick glacial ice flows from the interior into the Southern Ocean.
-
E.
South Sandwich microplate
The South Sandwich microplate is a small tectonic plate in the South Atlantic associated with the South Sandwich Islands and an active subduction zone and volcanic arc east of the Scotia Plate.
- F. None of above. chosen
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.