Joinville Island is the largest island of the Joinville Island group, about 40 nautical miles long in an east–west direction and 12 nautical miles wide, lying off the northeastern tip of the Antarctic Peninsula, from which it is separated by the Antarctic Sound.
Hope Bay is a bay 3 nautical miles long and 2 nautical miles wide, indenting the tip of the Antarctic Peninsula and opening on Antarctic Sound.
James Ross Island is a large island off the southeast side and near the northeastern extremity of the Antarctic Peninsula, from which it is separated by Prince Gustav Channel. Rising to 1,630 metres (5,350 ft), it is irregularly shaped and extends 40 nautical miles in a north–south direction.
Northeast Glacier is a steep, heavily crevassed glacier, 13 nautical miles long and 5 nautical miles wide at its mouth, which flows from McLeod Hill westward and then south-westwards into Marguerite Bay between the Debenham Islands and Roman Four Promontory, on the west coast of Graham Land, Antarctica.
The Longing Peninsula is a peninsula 9 nautical miles long terminating in Cape Longing, situated at the northeast end of the Nordenskjöld Coast where it separates the Larsen Ice Shelf from the Prince Gustav Ice Shelf.
The Prince Gustav Channel is a strait about 80 nautical miles long and from 4 to 15 nautical miles wide, separating James Ross Island and Vega Island from the Trinity Peninsula, Antarctica.
Blaiklock Island is a high and rugged, irregular-shaped island 17 kilometres (9 nmi) long, lying between Bigourdan Fjord and Bourgeois Fjord. It is separated from Pourquoi Pas Island by The Narrows and from the west coast of Graham Land by Jones Channel. The feature was partially surveyed in 1936 by the British Graham Land Expedition under Rymill, at which time it was charted as a promontory. It was determined to be an island in 1949 by Kenneth V. Blaiklock, a Falkland Islands Dependencies Survey (FIDS) surveyor for whom it is named.
Ulu Peninsula is that portion of James Ross Island northwest of the narrow neck of land between Rohss Bay and Croft Bay, extending from Cape Obelisk to Cape Lachman, in Antarctica.
Aitkenhead Glacier is a 10 nautical miles long glacier flowing east-southeast from the Detroit Plateau, Graham Land, into Prince Gustav Channel.
Eagle Island is an island 5 nautical miles long and 4 nautical miles wide, rising to 560 metres (1,840 ft) on the NE side. It is the largest island in the archipelago which lies between Trinity Peninsula and Vega Island. Eagle Island is separated from the Antarctic mainland by the 1.77 km wide Aripleri Passage. It is volcanic in origin, having been K-Ar dated 1.7 ± 0.2 and 2.0 ± 0.2 million years old. It forms part of the James Ross Island Volcanic Group.
Orford Cliff is a coastal cliff of Pernik Peninsula, Loubet Coast in Graham Land, overlooking the east side of Lallemand Fjord just east of Andresen Island. Surveyed by Falkland Islands Dependencies Survey (FIDS) in 1956. Named for Michael J.H. Orford, FIDS assistant surveyor at Detaille Island in 1956, a member of the party which found a route from Detaille Island to Avery Plateau, via Orford Cliff and Murphy Glacier.
Nobby Nunatak is a nunatak, 270 m, standing 1 nautical mile (1.9 km) south of Lake Boeckella and 1 nautical mile (1.9 km) east of Mount Flora, at the northeast end of Antarctic Peninsula.
Croft Bay is a bay which indents the north-central side of James Ross Island and forms the southern part of Herbert Sound, south of the northeastern end of the Antarctic Peninsula.
Cugnot Ice Piedmont is an ice piedmont in Trinity Peninsula, Antarctica. It is about 15 nautical miles long and between 3 and 6 nautical miles wide, extending from Russell East Glacier to Eyrie Bay and bounded on the landward side by Louis Philippe Plateau.
Duse Bay is a bay indenting the south side of Trinity Peninsula between View Point and the western side of Tabarin Peninsula, Antarctica.
Sjögren Glacier is a glacier 15 nautical miles long in the south part of Trinity Peninsula, Antarctica. It flows southeast from Detroit Plateau to the south side of Mount Wild, where it enters Prince Gustav Channel.
View Point is 150m long eastern tip of a promontory, on Antarctica, forming the west side of the entrance to Duse Bay on the south coast of Trinity Peninsula, on the northern portion of the Antarctic Peninsula. Situated 6.79 km east of Skomlya Hill and 6.45 km southeast of Boil Point. Discovered by a party under J. Gunnar Andersson of the Swedish Antarctic Expedition, 1901-04. So named by the Falkland Islands Dependencies Survey (FIDS) following their survey of the area in 1945 because from this promontory, good panoramic photographs were obtained.
Victory Glacier is a gently sloping glacier, 8 nautical miles long, flowing east-southeast from the north end of Detroit Plateau on Trinity Peninsula to Prince Gustav Channel immediately north of Pitt Point. It is bounded by Trakiya Heights to the north and Kondofrey Heights to the south.
Znepole Ice Piedmont is the glacier extending 13 kilometres (8.1 mi) in northwest-southeast direction and 7.5 kilometres (4.7 mi) wide on Trinity Peninsula in Graham Land, Antarctica.
Bone Bay is a rectangular bay along the northwest coast of Trinity Peninsula, Antarctica. It is nearly 10 nautical miles wide at the entrance between Notter Point and Cape Roquemaurel.
