The Antarctic Peninsula, known as O'Higgins Land in Chile and Tierra de San Martín in Argentina, and originally as Graham Land in the United Kingdom and the Palmer Peninsula in the United States, is the northernmost part of mainland Antarctica.
Sestrimo Glacier is the 11 km long and 4 km wide glacier on the northwest side of Trinity Peninsula in Graham Land on the Antarctic Peninsula. Situated southwest of Ogoya Glacier, west-northwest of Broad Valley and north of Cugnot Ice Piedmont. Draining the north slopes of Windy Gap, and flowing northwards east of Mount D'Urville and west of Argentino (Guerrero) Peak to enter Lafond Bay in Bransfield Strait south of Cockerell Peninsula.
Swithinbank Glacier is a glacier on the west side of Hemimont Plateau flowing north to the southeast corner of Square Bay, in Graham Land. Mapped by Falkland Islands Dependencies Survey (FIDS) from surveys and air photos, 1946–59. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) for Charles Swithinbank, British glaciologist, a participant in several British, New Zealand and American expeditions to Antarctica, 1949–62.
Jorum Glacier is a glacier draining the southeast slopes of Forbidden Plateau, and lowing east into Exasperation Inlet, just north of Caution Point, on the east coast of Graham Land, Antarctica. It was surveyed by the Falkland Islands Dependencies Survey in 1947 and 1955. The UK Antarctic Place-Names Committee name alludes to the punchbowl shape of the head of the glacier, a "jorum" being a large drinking bowl used for punch.
Toynbee Glacier is a glacier situated in the northeast portion of Alexander Island, Antarctica, extending 17 nautical miles (31 km) long and 5 nautical miles (9 km) wide, lying between Mount Huckle, Mount Spivey and Mount Stephenson of the northern portion of the Douglas Range on the west and Mount Tyrrell and Mount Tilley on the east. It flows north from the east face of Mount Stephenson into the George VI Ice Shelf that occupies George VI Sound. The glacier was first photographed from the air in 1937 by the British Graham Land Expedition under Rymill. Surveyed in 1948 by the Falkland Islands Dependencies Survey and named for Patrick A. Toynbee, FIDS air pilot at Stonington Island in 1948 and 1949.
Pluto Glacier is a glacier on the east coast of Alexander Island, Antarctica, 10 nautical miles (18 km) long and 4 nautical miles (7 km) wide, which flows east into George VI Sound to the north of Succession Cliffs. Although Pluto Glacier is not located within nearby Planet Heights, the glacier was named in association with the mountain range along with many other nearby glaciers that are named after planets of the Solar System. The glacier was first photographed from the air on November 23, 1935, by Lincoln Ellsworth and mapped from these photos by W.L.G. Joerg. Roughly surveyed in 1936 by the British Graham Land Expedition (BGLE). Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) for Pluto, then considered the ninth planet of the Solar System, following Falkland Islands Dependencies Survey (FIDS) surveys in 1948 and 1949.
Evans Glacier is a gently-sloping glacier 15 nautical miles (28 km) long and 4 nautical miles (7 km) wide, draining the southeast slopes of Travnik Buttress eastwards between Rugate Ridge and Poibrene Heights to flow into Vaughan Inlet on the east coast of Graham Land, Antarctica. It was discovered by Sir Hubert Wilkins in an aerial flight, December 20, 1928, and named "Evans Inlet" by him for E.S. Evans of Detroit. A further survey by the Falkland Islands Dependencies Survey in 1955 reported that this low-lying area is not an inlet, but is formed by the lower reaches of Hektoria Glacier and the feature now described.
Fleming Glacier is a broad glacier 25 nautical miles (46 km) long on the west side of the Antarctic Peninsula, flowing west-northwest and terminating in Forster Ice Piedmont to the east of the Wordie Ice Shelf. The glacier was charted by the British Graham Land Expedition (BGLE) under John Rymill, 1934–37, and was photographed from the air by the United States Antarctic Service on September 29, 1940. This hitherto unnamed feature was named by the Advisory Committee on Antarctic Names in 1947 for Reverend W.L.S. Fleming, Dean of Trinity Hall, Cambridge University; also, chaplain, chief scientist, and geologist of the BGLE.
Russell West Glacier is a glacier, 11 nautical miles (20 km) long and 4 nautical miles (7 km) wide, which lies immediately north of Detroit Plateau and flows from Mount Canicula, Verdikal Gap and Trajan Gate westward into Bone Bay on the north side of Trinity Peninsula. This glacier together with Russell East Glacier, which flows eastward into Prince Gustav Channel on the south side of Trinity Peninsula, form a through glacier across the north part of Antarctic Peninsula. It was first surveyed in 1946 by the Falkland Islands Dependencies Survey (FIDS). Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) for V.I. Russell, surveyor and leader of the FIDS base at Hope Bay in 1946.
Remus Glacier is a glacier, 8 nautical miles (15 km) long, which flows from the north slopes of Mount Lupa northwestward along the northeast side of the Blackwall Mountains into Providence Cove, Neny Fjord, on the west coast of Graham Land. The lower reaches of the glacier were first roughly surveyed in 1936 by the British Graham Land Expedition (BGLE) under Rymill. Resurveyed in 1948-49 by the Falkland Islands Dependencies Survey (FIDS), who so named it for its association with Romulus Glacier, whose head lies near the head of this glacier.
Vallot Glacier is a glacier flowing northwest to Laubeuf Fjord close south of Lewis Peaks, on Arrowsmith Peninsula in Graham Land. It was mapped by the Falkland Islands Dependencies Survey (FIDS) from surveys and air photos, 1948–59, and was named by the United Kingdom Antarctic Place-Names Committee (UK-APC) for Joseph Vallot, a French naturalist and glaciologist who first measured the surface velocity of a glacier over a long period, in Switzerland, 1891–99.
Verdikal Gap is the flat ice-covered saddle with an elevation of 801 m located on Trinity Peninsula in Graham Land, Antarctica. It is part of the ice divide between Bransfield Strait and Prince Gustav Channel. It extends 5.3 km between Louis-Philippe Plateau to the north and Mount Canicula and Trakiya Heights to the south, and overlooks Russell West Glacier to the west and Russell East Glacier to the southeast.
Belgun Peak is the ice-covered peak with precipitous, partly ice-free west slopes, rising to 1205 m in the northwest extremity of Trakiya Heights on Trinity Peninsula in Graham Land, Antarctica. It is situated on the east side of Zlidol Gate, surmounting the head of Russell West Glacier to the north, and the upper course of Victory Glacier to the south.
Lepitsa Peak is the ice-covered peak rising to 1110 m in the northeast foothills of Detroit Plateau on Trinity Peninsula in Graham Land, Antarctica. It is situated on the west side of Zlidol Gate, surmounting the head of Russell West Glacier to the north, and the upper course of Victory Glacier to the southeast.
Dreatin Glacier is the 12 km long and 7.5 km wide glacier on the northeast side of Detroit Plateau on Trinity Peninsula in Graham Land, Antarctica. It lies southwest of Znepole Ice Piedmont and north of Aitkenhead Glacier, draining the area southwest of Mount Bradley and north of Tufft Nunatak, and flowing southeastwards into Prince Gustav Channel, Weddell Sea west of Marmais Point.