The Dennistoun Glacier is a glacier, 50 nautical miles long, draining the northern slopes of Mount Black Prince, Mount Royalist and Mount Adam in the Admiralty Mountains of Victoria Land, Antarctica. It flows northwest between the Lyttelton Range and Dunedin Range, turning east on rounding the latter range to enter the sea south of Cape Scott.
The Everett Range is a rugged, mainly ice-covered range nearly 60 nautical miles long between Greenwell Glacier and Ebbe Glacier in northwest Victoria Land, Antarctica.
The Lyttelton Range is a narrow northwest-trending mountain range located south of Dunedin Range in the Admiralty Mountains of Antarctica. The range is 16 nautical miles long and forms the western wall of the upper part of the Dennistoun Glacier.
The Dunedin Range is a northwest-trending mountain range, 23 nautical miles long and 2 to 4 nautical miles wide. It is located 5 nautical miles east of Lyttelton Range in the Admiralty Mountains of Victoria Land, Antarctica.
The Homerun Range is a northwest-trending range, 28 nautical miles long and 2 to 7 nautical miles wide, east of Everett Range at the heads of the Ebbe Glacier and Tucker Glacier in Victoria Land, Antarctica.
The Anare Mountains are a large group of mainly snow-covered peaks and ridges along the northern coast of Victoria Land, Antarctica. The group is bounded on the north and east by the Pacific Ocean, on the west by Lillie Glacier, and on the south by Ebbe Glacier and Dennistoun Glacier. They are north of the Concord Mountains and east of the Bowers Mountains.
Lillie Glacier is a large glacier in Antarctica, about 100 nautical miles long and 10 nautical miles wide. It lies between the Bowers Mountains on the west and the Concord Mountains and Anare Mountains on the east, flowing to Ob' Bay on the coast and forming the Lillie Glacier Tongue.
Bowers Mountains is a group of north–south trending mountains in Antarctica, about 90 nautical miles long and 35 nautical miles wide, bounded by the coast on the north and by the Rennick Glacier, Canham Glacier, Black Glacier and Lillie Glacier in other quadrants. They are west of the Usarp Mountains, north of the Freyberg Mountains, northeast of the Concord Mountains, east of the Anare Mountains.
Concord Mountains is a group name applied to a complex system of ranges in northwest Victoria Land, Antarctica. They comprise the Everett Range, Mirabito Range, King Range, Leitch Massif, East Quartzite Range and West Quartzite Range. They are north of the Admiralty Mountains, northeast of the Victory Mountains, southeast of the Bowers Mountains and south of the Anare Mountains.
Tucker Glacier is a major valley glacier of Victoria Land, Antarctica, about 90 nautical miles long, flowing southeast between the Admiralty Mountains and the Victory Mountains to the Ross Sea. There is a snow saddle at the glacier's head, just west of Homerun Range, from which the Ebbe Glacier flows northwestward.
The Victory Mountains is a major group of mountains in Victoria Land, Antarctica, about 100 nautical miles long and 50 nautical miles wide, which is bounded primarily by Mariner and Tucker glaciers and the Ross Sea. They are north of the Mountaineer Range, east of the Freyberg Mountains and south of the Concord Mountains and the Admiralty Mountains. The division between the Victory Mountains and the Concord Mountains is not precise but apparently lies in the vicinity of Thomson Peak.
Quam Heights is a mostly snow-covered heights, 15 nautical miles long and 4 nautical miles wide, rising over 1,000 metres (3,300 ft) and forming the coastline between the Barnett Glacier and Dennistoun Glacier in northern Victoria Land, Antarctica.
Barnett Glacier is a large glacier in the Anare Mountains that flows east along the south side of Tapsell Foreland into Smith Inlet, northern Victoria Land, Antarctica.
Pitkevitch Glacier is a glacier, 20 nautical miles long, flowing north from the Admiralty Mountains along the west side of DuBridge Range in Antarctica. The glacier reaches the sea just east of Atkinson Cliffs, where it forms Anderson Icefalls. A portion of the terminus merges northwestward with Fendley Glacier.
The Findlay Range71°39′S167°22′E is a range lying parallel to and west of Lyttelton Range, extending between Grigg Peak and Sorensen Peak.
Mount Freeman is a prominent mountain, 2,880 metres (9,450 ft) high, surmounting the base of Walker Ridge, 2 nautical miles northwest of Mount Lepanto, in the Victory Mountains of Victoria Land, Antarctica.
The Hedgpeth Heights are mainly snow-covered heights, 14 nautical miles long and with peaks rising to 1,300 metres (4,300 ft), located 2 nautical miles southwest of the Quam Heights in the Anare Mountains of Victoria Land, Antarctica.
The Saxby Range is a broad mountain range, rising to 2,450 metres (8,040 ft), in the Victory Mountains of Victoria Land, Antarctica. It is bounded by Jutland Glacier, Tucker Glacier, Pearl Harbor Glacier, and Midway Glacier.
Robinson Heights in Antarctica are the mainly ice-covered heights 2,170 metres (7,120 ft), elliptical in plan and 15 nautical miles long, which rise south of Anare Pass and form the northwest end of the Admiralty Mountains, Antarctica.
The McGregor Range is a mountain range 13 nautical miles long in the south-central Admiralty Mountains, Antarctica. The range is circumscribed by the flow of the Tucker Glacier, Leander Glacier, Fitch Glacier and Man-o-War Glacier.
