The Balleny Islands are a series of uninhabited islands in the Southern Ocean extending from 66°15' to 67°35'S and 162°30' to 165°00'E. The group extends for about 160 km (99 mi) in a northwest-southeast direction. The islands are heavily glaciated and of volcanic origin. Glaciers project from their slopes into the sea. The islands were formed by the so-called Balleny hotspot.
The Commonwealth Range is a north-south trending range of rugged mountains, 60 nautical miles long, located within the Queen Maud Mountains on the Dufek Coast of the continent of Antarctica. The range borders the eastern side of Beardmore Glacier from Keltie Glacier to the Ross Ice Shelf. The range is southeast of the Queen Alexandra Range, which is to the west of the Beardmore Glacier. It is west of the Hughes Range and north of the Supporters Range and the Barton Mountains.
The Deep Freeze Range is a rugged mountain range, over 80 nautical miles long and about 10 nautical miles wide, rising between Priestley and Campbell Glaciers in Victoria Land, Antarctica, and extending from the edge of the polar plateau to Terra Nova Bay. It is southwest of the Southern Cross Mountains, south of the Mesa Range and northeast of the Eisenhower Range of the Prince Albert Mountains.
The Priestley Glacier is a major valley glacier, about 60 nautical miles long, originating at the edge of the Polar Plateau of Victoria Land, Antarctica. The glacier drains southeast between the Deep Freeze Range and Eisenhower Range to enter the northern end of the Nansen Ice Sheet. It was first explored by the Northern Party of the British Antarctic Expedition, 1910–13, and named for Raymond Priestley, a geologist with the Northern Party.
Wilson Hills is a group of scattered hills, nunataks and ridges that extend northwest–southeast about 70 nautical miles between Matusevich Glacier and Pryor Glacier in Antarctica.
Holder Peak is the higher (northern) peak on a rock outcrop about 4 kilometres (2.5 mi) east of Mount Caroline Mikkelsen on the Ingrid Christensen Coast of Princess Elizabeth Land, Antarctica. The peak is about 140 metres (460 ft) high.
The Worcester Range is a high coastal range, about 30 nautical miles long, in Antarctica. It stands between Skelton Glacier and Mulock Glacier on the western side of the Ross Ice Shelf. It is southwest of the Royal Society Range and north of the Conway Range of the Cook Mountains.
The Latady Mountains are a group of mountains rising west of Gardner Inlet and between Wetmore Glacier and Ketchum Glacier, in southeastern Palmer Land, Antarctica.
The Carlstrom Foothills are a group of peaks and ridges in the Churchill Mountains, Antarctica.
The Demas Range is a range about 8 nautical miles long that forms the lower east margin of the Berry Glacier in Marie Byrd Land, Antarctica. The range trends north–south culminating in Mount Goorhigian, 1,115 metres (3,658 ft) high.
Kukri Hills is a prominent east-west trending range, about 25 nautical miles (46 km) long and over 2,000 metres (6,600 ft) high, forming the divide between Ferrar Glacier on the south and Taylor Glacier and Taylor Valley on the north, in Victoria Land, Antarctica. They are south of the Asgard Range, east of the Quartermain Mountains and north of the Royal Society Range.
Strover Peak is a low rock peak along the coast of Antarctica, standing 6 nautical miles (11 km) west-northwest of Mount Caroline Mikkelsen. Mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition, 1936–37, and named "Svartmulen". Renamed by Antarctic Names Committee of Australia (ANCA) for W.G.H. Strover, radio supervisor at Davis Station in 1963 and a member of the ANARE party that surveyed this feature. Acceptance of Strover Peak curtails the repetitive use of "Svart" (black) in Antarctic names.
Matusevich Glacier is a broad glacier about 50 nautical miles long, with a well developed glacier tongue, flowing to the coast of East Antarctica between the Lazarev Mountains and the northwestern extremity of the Wilson Hills.
Palmer Point is a rock point on the coast of Antarctica, about 2 nautical miles (3.7 km) west of Strover Peak and 8 nautical miles (15 km) west-northwest of Mount Caroline Mikkelsen. Photographed by U.S. Navy Operation Highjump, 1946–47. Visited by I.R. McLeod, geologist with the ANARE Prince Charles Mountains survey party, 1969. Named by Antarctic Names Committee of Australia (ANCA) for J. Palmer, helicopter pilot with ANARE in 1968.
The Marshall Mountains are a group of mountains overlooking Beardmore Glacier in the Queen Alexandra Range, Antarctica. They are bounded on the north by Berwick Glacier, and on the south by Swinford Glacier.
The Hutton Mountains are a group of mountains in southeast Palmer Land, Antarctica, bounded on the southwest by Johnston Glacier, on the northwest by Squires Glacier, on the north by Swann Glacier, and on the east by Keller Inlet.
McCarthy Nunatak is a small nunatak, the top of which is almost at the same level as the surrounding ice plateau, about 5 nautical miles (9 km) southeast of Depot Peak, Mac. Robertson Land, Antarctica. It was discovered from Australian National Antarctic Research Expeditions (ANARE) aircraft in 1970, and was named by the Antarctic Names Committee of Australia after I. McCarthy, a senior weather observer at Mawson Station in 1970, and a member of the ANARE Prince Charles Mountains survey party in 1971.
The Tomilin Glacier is a glacier over 15 nautical miles long, draining north from Pope Mountain in the central Wilson Hills. It enters the sea east of Goodman Hills and Cape Kinsey, forming a substantial glacier tongue.
Blue Glacier is a large glacier which flows into Bowers Piedmont Glacier about 10 nautical miles south of New Harbour, in Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition (BrNAE) under Robert Falcon Scott, 1901–04, who gave it this name because of its clear blue ice at the time of discovery.
This article incorporates public domain material from "Young Peak". Geographic Names Information System . United States Geological Survey. 
