Skelton Glacier is a large glacier flowing from the polar plateau into the Ross Ice Shelf at Skelton Inlet on the Hillary Coast, south of Victoria Land, Antarctica.
The Churchill Mountains are a mountain range group of the Transantarctic Mountains System, located in the Ross Dependency region of Antarctica. They border on the western side of the Ross Ice Shelf, between Byrd Glacier and Nimrod Glacier.
The Royal Society Range is a majestic range of mountains in Victoria Land, Antarctica, rising to 4,025 metres (13,205 ft) along the west shore of McMurdo Sound between the Koettlitz, Skelton and Ferrar Glaciers. They are south of the Kukri Hills, southeast of the Quartermain Mountains, and northeast of the Worcester Range.
The Prince Albert Mountains are a major mountain group in Antarctica over 200 nautical miles long. Located in Victoria Land, they run north–south between the Priestley Glacier to the north and Ferrar Glacier to the south. They are south of the Deep Freeze Range and north of the Kirkwood Range.
Convoy Range is a broad range in Antarctica. It is south of the Kirkwood Range and north of the Clare Range.
Mount Lister is a massive mountain, 4,025 metres (13,205 ft) high, forming the highest point in the Royal Society Range of Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition (1901–1904) which named it for Lord Joseph Lister, President of the Royal Society, 1895–1900.
Victoria Valley is an extensive ice-free valley, formerly occupied by a large glacier, extending from Victoria Upper Glacier to Victoria Lower Glacier in Victoria Land, Antarctica. It is one of the larger McMurdo Dry Valleys.
The Olympus Range is a primarily ice-free mountain range of Victoria Land, Antarctica, with peaks over 2,000 metres (6,600 ft) high, between Victoria Valley and McKelvey Valley on the north and Wright Valley on the south. It is south of the Clare Range and north of the Asgard Range.
The Nash Range is a mainly ice-covered coastal range in the Churchill Mountains of Antarctica.
Fry Glacier is a glacier draining the slopes at the northeast corner of the Convoy Range and flowing along the south end of the Kirkwood Range into Tripp Bay, Victoria Land, Antarctica. It was first charted by the British Antarctic Expedition, 1907–09, and named for A.M. Fry, a contributor to the expedition.
Greenville Valley is the large mainly ice-free valley lying south of Elkhorn Ridge in the Convoy Range of Victoria Land, Antarctica. A lobe of the Northwind Glacier flows a short distance west into the mouth of the valley. Near the head of the valley the south wall is breached by the entrance to Merrell Valley.
Evans Piedmont Glacier is a broad ice sheet occupying the low-lying coastal platform between Tripp Island and Cape Archer in Victoria Land, Antarctica.
Flagship Mountain is a prominent, conical rock peak, 1,720 metres (5,640 ft) high, surmounting the south part of the large rock mass between Northwind Glacier and Atka Glacier.
The Gonville and Caius Range is a range of peaks, 1,000 to 1,500 metres high, between Mackay Glacier and Debenham Glacier in Victoria Land, Antarctica.
Harvey Summit is a peak 2,644 metres (8,675 ft) high at the head of McDermott Glacier in the Royal Society Range of Victoria Land, Antarctica. It was named by the United States Advisory Committee on Antarctic Names (US-ACAN) after John W. Harvey of the National Solar Observatory who, along with Thomas L. Duvall, Jr. and Martin A. Pomerantz, conducted research in helioseismology at the South Pole for some years from 1980 onwards.
The Mawson Glacier is a large glacier on the east coast of Victoria Land, Antarctica, descending eastward from the Antarctic Plateau to the north of Trinity Nunatak and the Kirkwood Range, to enter the Ross Sea, where it forms the Nordenskjöld Ice Tongue. The glacier was first mapped by the British Antarctic Expedition (1907–09) and named for Douglas Mawson, the expedition physicist, who later led two other Antarctic expeditions, 1911–14, and 1929–31.
Mackay Glacier is a large glacier in Victoria Land, descending eastward from the Antarctic Plateau, between the Convoy Range and Clare Range, into the southern part of Granite Harbour. It was discovered by the South magnetic pole party of the British Antarctic Expedition, 1907–09, and named for Alistair Mackay, a member of the party. The glacier's tongue is called Mackay Glacier Tongue. First mapped by the British Antarctic Expedition, 1910–13 and named for Alistair F. Mackay, a member of the party. Its mouth is south of the Evans Piedmont Glacier and the Mawson Glacier. It is north of the Wilson Piedmont Glacier and the Ferrar Glacier.
Saint Johns Range is a crescent-shaped mountain range about 20 nautical miles long, in Victoria Land, Antarctica. It is bounded on the north by the Cotton Glacier, Miller Glacier and Debenham Glacier, and on the south by Victoria Valley and the Victoria Upper Glacier and Victoria Lower Glacier.
Staten Island Heights is a predominantly flat, ice-covered upland between Greenville Valley and Alatna Valley in the Convoy Range of Victoria Land, Antarctica.
Rampart Ridge is a prominent broken ridge on the west side of the Royal Society Range, Antarctica. It stands north of Rutgers Glacier and extends from The Spire to Bishop Peak.
