Koettlitz Glacier is a large Antarctic glacier lying west of Mount Morning and Mount Discovery in the Royal Society Range, flowing from the vicinity of Mount Cocks northeastward between Brown Peninsula and the mainland into the ice shelf of McMurdo Sound.
The Taylor Glacier is a glacier in Antarctica about 35 nautical miles long, flowing from the plateau of Victoria Land into the western end of Taylor Valley, north of the Kukri Hills. It flows to the south of the Asgard Range. The middle part of the glacier is bounded on the north by the Inland Forts and on the south by Beacon Valley.
The Quartermain Mountains are a group of exposed mountains in Antarctica, about 20 nautical miles long, typical of ice-free features of the McMurdo Dry Valleys, Victoria Land. They are located south of Taylor Glacier and bounded by Finger Mountain, Mount Handsley, Mount Feather and Tabular Mountain; also including Knobhead, Terra Cotta Mountain, New Mountain, Beacon Heights, Pyramid Mountain, Arena Valley, Kennar Valley, Turnabout Valley and the several valleys and ridges within Beacon Valley.
The Labyrinth is an extensive flat upland area which has been deeply eroded, at the west end of Wright Valley, in Victoria Land, Antarctica. It was so named by the Victoria University of Wellington Antarctic Expedition (VUWAE) (1958–59) because the eroded dolerite of which it is formed gives an appearance of a labyrinth.
The Asgard Range is a mountain range in Victoria Land, Antarctica. It divides Wright Valley from Taylor Glacier and Taylor Valley. It was named by the Victoria University of Wellington Antarctic Expedition (1958–59) after Asgard, the home of the Norse gods.
The Inland Forts are a line of peaks extending between Northwest Mountain and Saint Pauls Mountain, in the Asgard Range of Victoria Land, Antarctica. The peaks were discovered by Ervon r. Koenig and named by the British National Antarctic Expedition, 1901–04.
The Insel Range is a series of ice-free flat-topped peaks resembling islands which rise above the surrounding terrain and separate McKelvey Valley from Balham Valley, in Victoria Land, Antarctica. It was so named by the Victoria University of Wellington Antarctic Expedition because of the resemblance to islands.
Taylor Valley77°37′S163°00′E is an ice-free valley about 18 nautical miles long, once occupied by the receding Taylor Glacier. It lies north of the Kukri Hills between the Taylor Glacier and New Harbour in Victoria Land, Antarctica. Taylor Valley is the southernmost of the three large McMurdo Dry Valleys in the Transantarctic Mountains, located west of McMurdo Sound.
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.
Mount Newall is a peak, 1,920 metres (6,300 ft) high, the northeast extremity of Asgard Range, in Victoria Land, Antarctica. It was discovered by the Discovery Expedition (1901–04) and named for one of the men who helped raise funds to send a relief ship for the expedition.
Wilson Piedmont Glacier is a large piedmont glacier extending from Granite Harbour to Marble Point on the coast of Victoria Land.
Wright Upper Glacier is an ice apron at the upper west end of Wright Valley in the Asgard Range, Antarctica. It is formed by a glacier flowing east from the inland ice plateau. It was named by the Victoria University of Wellington Antarctic Expedition (VUWAE) (1958–59) for C. S. Wright, a member of the British Antarctic Expedition (1910–13), after whom the "Wright Glacier" was named.
Barwick Valley is an ice-free valley north of Apocalypse Peaks, extending from Webb Glacier to Victoria Valley in Victoria Land, Antarctica. A large part of the valley has been designated an Antarctic Specially Protected Area because of its pristine condition.
The Brown Hills are a group of mainly snow-free hills in the Cook Mountains of Antarctica.
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.
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.
Pearse Valley is an ice-free valley 3 nautical miles long, lying immediately west of Catspaw Glacier, at the south side of the Asgard Range in Victoria Land, Antarctica. It was named by the United States Advisory Committee on Antarctic Names (US-ACAN) for John S. Pearse, biologist at McMurdo Station, 1961, and the season 1961–62.
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.
The Horowitz Ridge is a rock ridge between David Valley and King Valley in the Asgard Range of Victoria Land, Antarctica.
Mount Odin is the most prominent peak, though not the highest, in the Asgard Range, of Victoria Land, Antarctica. It rises over 2,000 m (6,600 ft) just south of Lake Vanda. It was named by the Victoria University of Wellington Antarctic Expedition (VUWAE) (1958–59) for the Norse god Odin.
