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The Deep Freeze Range is a rugged mountain range, over 128 km (80 mi) long and about 16 km (10 mi) wide, rising between Priestley and Campbell Glaciers in Victoria Land, Antarctica, and extending from the edge of the polar plateau to Terra Nova Bay. Peaks in the low and mid portions of the range were observed by early British expeditions to the Ross Sea.
The Scaife Mountains is a group of mountains rising west of Prehn Peninsula and between the Ketchum and Ueda glaciers, in Palmer Land, at the base of Antarctic Peninsula.
The Prince Charles Mountains are a major group of mountains in Mac. Robertson Land in Antarctica, including the Athos Range, the Porthos Range, and the Aramis Range. The highest peak is Mount Menzies, with a height of 3,228 m (10,591 ft). Other prominent peaks are Mount Izabelle and Mount Stinear. These mountains, together with other scattered peaks, form an arc about 420 km (260 mi) long, extending from the vicinity of Mount Starlight in the north to Goodspeed Nunataks in the south.
The Trojan Range is a mountain range rising to 2,760 metres (9,055 ft), extending northward from Mount Francais along the east side of Iliad Glacier, Anvers Island, in the Palmer Archipelago of the British Antarctic Territory. It was surveyed by the Falkland Islands Dependencies Survey (FIDS) in 1955 and named by the UK Antarctic Place-Names Committee (UK-APC) for the Trojans, one of the opposing sides in the Trojan War in Homer's Iliad.
Cape Longing is a rocky cape on the east coast of Graham Land, Antarctica, forming the south end of a large ice-covered promontory which marks the west side of the south entrance to Prince Gustav Channel. It was discovered by the Swedish Antarctic Expedition under Otto Nordenskiöld in 1902, and so named by him because from the position of his winter hut on Snow Hill Island the cape lay in the direction of his "land of longing" which he was anxious to explore.
Athos Range is the northernmost range in the Prince Charles Mountains of Mac. Robertson Land, Antarctica. The range consists of many individual mountains and nunataks that trend east–west for 40 miles (64 km) along the north side of Scylla Glacier.
Wilson Hills is a group of scattered hills, nunataks and ridges that extend NW-SE for about 110 kilometres (68 mi) between Matusevich Glacier and Pryor Glacier in Antarctica. They were discovered by Lieutenant Harry Pennell, Royal Navy, on the Terra Nova Expedition in February 1911 during Robert Falcon Scott's last expedition, and named after Edward Adrian Wilson, a zoologist with the expedition, who perished with Scott on the return journey from the South Pole.
Zephyr Glacier 1 is a glacier, about 8 miles (13 km) long, flowing westward from the southwest side of Mount Edgell into George VI Sound to the south of Cape Jeremy. The feature was surveyed by Falkland Islands Dependencies Survey (FIDS), 1948, and British Antarctic Survey (BAS), 1971–72; photographed from the air by U.S. Navy, 1966. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) in 1977 after Zephyrus, the west wind. One of the several features in this area is named after winds.
Explorers Range is a large mountain range in the Bowers Mountains of Victoria Land, Antarctica, extending from Mount Bruce in the north to Carryer Glacier and McLin Glacier in the south. Named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for the northern party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1963–64, whose members carried out a topographical and geological survey of the area. The names of several party members are assigned to features in and about this range. All of the geographical features listed below lie situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Lawrie Glacier is a glacier flowing between Mount Genecand and Mezzo Buttress, and entering the head of Barilari Bay between Cherkovna Point and Prestoy Point on the west coast of Graham Land, Antarctica. It was charted by the British Graham Land Expedition under Rymill, 1934–37, and was named by the UK Antarctic Place-Names Committee in 1959 for Robert Lawrie, an English alpine and polar equipment specialist.
The Porthos Range is the second range south in the Prince Charles Mountains of Antarctica, extending for about 30 miles in an east-to-west direction between Scylla Glacier and Charybdis Glacier. First visited in December 1956 by the Australian National Antarctic Research Expeditions (ANARE) southern party under W.G. Bewsher (1956-57) and named after Porthos, a character in Alexandre Dumas, père's novel The Three Musketeers, the most popular book read on the southern journey.
The McCuddin Mountains are a small cluster of mountains in Antarctica consisting mainly of two large mountains, Mount Flint and Mount Petras, along with several scattered peaks and nunataks. Located in Marie Byrd Land, 64 km (40 mi) east of the Ames Range, with Wallace Rock as its southeast extremity.
The Anare Nunataks are a group of mainly snow-covered ridges with exposed rock summits rising to 2,035 metres (6,680 ft), standing 16 nautical miles (30 km) south of the Stinear Nunataks in Mac. Robertson Land. First visited in November 1955 by an Australian National Antarctic Research Expeditions (ANARE) party led by John Béchervaise, the name is taken from the acronym of the expedition.
Bagshawe Glacier is a glacier which drains the northeast slopes of Mount Theodore and discharges into Lester Cove, Andvord Bay west of Mount Tsotsorkov, on the west coast of Graham Land, Antarctica.
Depot Peak is a solitary nunatak, with a single needle-shaped peak, lying about 37 nautical miles (70 km) north of the Stinear Nunataks in Mac. Robertson Land. It was discovered by an Australian National Antarctic Research Expeditions party led by R.G. Dovers during a southern journey in December 1954, and so named because a depot was established in the vicinity.
Tumble Glacier is a glacier extending along the east side of Alexander Island, Antarctica, 7 nautical miles (13 km) long and 3 nautical miles (6 km) wide, which flows east from the cliffs of Mount Egbert, Mount Ethelwulf and Mount Ethelred of the Douglas Range into the west side of the George VI Ice Shelf that occupies George VI Sound immediately south of Mount King. The glacier was first roughly surveyed in 1936 by the British Graham Land Expedition under Rymill. Resurveyed in 1948 by the Falkland Islands Dependencies Survey, and so named by them because of the extremely broken condition of the lower reaches of the glacier.
The Gowlett Peaks are a small group of isolated peaks, consisting of tall, sharp twin peaks and two close outliers, about 8 nautical miles (15 km) northeast of the Anare Nunataks in Mac. Robertson Land, Antarctica. They were sighted in November 1955 by an Australian National Antarctic Research Expeditions party led by John Béchervaise, and were named by the Antarctic Names Committee of Australia for Alan Gowlett, an engineer at Mawson Station in 1955.
Mount Egbert is a mainly ice-covered mountain, 2,895 metres (9,500 ft) high, 8 nautical miles (15 km) south-southeast of Mount Stephenson in the Douglas Range of Alexander Island, Antarctica. It was possibly first seen in 1909 by the French Antarctic Expedition under Jean-Baptiste Charcot, but was not recognized as a part of Alexander Island. It was surveyed in 1936 by the British Graham Land Expedition under John Rymill, then resurveyed in 1948 by the Falkland Islands Dependencies Survey, who named the mountain for Egbert, a ninth-century Saxon king of England. Mount Egbert is the second highest peak of Alexander Island, while Mount Stephenson remains the highest point.
Macklin Island is a small island in the eastern part of the Robinson Group, about 3 kilometres (1.5 nmi) north of Kirton Island, and 6 kilometres (3 nmi) northwest of Cape Daly, Mac. Robertson Land, Antarctica. It was mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition, 1936–37, and was named by the Antarctic Names Committee of Australia for E.L. Macklin, a radio officer at Mawson Station in 1955 and 1959.
Kaminuma Bluff is a bold ice-covered bluff that rises to over 200 metres (660 ft) near the shore in southeastern Ross Island, off the coast of Antarctica. The bluff is midway between Cape MacKay and Cape Crozier. At the suggestion of P.R. Kyle, it was named by the Advisory Committee on Antarctic Names (2000) after Katsutada Kaminuma of the National Institute of Polar Research (Japan), who was a founding member of the International Mount Erebus Seismic Study, 1980–81 through 1986. This was a joint project with the United States, Japan, and New Zealand. Kaminuma was the lead Japanese member and continued to work in Antarctica and on Mount Erebus for many years.
References
- ↑ "Mount Macklin". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2013-07-18.
This article incorporates public domain material from "Mount Macklin". Geographic Names Information System . United States Geological Survey.
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