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Smith Ridge ( 79°7′S86°32′W / 79.117°S 86.533°W ) is a ridge 4 nautical miles (7 km) long, lying 1 nautical mile (1.9 km) west of Frazier Ridge in the Founders Peaks, Heritage Range in Antarctica. Named by the University of Minnesota Geological Party to these mountains, 1963–64, for Carl W. Smith who served that season as helicopter engine technical representative with the 62nd Transportation Detachment.
Geographical features include:
Mount Terror is an extinct volcano about 3,230 metres (10,600 ft) high on Ross Island, Antarctica, about 20 nautical miles eastward of Mount Erebus. Mount Terror was named in 1841 by Sir James Clark Ross for his second ship, HMS Terror. The captain of Terror was Francis Crozier, a close friend of Ross for whom the nearby Cape Crozier is named.
The Neptune Range is a mountain range, 112 km (70 mi) long, lying WSW of Forrestal Range in the central part of the Pensacola Mountains in Antarctica. The range is composed of Washington Escarpment with its associated ridges, valleys and peaks, the Iroquois Plateau, and the Schmidt and Williams Hills. It was discovered and photographed on 13 January 1956 on a US Navy transcontinental plane flight from McMurdo Sound to Weddell Sea and return.
The Reedy Glacier is a major glacier in Antarctica, over 100 nautical miles long and 6 to 12 nautical miles wide, descending from the polar plateau to the Ross Ice Shelf between the Michigan Plateau and Wisconsin Range in the Transantarctic Mountains. It marks the limits of the Queen Maud Mountains on the west and the Horlick Mountains on the east.
The Amundsen Glacier is a major Antarctic glacier, about 7 to 11 km wide and 150 km (80 nmi) long. It originates on the Antarctic Plateau where it drains the area to the south and west of Nilsen Plateau, then descends through the Queen Maud Mountains to enter the Ross Ice Shelf just west of the MacDonald Nunataks.
The Prince Olav Mountains is a mountain group in the Queen Maud Mountains in Antarctica stretching from Shackleton Glacier to Liv Glacier at the head of the Ross Ice Shelf.
The Branscomb Glacier is an Antarctic glacier, 11 nautical miles long, flowing west from the north-west side of Vinson Massif into Nimitz Glacier, in the Sentinel Range of the Ellsworth Mountains. Its upper course receives ice influx from both Goodge Col and Jacobsen Valley, while the tributary Roché Glacier joins Branscomb Glacier just northwest of Príncipe de Asturias Peak.
The Scott Mountains are a large number of isolated peaks lying south of Amundsen Bay in Enderby Land of East Antarctica, Antarctica. Discovered on 13 January 1930 by the British Australian New Zealand Antarctic Research Expedition (BANZARE) under Sir Douglas Mawson. He named the feature Scott Range after Captain Robert Falcon Scott, Royal Navy. The term mountains is considered more appropriate because of the isolation of its individual features.
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.
The Hays Mountains are a large group of mountains and peaks of the Queen Maud Mountains of Antarctica, surmounting the divide between the lower portions of Amundsen Glacier and Scott Glacier and extending from the vicinity of Mount Thorne on the northwest to Mount Dietz on the southeast.
The Kyle Hills are a prominent group of volcanic cones, hills, ridges, and peaks that occupy the eastern part of Ross Island, Antarctica, between Mount Terror and Cape Crozier. The hills extend east–west for 8 nautical miles (15 km), rising from sea level at Cape Crozier to about 2,600 metres (8,500 ft) in Mount McIntosh at the western end of the group. Local relief of features is on the order of 200 metres (660 ft).
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.
On the continent of Antarctica, the Aramis Range is the third range south in the Prince Charles Mountains, situated 11 miles southeast of the Porthos Range and extending for about 30 miles in a southwest–northeast direction. It was first visited in January 1957 by Australian National Antarctic Research Expeditions (ANARE) southern party led by W.G. Bewsher, who named it for a character in Alexandre Dumas' novel The Three Musketeers, the most popular book read on the southern journey.
The Bender Mountains are a small group of mountains 4 nautical miles southwest of the Berry Peaks, between the southeast edge of the Ross Ice Shelf and the Watson Escarpment.
Nilsen Plateau is a rugged, ice-covered plateau in Antarctica. When including Fram Mesa, the plateau is about 30 nautical miles long and 1 to 12 nautical miles wide, rising to 3,940 metres (12,930 ft) high between the upper reaches of the Amundsen and Scott glaciers, in the Queen Maud Mountains. Discovered in November 1911 by the Norwegian expedition under Roald Amundsen, and named by him for Captain Thorvald Nilsen, commander of the ship Fram.
Gowan Glacier is a glacier about 15 nautical miles long in the Heritage Range of the Ellsworth Mountains of Antarctica, flowing north from the vicinity of Cunningham Peak in the Founders Escarpment to enter Minnesota Glacier just east of Welcome Nunatak. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1961–66, and was named by the Advisory Committee on Antarctic Names for Lieutenant Jimmy L. Gowan, U.S. Navy Medical Corps, officer in charge and doctor at Plateau Station in 1966.
Pipe Peak is a sharp peak on a ridge, 1,720 m, rising 1.5 nautical miles (2.8 km) north of Matney Peak in the Founders Peaks, Heritage Range. It was named so by members of the University of Minnesota Geological Party of 1963–64 because a pipe was left here after a visit to the area.
The Duncan Mountains are a group of rugged coastal foothills, about 18 nautical miles long, extending from the mouth of Liv Glacier to the mouth of Strom Glacier at the head of the Ross Ice Shelf in Antarctica.
The Medina Peaks are rugged, mainly ice-free, peaks surmounting a ridge 15 nautical miles long, extending north along the east side of Goodale Glacier to the edge of the Ross Ice Shelf, Antarctica.
The La Gorce Mountains are a group of mountains, 20 nautical miles long, standing between the tributary Robison Glacier and Klein Glacier at the east side of the upper reaches of the Scott Glacier, in the Queen Maud Mountains of Antarctica.
The Rawson Mountains lie within the Queen Maud Mountains to the southeast of the Ross Ice Shelf in Antarctica. They are a crescent-shaped range of tabular, ice-covered mountains including Fuller Dome, Mount Wyatt and Mount Verlautz, standing southeast of Nilsen Plateau and extending southeast for 18 nautical miles to the west side of Scott Glacier.
This article incorporates public domain material from "Smith Ridge". Geographic Names Information System . United States Geological Survey.
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