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The Sweeney Mountains are a group of mountains of moderate height and about 40 nautical miles extent, located 30 nautical miles north of the Hauberg Mountains in eastern Ellsworth Land, Antarctica.
Borchgrevink Glacier is a large glacier in the Victory Mountains, Victoria Land, Antarctica. It drains south between Malta Plateau and Daniell Peninsula, and thence projects into Glacier Strait, Ross Sea, as a floating glacier tongue.
Lambert Glacier is a major glacier in East Antarctica. At about 80 km (50 mi) wide, over 400 km (250 mi) long, and about 2,500 m (8,200 ft) deep, it is the world's largest glacier. It drains 8% of the Antarctic ice sheet to the east and south of the Prince Charles Mountains and flows northward to the Amery Ice Shelf. It flows in part of Lambert Graben and exits the continent at Prydz Bay.
Miers Valley is a valley just south of Marshall Valley and west of Koettlitz Glacier, on the coast of Victoria Land, Antarctica. The valley is ice-free except for Miers Glacier in its upper (western) part and Lake Miers near its center. It was mapped and named by Robert Falcon Scott's British Antarctic Expedition, 1910–13. The name is possibly after Edward J. Miers, a marine biologist from the British Museum who examined crustacea from the Erebus and Terror expeditions.
Sibelius Glacier is a glacier, 12 miles (19 km) long and 6 miles (10 km) wide, flowing south into the Mozart Ice Piedmont 10 miles (16 km) southwest of Mount Stephenson in the northern portion of Alexander Island, Antarctica. The glacier was first sighted from the air by the British Graham Land Expedition in 1937. Mapped from air photos taken by the Ronne Antarctic Research Expedition in 1947–48, by Searle of the Falkland Islands Dependencies Survey in 1960. This feature was named by the United Kingdom Antarctic Place-Names Committee for Jean Sibelius (1865-1957), Finnish composer.
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 Latady Mountains are a group of mountains rising west of Gardner Inlet and between Wetmore Glacier and Ketchum Glacier, in southeastern Palmer Land, Antarctica.
Arena Corner is an arcuate (curved) nunatak at the north end of the Traverse Mountains, 2 nautical miles (4 km) east of McHugo Peak, on the Rymill Coast, Palmer Land. It was named in 1977 by the UK Antarctic Place-Names Committee, the name being descriptive of the shape of this feature, which serves as a landmark in the area.
Brodie Peak is one of the Bristly Peaks, rising to 1,410 metres (4,630 ft) 5 nautical miles (9 km) south-southeast of Mount Castro, in the central Antarctic Peninsula. It was named by the Advisory Committee on Antarctic Names in 1977 after Earl E. Brodie, a United States Antarctic Research Program engineer in the Palmer Station winter party, 1969.
Wade Ice Rise is a small ice rise in Wordie Ice Shelf, 8 nautical miles (15 km) northwest of Triune Peaks, Fallières Coast. Photographed from the air by Ronne Antarctic Research Expedition (RARE), 1947–48, and surveyed by Falkland Islands Dependencies Survey (FIDS), 1958. Named in 1977 by Advisory Committee on Antarctic Names (US-ACAN) after George W. Wade, Jr., U.S. Navy, Chief Construction Electrician, Palmer Station, winter party 1970.
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.
Dobbratz Glacier is a broad tributary glacier which drains the south part of the White Escarpment and flows northeast between the Watlack Hills and the Webers Peaks into Splettstoesser Glacier, in the Heritage Range. It was named by the University of Minnesota Geological Party, 1963–64, for Major Joseph Dobbratz, a United States Marine Corps pilot who supported the party.
Gibraltar Peak is a peak in Antarctica.
Miller Ice Rise is an ice rise nearly 2 nautical miles (4 km) long and 1 nautical mile (2 km) wide at the ice front (1974) of the Wordie Ice Shelf, 16 nautical miles (30 km) west-northwest of the Triune Peaks, in southern Marguerite Bay, Antarctica. It was surveyed by the Falkland Islands Dependencies Survey in 1948–49, and was photographed from the air by the U.S. Navy in 1966. The feature was named, in 1977, by the Advisory Committee on Antarctic Names for Richard Miller, a U.S. Navy chief radioman at Palmer Station in the winter party of 1968.
Mount Martine is a massive mountain, about 800 metres (2,600 ft) high, with a prominent rocky north face and ice-covered south slopes, overlooking the north shore of Charcot Island, south of Cheesman Island, in the east Bellinghausen Sea of Antarctica.
The Hull Glacier is a glacier, about 35 nautical miles long, flowing northwest between Mount Giles and Mount Gray into Hull Bay, in Marie Byrd Land, Antarctica.
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.
Stellar Crests is a four prominent snow-covered peaks, rising to about 2,000 m, surmounting LeMay Range west of the north part of Planet Heights in central Alexander Island, Antarctica. The peaks were first mapped from air photos taken by the Ronne Antarctic Research Expedition in 1947–48, by Searle of the Falkland Islands Dependencies Survey in 1960. Named by the United Kingdom Antarctic Place-Names Committee for their proximity to features named for planets and their satellites.
Relay Hills is a group of low, ice-covered hills, mainly conical in shape, between Mount Edgell and Kinnear Mountains in western Antarctic Peninsula. First roughly surveyed from the ground by British Graham Land Expedition (BGLE), 1936–37. Photographed from the air by Ronne Antarctic Research Expedition (RARE), November 1947. Resurveyed by Falkland Islands Dependencies Survey (FIDS), November 1958. The name, applied by the United Kingdom Antarctic Place-Names Committee (UK-APC), arose because both the BGLE and the FIDS sledging parties had to relay their loads through this area to the head of Prospect Glacier.
References
- ↑ "McHugo Peak". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2013-09-06.
This article incorporates public domain material from "McHugo Peak". Geographic Names Information System . United States Geological Survey.
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