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The Sentinel Range is a major mountain range situated northward of Minnesota Glacier and forming the northern half of the Ellsworth Mountains in Antarctica. The range trends NNW-SSE for about 185 km (115 mi) and is 24 to 48 km wide. Many peaks rise over 4,000 m (13,100 ft) and Vinson Massif (4892 m) in the southern part of the range is the highest elevation on the continent.
Terra Nova Bay is a bay which is often ice free, about 40 nautical miles long, lying between Cape Washington and the Drygalski Ice Tongue along the coast of Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition under Robert Falcon Scott, 1901–1904, and named by him after Terra Nova, one of the relief ships for the expedition.
Mount Discovery is a conspicuous, isolated volcanic cone, 2,680 metres (8,790 ft) high, lying at the head of McMurdo Sound and east of Koettlitz Glacier, overlooking the northwest portion of the Ross Ice Shelf. It forms the center of a three-armed mass of which Brown Peninsula is one extension to the north; Minna Bluff is a second to the east; the third is Mount Morning to the west. Mount Discovery was discovered by the British National Antarctic Expedition (1901–04) and named for their expedition ship Discovery.
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.
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.
Shambles Glacier is a steep glacier 4 miles (6 km) long and 6 miles (10 km) wide, with very prominent hummocks and crevasses, flowing east between Mount Bouvier and Mount Mangin into Stonehouse Bay on the east side of Adelaide Island. It is the island's largest glacier, and provides an eastern outlet from the giant Fuchs Ice Piedmont which covers the entire western two-thirds of the island. In doing so, Shambles Glacier provides the largest 'gap' in Adelaide Island's north–south running mountain chain.
The Airy Glacier is a glacier 20 nautical miles (37 km) long and 6 nautical miles (11 km) wide, flowing west to the northeast portion of Forster Ice Piedmont, near the west coast of the Antarctic Peninsula.
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.
Il Polo Glacier is a small glacier draining northward between Polar Times Glacier and Polarforschung Glacier into the Publications Ice Shelf, Antarctica. It was delineated in 1952 by John H. Roscoe from air photos taken by the U.S. Navy during Operation Highjump, 1946–47. Roscoe named it after Il Polo, a polar journal published by the Istituto Geografico in Forlì, Italy.
Haas Glacier is a steep tributary glacier draining northward from Rawson Plateau to enter the south side of Bowman Glacier, in the Queen Maud Mountains of Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for Charles G. Haas, a meteorologist in the South Pole Station winter party, 1960.
Prospect Glacier is a glacier between Kinnear Mountains and Mayer Hills, flowing north into Forster Ice Piedmont on the west coast of Antarctic Peninsula. It was first roughly surveyed in 1936 by the British Graham Land Expedition (BGLE) under Rymill. In 1954 the United Kingdom Antarctic Place-Names Committee (UK-APC) gave the name Prospect Pass to a col between Eureka Glacier and the glacier here described. During resurvey of the area by the Falkland Islands Dependencies Survey (FIDS) in 1958, the col was found to be an indeterminate feature, while this glacier is well marked and requires a name.
Gilbert Glacier is a glacier about 20 nautical miles (37 km) long flowing south from Nichols Snowfield into Mozart Ice Piedmont, situated in northern Alexander Island, 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. It is south of the Clare Range and north of the Asgard Range.
Hamblin Glacier is a glacier flowing to the southeast side of Widmark Ice Piedmont, in Graham Land, Antarctica. It was photographed by Hunting Aerosurveys Ltd in 1955–57, and mapped from these photos by the Falkland Islands Dependencies Survey. It was named by the UK Antarctic Place-Names Committee in 1959 for Theodore Hamblin (1873–1952), an English optician who in the 1930s helped in the evolution of the first satisfactory snow goggle design.
Lucchitta Glacier is a glacier about 20 nautical miles (37 km) long flowing south from the Hudson Mountains of Antarctica into Pine Island Bay. It was named by the Advisory Committee on Antarctic Names after geologist Baerbel K. Lucchitta of the United States Geological Survey, Flagstaff, Arizona, a specialist in the use of satellite imagery for geological and glaciological studies from the early 1980s to the early 2000s (decade), and one of the pioneers in the use of imagery for glacier velocity measurements in Antarctica.
Hudman Glacier is a glacier draining south of Mount Landolt between Marze Peak and Miller Peak in Petvar Heights at the south end of the Sentinel Range, in the Ellsworth Mountains of Antarctica, flowing south-southeast to Minnesota Glacier. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1957–59, and was named by the Advisory Committee on Antarctic Names for Captain Rayburn A. Hudman, United States Marine Corps, who died in the crash of a Lockheed P2V-2n Neptune, modified for extreme range, flying in sub zero temperatures and Ski equipped for landing on the Ice runways at McMurdo Sound Antarctica on October 18, 1956.
Maumee Ice Piedmont is an ice piedmont at the terminus of Kohler Glacier, east of the Jenkins Heights, on the Walgreen Coast of Marie Byrd Land, Antarctica. It was mapped by the United States Geological Survey from U.S. Navy aerial photographs taken 1965–67, and was named by the Advisory Committee on Antarctic Names after the USNS Maumee, a supply tanker that serviced McMurdo Station from 1970 to 1985. Upon construction of fuel storage tanks at McMurdo Station, completed in 1970, the Maumee replaced smaller tankers used earlier, delivering in one voyage a year's supply of petroleum fuels.
Blue Glacier is a large glacier which flows into Bowers Piedmont Glacier about 10 nautical miles south of New Harbour, in Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition (BrNAE) under Robert Falcon Scott, 1901–04, who gave it this name because of its clear blue ice at the time of discovery.
New Harbour is a bay about 10 nautical miles wide between Cape Bernacchi and Butter Point along the coast of Victoria Land, due west of Ross Island.
Silverfish Bay is a roughly triangular body of water that lies within Terra Nova Bay along the Scott Coast of Victoria Land. Its outline may be defined by a line that connects the tip of the Campbell Glacier Tongue, Shield Nunatak, Oscar Point, and then returns to the Campbell Glacier Tongue. It was named by the New Zealand Geographic Board in 2006 because of an abundance of Antarctic silverfish eggs in the bay.
References
This article incorporates public domain material from "Vacchi Piedmont Glacier". Geographic Names Information System . United States Geological Survey.
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