Holdsworth was a bicycle manufacturer in London, England.
Holdsworth may also refer to:
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A crevasse is a deep crack, or fracture, found in an ice sheet or glacier, as opposed to a crevice that forms in rock. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement. The resulting intensity of the shear stress causes a breakage along the faces.
The Pensacola Mountains are a large group of mountain ranges of the Transantarctic Mountains System, located in the Queen Elizabeth Land region of Antarctica.
The Victory Mountains is a major group of mountains in Victoria Land, Antarctica, about 160 kilometres (99 mi) long and 80 km (50 mi) wide, which is bounded primarily by Mariner and Tucker glaciers and the Ross Sea. The division between these mountains and the Concord Mountains is less precise but apparently lies in the vicinity of Thomson Peak.
Aviator Glacier is major valley glacier in Antarctica that is over 60 miles (97 km) long and 5 miles (8.0 km) wide, descending generally southward from the plateau of Victoria Land along the west side of Mountaineer Range, and entering Lady Newnes Bay between Cape Sibbald and Hayes Head where it forms the Aviator Glacier Tongue.
Denman Glacier is a glacier 7 to 10 nautical miles wide, descending north some 70 nautical miles, which debouches into the Shackleton Ice Shelf east of David Island, Queen Mary Land. It was discovered in November 1912 by the Western Base party of the Australasian Antarctic Expedition under Sir Douglas Mawson. Mawson named the glacier for Lord Denman, Governor-General of Australia in 1911, a patron of the expedition.
Thwaites Glacier, sometimes referred to as the Doomsday Glacier, is an unusually broad and vast Antarctic glacier flowing into the Pine Island Bay, part of the Amundsen Sea, east of Mount Murphy, on the Walgreen Coast of Marie Byrd Land. Its surface speeds exceed 2 kilometres per year near its grounding line. Its fastest flowing grounded ice is centred between 50 and 100 kilometres east of Mount Murphy. It was named by the Advisory Committee on Antarctic Names in 1967 after Fredrik T. Thwaites (1883–1961), a glacial geologist, geomorphologist and professor emeritus at the University of Wisconsin–Madison. The historian Reuben Gold Thwaites was his father.
Boyana Glacier in Levski Ridge, Tangra Mountains on Livingston Island, South Shetland Islands in Antarctica is situated southeast of Macy Glacier and west-southwest of Srebarna Glacier. It is bounded by Vazov Rock on the west, St. Naum Peak, Starosel Gate, Silistra Knoll and Kotel Gap on the north, and Christoff Cliff on the east. The glacier extends 3 km in east-west direction and 1.6 km in north-south direction, and flows southeastward into the Bransfield Strait between Vazov Point and Aytos Point.
Kaliakra Glacier is a glacier in northeastern Livingston Island, Antarctica extending 3.8 nautical miles in east-west direction and 4.3 nautical miles in north-south direction, and situated southeast of Saedinenie Snowfield, southwest of Panega Glacier, north of Struma Glacier and upper Huron Glacier, and northeast of Perunika Glacier. It is bounded by Melnik Ridge and Bowles Ridge to the south, by Hemus Peak, Gurev Gap, Gleaner Heights, Elhovo Gap, Leslie Hill, Leslie Gap and Radnevo Peak to the west, and Miziya Peak and Samuel Peak to the north. The glacier drains eastwards into Moon Bay south of Perperek Knoll and north of Sindel Point.
Murgash Glacier is the 3.4 km long and 3.2 km wide glacier on Greenwich Island in the South Shetland Islands, Antarctica situated southeast of Yakoruda Glacier, south of Teteven Glacier, southwest of Traub Glacier and west-northwest of Bravo Glacier. It is bounded by Lloyd Hill on the northwest, Tile Ridge on the east and Hebrizelm Hill on the southeast, and drains southwards into Kramolin Cove in McFarlane Strait between Yovkov Point and Kaspichan Point.
Berkovitsa Glacier is a glacier on Livingston Island, Antarctica situated east of Etar Snowfield, south of Medven Glacier, west-northwest of Tundzha Glacier and north-northeast of Verila Glacier. It is bounded by the southeastern slopes of Oryahovo Heights and the northwestern slopes of Snow Peak. It extends 4 km in southeast-northwest direction and 2.8 km in northwest-southeast direction, and drains northeastwards into Hero Bay between Avitohol Point and Remetalk Point.
Dan Holdsworth is a British photographer who creates large-scale photographs and digital art characterized by the use of traditional techniques and unusually long exposure times, and by radical abstractions of geography. He has exhibited internationally including solo shows at BALTIC Centre for Contemporary Art, Gateshead, and Barbican Art Gallery, London; and group shows at Tate Britain, London, and Centre Pompidou, Paris. His work is held in collections including the Tate Collection, Saatchi Collection, and the Victoria and Albert Museum, London. He lives and works in Newcastle upon Tyne and London.
The Erebus Ice Tongue is a mountain outlet glacier and the seaward extension of Erebus Glacier from Ross Island. It projects 11 kilometres (6.8 mi) into McMurdo Sound from the Ross Island coastline near Cape Evans, Antarctica. The glacier tongue varies in thickness from 50 metres (160 ft) at the snout to 300 metres (980 ft) at the point where it is grounded on the shoreline. Explorers from Robert F. Scott's Discovery Expedition (1901–1904) named and charted the ice tongue.
Shipley Glacier is a glacier, 25 miles (40 km) long, in the north-central Admiralty Mountains of Antarctica. The glacier drains the northern slopes of Mount Adam and flows along the east wall of DuBridge Range to Pressure Bay on the north coast of Victoria Land. Some of the glacier bypasses Pressure Bay and reaches the sea west of Flat Island. The seaward end of the glacier was first mapped by the Northern Party, led by Victor Campbell, of the British Antarctic Expedition, 1910–13. Named by Campbell for Sir Arthur Shipley, master of Christ's College, Cambridge, England, at the suggestion of Priestley. The entire glacier was mapped by United States Geological Survey (USGS), 1960–63.
Pastra Glacier is a 4.8 km long and 2 km wide glacier in the central part of Trinity Island in the Palmer Archipelago, Antarctica. Draining northwards to flow into Milburn Bay.
Kranz Peak is a peak 2,680 metres (8,800 ft) high, standing 6 nautical miles (11 km) northwest of Mount Przywitowski, between the heads of Holdsworth Glacier and Bartlett Glacier, in the Queen Maud Mountains of Antarctica. It was named by the Advisory Committee on Antarctic Names for Commander Arthur C. Kranz, staff meteorological officer, U.S. Naval Support Force, Antarctica, during U.S. Navy Operation Deep Freeze 1966 and 1967.
The Monteath Hills are a group of mountains in the Victory Mountains of Victoria Land, Antarctica, bounded by Jutland Glacier, Midway Glacier, Pearl Harbor Glacier, and Plata Glacier. The group includes Mount Crowder, Mount Tararua, and Mount Holdsworth. The hills were named by the New Zealand Antarctic Place-Names Committee in 1983, after Colin Monteath, a field operations officer with the Antarctic Division of the New Zealand Department of Scientific and Industrial Research.
McNally Peak is a peak 2,570 metres (8,430 ft) high, standing 3.5 nautical miles (6 km) west of Mount Farley, near the southeast side of Holdsworth Glacier, in the Queen Maud Mountains of Antarctica. It was named by the Advisory Committee on Antarctic Names for Commander Joseph J. McNally, U.S. Navy, supply officer at McMurdo Station, winter 1959, and on the staff of the Commander, U.S. Naval Support Force, Antarctica, during U.S. Navy Operation Deep Freeze 1967.
Holdsworth Glacier is a tributary glacier about 8 nautical miles (15 km) long, flowing northeast from Fuller Dome to enter the southeast side of Bartlett Glacier, in the Queen Maud Mountains of Antarctica. It was named by the Advisory Committee on Antarctic Names for Gerald Holdsworth, who was involved in geological studies at McMurdo Station in the summer of 1965–66.
Tongue Peak is a peak rising to about 2,450 m between Holdsworth Glacier and Scott Glacier, 3 nautical miles (6 km) west-northwest of Mount Farley, in the Queen Maud Mountains, Antarctica. The peak was mapped by United States Geological Survey (USGS) from surveys and U.S. Navy aerial photographs, 1960–64. It was geologically mapped by a United States Antarctic Research Program (USARP)-Arizona State University field party, 1978–79, and was named by geologist Scott G. Borg, a member of the party. The name derives from a well-developed tongue-shaped moraine in an abandoned cirque between the west and north ridges of the peak.
Bender Glacier is a glacier that flows from Mount Atkinson and Mount Craddock southwards between Chaplin Peak and Krusha Peak, and joins Nimitz Glacier just south of Gilbert Spur in the southern Sentinel Range, Ellsworth Mountains in Antarctica. Receiving ice influx from its left tributaries Severinghaus Glacier, Brook Glacier and Bolgrad Glacier.