Dominion Range
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Dominion Range
The Dominion Range () is a broad mountain range, about long, forming a prominent salient at the juncture of the Beardmore and Mill glaciers in Antarctica. The range is part of the Queen Maud Mountains The range was discovered by the British Antarctic Expedition (1907–09) and named by Shackleton for the Dominion of New Zealand, which generously aided the expedition. The highest peak is Mount Mills at . Key geological features Mount Mills Mount Mills () is the highest mountain in the range at , forming part of the northern escarpment overlooking the Beardmore Glacier 13 km north of Mount Saunders. The mountain was discovered by the British Antarctic Expedition (1907–09) under Shackleton, and named for Sir James Mills who, with the government of New Zealand, paid the cost of towing the expedition ship ''Nimrod'' to Antarctica in 1908. Mount Nimrod Mount Nimrod () is a mountain at , standing 6 km SSE of Mount Saunders. It was discovered by the British Anta ...
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Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ...
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Vandament Glacier
Vandament Glacier () is an east-flowing glacier, 6 nautical miles (11 km) long, draining the east-central portion of the Dominion Range icecap. The glacier lies close south of Koski Glacier, whose flow it parallels, and terminates 2 nautical miles (3.7 km) northwest of Safety Spur. It was named by the Advisory Committee on Antarctic Names (US-ACAN) for Charles H. Vandament, the United States Antarctic Research Program (USARP) ionospheric physicist at South Pole Station South is one of the cardinal directions or compass points. The direction is the opposite of north and is perpendicular to both east and west. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Proto-Germanic ''*sunþaz ..., 1962. Charles H. Vandament (08/02/1935- 10/10/2005), known to family and friends as "Smilin' Chuck", was an engineer and scientist specializing in radio and antenna design. An Electrical Engineering graduate of the University of Arkansas, Mr. Vandament ...
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Scott Icefalls
Mill Glacier is a tributary glacier, wide, flowing northwest between the Dominion Range and the Supporters Range into Beardmore Glacier, Antarctica. It was discovered by the British Antarctic Expedition, 1907–09, and named for Hugh Robert Mill, a British geographer and Antarctic historian. See also * List of glaciers in the Antarctic There are many glaciers in the Antarctic. This set of lists does not include ice sheets, ice caps or ice fields, such as the Antarctic ice sheet, but includes glacial features that are defined by their flow, rather than general bodies of ice. Th ... References Glaciers of Dufek Coast {{DufekCoast-glacier-stub ...
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Rutkowski Glacier
Rutkowski Glacier () is a glacier which drains the northern part of the Dominion Range icecap eastward of Mount Mills. It descends northeastward into Meyer Desert where it terminates without reaching Beardmore Glacier. Named by Advisory Committee on Antarctic Names (US-ACAN) for Richard L. Rutkowski, United States Antarctic Research Program (USARP) meteorologist at the South Pole Station South is one of the cardinal directions or compass points. The direction is the opposite of north and is perpendicular to both east and west. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Proto-Germanic ''*sunþaz ..., 1962. Glaciers of Dufek Coast {{DufekCoast-glacier-stub ...
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Plunket Point
Plunket Point () is a conspicuous rock point marking the northern end of the Dominion Range and the confluence of the Beardmore and Mill Glaciers. Discovered by the British Antarctic Expedition (1907–09) and named for Lord Plunket, at that time Governor of New Zealand New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island count .... Headlands of the Ross Dependency Dufek Coast {{DufekCoast-geo-stub ...
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Mount Mills (Antarctica)
Mount Mills is a mountain, high, forming part of the north escarpment of the Dominion Range in Antarctica, overlooking Beardmore Glacier north of Mount Saunders. It was discovered by the British Antarctic Expedition (1907–09) and named for Sir James Mills who, with the government of New Zealand, paid the cost of towing the expedition ship ''Nimrod Nimrod (; ; arc, ܢܡܪܘܕ; ar, نُمْرُود, Numrūd) is a biblical figure mentioned in the Book of Genesis and Books of Chronicles. The son of Cush and therefore a great-grandson of Noah, Nimrod was described as a king in the land of ...'' to Antarctica in 1908. References Mountains of the Ross Dependency Dufek Coast {{DufekCoast-geo-stub ...
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Mount Cecily
Mount Cecily () is a prominent peak, high, standing northwest of Mount Raymond, in the Grosvenor Mountains. It was discovered by the British Antarctic Expedition, 1907–09, and named for Shackleton's daughter. The position agrees with that shown on Shackleton's map but the peak does not lie in the Dominion Range as he thought, being separated from that range by the Mill Glacier Mill Glacier is a tributary glacier, wide, flowing northwest between the Dominion Range and the Supporters Range into Beardmore Glacier, Antarctica. It was discovered by the British Antarctic Expedition, 1907–09, and named for Hugh Robert Mill .... References Mountains of the Ross Dependency Dufek Coast {{DufekCoast-geo-stub ...
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Meyer Desert
The Meyer Desert is a triangular ice-free area of about at the northern end of the Dominion Range, Antarctica, near the confluence of Beardmore Glacier and Mill Glacier. It was named by the New Zealand Geological Survey Antarctic Expedition of 1961–62 for George Meyer of the United States Antarctic Research Program, who was scientific leader at McMurdo Station in 1961, and led a field party into this area in the summer of 1961–62. A paper from 2003 reports the discovery of the first freshwater mollusc remains from Antarctica in the Meyer Desert Formation. These include both an unidentified fragmentary lymnaeid (a freshwater snail), and an unidentified true ''Pisidium'' (a freshwater bivalve Freshwater bivalves are one kind of freshwater mollusc, along with freshwater snails. They are bivalves that live in fresh water as opposed to salt water, which is the main habitat type for bivalves. The majority of species of bivalve molluscs l ...). References Landforms of the ...
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Koski Glacier
Mill Glacier is a tributary glacier, wide, flowing northwest between the Dominion Range and the Supporters Range into Beardmore Glacier, Antarctica. It was discovered by the British Antarctic Expedition, 1907–09, and named for Hugh Robert Mill, a British geographer and Antarctic historian. See also * List of glaciers in the Antarctic There are many glaciers in the Antarctic. This set of lists does not include ice sheets, ice caps or ice fields, such as the Antarctic ice sheet, but includes glacial features that are defined by their flow, rather than general bodies of ice. Th ... References Glaciers of Dufek Coast {{DufekCoast-glacier-stub ...
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Kane Rocks
The Kane Rocks () form an east–west trending ridge, long, forming a rock median between the upper reaches of Koski Glacier and Vandament Glacier in the Dominion Range, Antarctica. The ridge was named by the Advisory Committee on Antarctic Names for Henry Scott Kane, a United States Antarctic Research Program cosmic rays scientist at South Pole Station, winter 1964, and a member of the South Pole—Queen Maud Land Traverse South is one of the cardinal directions or compass points. The direction is the opposite of north and is perpendicular to both east and west. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Proto-Germanic ''*sunþaz' ... I and II, 1964–65 and 1965–66. References Ridges of the Ross Dependency Dufek Coast {{DufekCoast-geo-stub ...
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Davis Nunataks
The Davis Nunataks () are a small cluster of rock nunataks northwest of Mount Ward, the feature being a southern outlier of the main body of the Dominion Range. The group was named by the Advisory Committee on Antarctic Names for Ronald N. Davis, a United States Antarctic Research Program geomagnetist-seismologist at South Pole Station South is one of the cardinal directions or compass points. The direction is the opposite of north and is perpendicular to both east and west. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Proto-Germanic ''*sunþaz ..., winter 1963. References Nunataks of the Ross Dependency Dufek Coast {{DufekCoast-geo-stub ...
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Browns Butte
Browns Butte () is a bare rock butte at the north side of the mouth of Koski Glacier in the Dominion Range. It was named (without apostrophe) by the Advisory Committee on Antarctic Names for Craig W. Brown, United States Antarctic Research Program meteorologist at South Pole Station South is one of the cardinal directions or compass points. The direction is the opposite of north and is perpendicular to both east and west. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Proto-Germanic ''*sunþaz ..., 1963. References * Buttes of Antarctica Landforms of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ...
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