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Mount Mackellar
Mount Mackellar () is a massive mountain, high, standing at the head of Mackellar Glacier, south of Pagoda Peak in the Queen Alexandra Range, Antarctica. Discovery and name Mount Mackellar was discovered by the British Antarctic Expedition, 1907–09, and named after Campbell Mackellar, a supporter of the expedition. Location Mount Mackellar rises above the north of Grindley Plateau in the central Queen Alexandra Range. Mount Elizabeth is to the east. Mount Mackellar is at the head of Mackellar Glacier to the northwest. A line of peaks extends to the northwest along the west side of Tillite Glacier, ending in Fairchild Peak and Portal Rock. A ridge connects the mountain to Pagoda Peak to the north, from which Hampton Ridge extends between Montgomerie Glacier and Mackellar Glacier to Peneplain Peak. Features Nearby features include: Fairchild Peak . A conspicuous rock peak, high, standing south-southeast of Portal Rock, at the south side of the mouth of Tillite Glaci ...
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Mackellar Glacier
Lennox-King Glacier is a large valley glacier, about long, draining Bowden Névé and flowing northeast between the Holland Range and the Queen Alexandra Range of Antarctica to enter Richards Inlet, Ross Ice Shelf. It was named by the New Zealand Geological Survey Antarctic Expedition (1959–60) for Lieutenant Commander James Lennox-King, Royal New Zealand Navy, leader at Scott Base Scott Base is a New Zealand Antarctic research station at Pram Point on Ross Island near Mount Erebus in New Zealand's Ross Dependency territorial claim. It was named in honour of Captain Robert Falcon Scott, RN, leader of two British expedit ..., 1960. See also * Vertigo Bluff References Glaciers of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ...
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Queen Alexandra Range
The Queen Alexandra Range is a major mountain range of the Transantarctic Mountains System, located in the Ross Dependency region of Antarctica. It is about long, bordering the entire western side of Beardmore Glacier from the Polar Plateau to the Ross Ice Shelf. Alternate names for this range include Alexandra Mountains, Alexandra Range and Königin Alexandra Gebirge. The highest peak of the range is Mount Kirkpatrick at . Other peaks in the range include Mount Dickerson (4,120 m). Discovery This mountain range was discovered on the journey toward the South Pole by the British Antarctic Expedition, and was named by Ernest Shackleton for Queen consort Alexandra of the United Kingdom. Shackleton and his men, and a later expedition headed by Robert Falcon Scott, both collected rock samples from the range that contained fossils. The discovery that multicellular life forms had lived so close to the South Pole was an additional piece of evidence that accompanied the publica ...
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British Antarctic Expedition, 1907–09
The ''Nimrod'' Expedition of 1907–1909, otherwise known as the British Antarctic Expedition, was the first of three successful expeditions to the Antarctic led by Ernest Shackleton and his second expedition to the Antarctic. Its main target, among a range of geographical and scientific objectives, was to be first to the South Pole. This was not attained, but the expedition's southern march reached a Farthest South latitude of 88° 23' S, just from the pole. This was by far the longest southern polar journey to that date and a record convergence on either Pole. A separate group led by Welsh Australian geology professor Edgeworth David reached the estimated location of the South Magnetic Pole, and the expedition also achieved the first ascent of Mount Erebus, Antarctica's second highest volcano. The expedition lacked governmental or institutional support, and relied on private loans and individual contributions. It was beset by financial problems and its preparations ...
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Grindley Plateau
Grindley Plateau () is a high icecapped plateau in the central Queen Alexandra Range of Antarctica, bordered by the peaks of Mount Mackellar, Mount Bell and Mount Kirkpatrick. Name Grindley Plateau was named by the Northern Party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE; 1961–62) for George Grindley, senior geologist of the party. Location Grindley Plateau is in the central Queen Alexandra Range, north of Mount Kirkpatrick. The Garrard Glacier forms to its south and flows east into the Beardmore Glacier. The Wyckoff Glacier forms to its southeast and flows west to Lennox-King Glacier. The Wahl Glacier forms to its west and flows northwest to Lennox-King Glacier. Features surrounding the plateau include Mallory Bluff, Mount Mackellar, Mount Bell, Mount Kurlak, Mount Lockwood, Mount Stanley and Levi Peak. Features Mallory Bluff . A prominent bluff on the northwest slope of Grindley Plateau, just northeast of the head of Wahl Glacier. Named by the ...
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Mount Elizabeth (Antarctica)
Mount Elizabeth is a massive ice-free mountain, high, standing south of Mount Anne in the Queen Alexandra Range, Antarctica. It was discovered by the British Antarctic Expedition, 1907–09, and named for Elizabeth Dawson-Lambton, a supporter of the expedition. Events * On 23 January 2013, C-GKBC (c/n:650), a Kenn Borek Air DHC-6 Twin Otter skiplane, with three Canadians on board, crashed onto Mount Elizabeth. The Emergency Locator Transmitter (ELT) was detected on the same day. The plane had been en route from the South Pole's Amundsen–Scott US station to Terra Nova Bay's Zucchelli Italian station, operating under the auspices of the Italian National Agency for New Technologies, Energy and Sustainable Economic Development (ENEA). The aircraft was found on 25 January 2013. It had impacted at the level. The New Zealand helicopter rescue team which spotted the wreckage reported that the accident was not survivable. Canada has jurisdiction in investigating the crash. Reco ...
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Tillite Glacier
Tillite Glacier () is a tributary glacier flowing northwest from Pagoda Peak in Queen Alexandra Range to join Lennox-King Glacier north of Fairchild Peak. So named by New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62) because it contains outcrops of ancient moraine (tillite image:Geschiebemergel.JPG, Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as ''matrix support'', is d ...), indicative of glacial action in remote Paleozoic times. Glaciers of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ...
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Montgomerie Glacier
Montgomerie Glacier () is a narrow tributary glacier, long, flowing north along the west side of Hampton Ridge in the Queen Alexandra Range of Antarctica to enter Lennox-King Glacier. It was named by the Northern Party of the New Zealand Geological Survey Antarctic Expedition of 1961–62 for John Montgomerie Colonel John Montgomerie (died 1731) was colonial governor of New York and New Jersey from 1728 to 1731. Life Montgomerie was born in the parish of Beith in Scotland. His father, Francis Montgomerie, was a member of the Privy Council under ..., assistant surveyor of that party. References Glaciers of Shackleton Coast {{ShackletonCoast-glacier-stub ...
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Advisory Committee On Antarctic Names
The Advisory Committee on Antarctic Names (ACAN or US-ACAN) is an advisory committee of the United States Board on Geographic Names responsible for recommending commemorative names for features in Antarctica. History The committee was established in 1943 as the Special Committee on Antarctic Names (SCAN). It became the Advisory Committee on Antarctic Names in 1947. Fred G. Alberts was Secretary of the Committee from 1949 to 1980. By 1959, a structured nomenclature was reached, allowing for further exploration, structured mapping of the region and a unique naming system. A 1990 ACAN gazeeter of Antarctica listed 16,000 names. Description The United States does not recognise territorial boundaries within Antarctica, so ACAN assigns names to features anywhere within the continent, in consultation with other national nomenclature bodies where appropriate, as defined by the Antarctic Treaty System. The research and staff support for the ACAN is provided by the United States Geolog ...
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Ohio State University
The Ohio State University, commonly called Ohio State or OSU, is a public land-grant research university in Columbus, Ohio. A member of the University System of Ohio, it has been ranked by major institutional rankings among the best public universities in the United States. Founded in 1870 as the state's land-grant university and the ninth university in Ohio with the Morrill Act of 1862, Ohio State was originally known as the Ohio Agricultural and Mechanical College and focused on various agricultural and mechanical disciplines, but it developed into a comprehensive university under the direction of then-Governor and later U.S. president Rutherford B. Hayes, and in 1878, the Ohio General Assembly passed a law changing the name to "the Ohio State University" and broadening the scope of the university. Admission standards tightened and became greatly more selective throughout the 2000s and 2010s. Ohio State's political science department and faculty have greatly con ...
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New Zealand Geological Survey Antarctic Expedition
The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 1957–1958 expedition The 1957–1958 expedition went to the Ross Dependency and named the Borchgrevink Glacier. Other features named include: * Carter Ridge * Felsite Island * Halfway Nunatak * Hedgehog Island * Moraine Ridge 1958–1959 expedition * Cadwalader Beach * Cape Hodgson * Carter Ridge * Isolation Point * Mountaineer Range * Mount Aurora * Mount Hayward * Mount Henderson (White Island) * Mount Bird. 1960–1961 expedition * Deverall Island * Lonewolf Nunataks 1961–1962 expedition * Aurora Heights * The Boil * Ford Spur * Graphite Peak * Half Century Nunatak * Half Dome Nunatak * Hump Passage * Last Cache Nunatak * Lookout Dome * Montgomerie Glacier * Mount Fyfe * Mount Macdonald * Snowshoe ...
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Kukri Peneplain
The Kukri Peneplain is a near-horizontal and flat unconformity in the Transantarctic Mountains. The peneplain formed by erosion of the granitic and metamorphic basement rocks during the Paleozoic (Silurian to Devonian The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, w ...). Kukri Peneplain dips gently to the west. References Planation surfaces Unconformities Geology of Antarctica Paleozoic Antarctica Transantarctic Mountains {{geology-stub ...
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