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Mount Rees (Victoria Land)
Mount Rees () is a mountain () which rises above the cliffs at the west side of Koettlitz Névé, SSW of Mount Talmadge, Victoria Land. It is named after Margaret N. Rees, geologist, University of Nevada, Las Vegas, who conducted field studies in the Transantarctic Mountains, including the Skelton Glacier area of the Hillary Coast The Hillary Coast is a portion of the coast of Antarctica along the western margin of the Ross Ice Shelf between Minna Bluff and Cape Selborne. It was named by the New Zealand Antarctic Place-Names Committee in 1961 for Sir Edmund Hillary, the le ..., through several seasons, 1984–96. Mountains of Victoria Land Hillary Coast {{Ross-mountain-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Koettlitz Névé
Koettlitz Névé () is a roughly circular névé about wide at the head of Koettlitz Glacier, Victoria Land, Antarctica. The névé is bounded to the west and south by Mount Talmadge, Mount Rees and Mount Cocks, and to the east by Mount Morning Mount Morning is a shield volcano at the foot of the Transantarctic Mountains in Victoria Land, Antarctica. It lies from Ross Island. Mount Morning rises to an elevation of and is almost entirely mantled with snow and ice. A wide summit calder .... It was named by the Advisory Committee on Antarctic Names in 1994 in association with Koettlitz Glacier. References Snow fields of the Ross Dependency Landforms of Victoria Land Scott Coast Névés of Antarctica {{ScottCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Talmadge
Mount Talmadge () is a mountain (2,395 m) which rises above the steep cliffs at the west side of Koettlitz Neve, 3 nautical miles (6 km) south of Fisher Bastion, Victoria Land. Named by Advisory Committee on Antarctic Names (US-ACAN) in 1994 after John B. Talmadge, Head of Polar Coordination and Information Section (1984–95), Office of Polar Programs, National Science Foundation The National Science Foundation (NSF) is an independent agency of the United States government that supports fundamental research and education in all the non-medical fields of science and engineering. Its medical counterpart is the National I ... (NSF). Mountains of Victoria Land Scott Coast {{ScottCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Victoria Land
Victoria Land is a region in eastern Antarctica which fronts the western side of the Ross Sea and the Ross Ice Shelf, extending southward from about 70°30'S to 78°00'S, and westward from the Ross Sea to the edge of the Antarctic Plateau. It was discovered by Captain James Clark Ross in January 1841 and named after Queen Victoria. The rocky promontory of Minna Bluff is often regarded as the southernmost point of Victoria Land, and separates the Scott Coast to the north from the Hillary Coast of the Ross Dependency to the south. The region includes ranges of the Transantarctic Mountains and the McMurdo Dry Valleys (the highest point being Mount Abbott in the Northern Foothills), and the flatlands known as the Labyrinth. The Mount Melbourne is an active volcano in Victoria Land. Early explorers of Victoria Land include James Clark Ross and Douglas Mawson. In 1979, scientists discovered a group of 309 meteorites in Antarctica, some of which were found near the Allan Hills in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Margaret N
Margaret is a female first name, derived via French () and Latin () from grc, μαργαρίτης () meaning " pearl". The Greek is borrowed from Persian. Margaret has been an English name since the 11th century, and remained popular throughout the Middle Ages. It became less popular between the 16th century and 18th century, but became more common again after this period, becoming the second-most popular female name in the United States in 1903. Since this time, it has become less common, but was still the ninth-most common name for women of all ages in the United States as of the 1990 census. Margaret has many diminutive forms in many different languages, including Maggie, Madge, Daisy, Margarete, Marge, Margo, Margie, Marjorie, Meg, Megan, Rita, Greta, Gretchen, and Peggy. Name variants Full name * ( Irish) * ( Irish) * ( Dutch), (German), (Swedish) * ( English) Diminutives * ( English) * ( English) First half * (French) * (Welsh) Second half * ( En ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Transantarctic Mountains
The Transantarctic Mountains (abbreviated TAM) comprise a mountain range of uplifted (primarily sedimentary rock, sedimentary) rock in Antarctica which extend, with some interruptions, across the continent from Cape Adare in northern Victoria Land to Coats Land. These mountains divide East Antarctica and West Antarctica. They include a number of separately named mountain groups, which are often again subdivided into smaller ranges. The range was first sighted by James Clark Ross in 1841 at what was later named the Ross Ice Shelf in his honour. It was first crossed during the British National Antarctic Expedition of 1901-1904. Geography The mountain range stretches between the Ross Sea and the Weddell Sea, the entire width of Antarctica, hence the name. With a total length of about , the Transantarctic Mountains are one of the longest mountain ranges on Earth. The Antarctandes are even longer, having in common with the Transantarctic Mountains the ranges from Cape Adare to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skelton Glacier
Skelton Glacier is a large glacier flowing from the polar plateau into the Ross Ice Shelf at Skelton Inlet on the Hillary Coast, south of Victoria Land, Antarctica. Discovery and naming Named after the Skelton Inlet by the New Zealand party of the CTAE, 1956–58. The glacier was chosen in 1957 as the New Zealand party's route from the Ross Ice Shelf to the polar plateau in support of the main expedition led by Vivian Fuchs to make the first overland crossing of the continent. Allison Glacier descends from the west slopes of Royal Society Range into Skelton Glacier. It was also the route of the four month Victoria Land Traverse 1959-1960 which ascended the Skelton Glacier from the Ross Ice Shelf to make the first entry into the deep interior of Victoria Land from the head of the Skelton Glacier to the French Adelie Land Traverse of 1958-1959 near Dumont d'Urville Station on George V Coast, and thence to the Transantarctic Mountains in the vicinity of the USARP Mountains. See ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hillary Coast
The Hillary Coast is a portion of the coast of Antarctica along the western margin of the Ross Ice Shelf between Minna Bluff and Cape Selborne. It was named by the New Zealand Antarctic Place-Names Committee in 1961 for Sir Edmund Hillary, the leader of the New Zealand Party of the Commonwealth Trans-Antarctic Expedition, 1956–58. Various New Zealand parties carried out detailed surveys of portions of this coast and pioneered routes up Skelton Glacier Skelton Glacier is a large glacier flowing from the polar plateau into the Ross Ice Shelf at Skelton Inlet on the Hillary Coast, south of Victoria Land, Antarctica. Discovery and naming Named after the Skelton Inlet by the New Zealand party ... and Darwin Glacier to the polar plateau. References Coasts of the Ross Dependency Edmund Hillary {{RossDependency-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Victoria Land
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
