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Puke Toropa Mountain
Puke Toropa Mountain is a mostly ice-covered mountain in the Royal Society Range of Antarctica. It stands high and is situated south of Mount Rücker. It was named by the New Zealand Geographic Board (NZGB) in 1994. Its name is MÄori MÄori or Maori can refer to: Relating to the MÄori people * MÄori people of New Zealand, or members of that group * MÄori language, the language of the MÄori people of New Zealand * MÄori culture * Cook Islanders, the MÄori people of the C ... in origin and means "circular hill." Mountains of Victoria Land Scott Coast {{ScottCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Royal Society Range
The Royal Society Range () is a mountain range in Victoria Land, Antarctica. With its summit at , the massive Mount Lister forms the highest point in this range. Mount Lister is located along the western shore of McMurdo Sound between the Koettlitz, Skelton and Ferrar glaciers. Other notable local terrain features include Allison Glacier, which descends from the west slopes of the Royal Society Range into Skelton Glacier. Discovery and naming The range was probably first seen by Captain James Clark Ross in 1841. The range was explored by the British National Antarctic Expedition (BrNAE) under Robert Falcon Scott, who named the range after the Royal Society and applied names of its members to many of its peaks. For example, Mount Lister was named for Lord Joseph Lister, President of the Royal Society, 1895–1900. The Royal Society provided financial support to the expedition and its members had assisted on the committee which organized the expedition. Geology The Royal S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antarctica
Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest continent, being about 40% larger than Europe, and has an area of . Most of Antarctica is covered by the Antarctic ice sheet, with an average thickness of . Antarctica is, on average, the coldest, driest, and windiest of the continents, and it has the highest average elevation. It is mainly a polar desert, with annual precipitation of over along the coast and far less inland. About 70% of the world's freshwater reserves are frozen in Antarctica, which, if melted, would raise global sea levels by almost . Antarctica holds the record for the lowest measured temperature on Earth, . The coastal regions can reach temperatures over in summer. Native species of animals include mites, nematodes, penguins, seals and tardigrades. Where vegetation o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Rücker
Mount Rucker is a mountain, , immediately south of Johns Hopkins Ridge in the Royal Society Range of Victoria Land. Discovered by the Discovery Expedition (1901–04) which named it for Sir Arthur Rucker, Honorary Secretary of the Royal Society. Descending east from the mountain, Rucker Ridge () forms the divide between Radian Glacier and Walcott Glacier. It was named after Mount Rucker by the New Zealand Victoria University of Wellington Antarctic Expedition (VUWAE), 1960–61. Sulphide Pass () is a saddle that forms a mountain pass on Rucker Ridge in Antarctica. Its name comes from an exposed band of pyritized shale Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especial ... which gives off a sulphurous smell when struck by an instrument such as a hammer. References Mountains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Geographic Board
The New Zealand Geographic Board NgÄ Pou Taunaha o Aotearoa (NZGB) was established by the New Zealand Geographic Board Act 1946, which has since been replaced by the New Zealand Geographic Board (NgÄ Pou Taunaha o Aotearoa) Act 2008. Although an independent institution, it is responsible to the Minister for Land Information. The board has authority over geographical and hydrographic names within New Zealand and its territorial waters. This includes the naming of small urban settlements, localities, mountains, lakes, rivers, waterfalls, harbours and natural features and may include researching local MÄori names. It has named many geographical features in the Ross Sea region of Antarctica. It has no authority to alter street names (a local body responsibility) or the name of any country. The NZGB secretariat is part of ToitÅ« Te Whenua Land Information New Zealand (LINZ) and provides the board with administrative and research assistance and advice. The New Zealand Geograph ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
MÄori Language
MÄori (), or ('the MÄori language'), also known as ('the language'), is an Eastern Polynesian language spoken by the MÄori people, the indigenous population of mainland New Zealand. Closely related to Cook Islands MÄori, Tuamotuan, and Tahitian, it gained recognition as one of New Zealand's official languages in 1987. The number of speakers of the language has declined sharply since 1945, but a MÄori-language revitalisation effort has slowed the decline. The 2018 New Zealand census reported that about 186,000 people, or 4.0% of the New Zealand population, could hold a conversation in MÄori about everyday things. , 55% of MÄori adults reported some knowledge of the language; of these, 64% use MÄori at home and around 50,000 people can speak the language "very well" or "well". The MÄori language did not have an indigenous writing system. Missionaries arriving from about 1814, such as Thomas Kendall, learned to speak MÄori, and introduced the Latin alphabet. In 1 ... [...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] |
