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Mount Darwin, Tasmania
Mount Darwin is a mountain located in the West Coast region of Tasmania, Australia. With an elevation of above sea level, the mountain is situated on the West Coast Range. On the eastern side of the mountain is Darwin, a long-abandoned town site. Mount Darwin is the southernmost mountain of the West Coast range. Mount Jukes is north of the mountain while Mount Sorell is west of it. The mountain is named in honour of Charles Darwin. Mine sites Long abandoned short drives and shallow holes are found on Mount Darwin and are usually cited as being part of the Jukes-Darwin field. Features and access The mountain has a plateau and has mining exploration tracks that lead to some of the older workings. It was possible in the 1970s to travel to the top of Mount Darwin in four wheel drive vehicles. The tracks also lead over towards the Clark River Valley which lies between Darwin and Mount Sorell to the west, and some tracks also were made on the ridge between Mount Darwin and t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tasmania
Tasmania (; palawa kani: ''Lutruwita'') is an island States and territories of Australia, state of Australia. It is located to the south of the Mainland Australia, Australian mainland, and is separated from it by the Bass Strait. The state encompasses the main island of Tasmania, the List of islands by area#Islands, 26th-largest island in the world, and the List of islands of Tasmania, surrounding 1000 islands. It is Australia's smallest and least populous state, with 573,479 residents . The List of Australian capital cities, state capital and largest city is Hobart, with around 40% of the population living in the Greater Hobart area. Estimated resident population, 30 June 2017. Tasmania is the most decentralised state in Australia, with the lowest proportion of its residents living within its capital city. Tasmania's main island was first inhabited by Aboriginal Australians, Aboriginal peoples, who today generally identify as Palawa or Pakana. It is believed that Abori ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Peaks Of Lyell
''The Peaks of Lyell'' is a book by Geoffrey Blainey, based on his University of Melbourne MA thesis that was originally published in 1954. It contains the history of the Mount Lyell Mining and Railway Company, and through association, Queenstown and further the West Coast Tasmania. It is unique for this type of book in that it has gone to the sixth edition in 2000, and few company histories in Australia have achieved such continual publishing. Blainey was fortunate in being able to speak to older people about the history of the West Coast, some who had known Queenstown in its earliest years. The book gives an interesting overview from the materials and people Blainey was able to access in the early 1950s, and the omissions. Due to the nature of a company history, a number of items of Queenstown history did have alternative interpretations on events such as the 1912 North Mount Lyell Disaster, and there were residents of Queenstown living in the town as late as the 1970s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Highest Mountains Of Tasmania
The Australian island state of Tasmania has a diverse range of geography but a prominent feature is the mountains of the island. Overall Tasmania is comparatively low-lying with the highest point at . Tasmania has ten peaks over the height of . With thirty peaks higher than , it is one of the most mountainous islands in the world, and Tasmania is Australia's most mountainous state. The majority of the mountain peaks of Tasmania are located in the Western half of the state, starting at the coast in the South West and extending inland to the north, or in the Central Highlands. Tasmania's mountains were part of an ancient range of volcanic peaks from the period of Gondwana, and are the source of a large portion of Tasmania's wealth in the form of mining. Although the eastern half of the state is generally lower and flatter, there are still sizeable peaks located there, such as kunanyi/Mt Wellington. Notable peaks The following notable mountain peaks in Tasmania range in h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1855 - 1900)
Events January–March * January 1 – Ottawa, Ontario, is incorporated as a city.' * January 5 – Ramón Castilla begins his third term as President of Peru. * January 23 ** The first bridge over the Mississippi River opens in modern-day Minneapolis, a predecessor of the Father Louis Hennepin Bridge. ** The 8.2–8.3 Wairarapa earthquake claims between five and nine lives near the Cook Strait area of New Zealand. * January 26 – The Point No Point Treaty is signed in the Washington Territory. * January 27 – The Panama Railway becomes the first railroad to connect the Atlantic and Pacific Oceans. * January 29 – Lord Aberdeen resigns as Prime Minister of the United Kingdom, over the management of the Crimean War. * February 5 – Lord Palmerston becomes Prime Minister of the United Kingdom. * February 11 – Kassa Hailu is crowned Tewodros II, Emperor of Ethiopia. * February 12 – Michigan State University (the "pioneer" land-g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Impact Crater
An impact crater is a depression (geology), depression in the surface of a solid astronomical body formed by the hypervelocity impact event, impact of a smaller object. In contrast to volcanic craters, which result from explosion or internal collapse, impact craters typically have raised rims and floors that are lower in elevation than the surrounding terrain. Impact craters are typically circular, though they can be elliptical in shape or even irregular due to events such as landslides. Impact craters range in size from microscopic craters seen on lunar rocks returned by the Apollo Program to simple bowl-shaped depressions and vast, complex, multi-ringed impact basins. Meteor Crater is a well-known example of a small impact crater on Earth. Impact craters are the dominant geographic features on many solid Solar System objects including the Moon, Mercury (planet), Mercury, Callisto (moon), Callisto, Ganymede (moon), Ganymede, and most small moons and asteroids. On other planet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Darwin Crater
Darwin Crater is a suspected meteorite impact crater in Western Tasmania about south of Queenstown, just within the Franklin-Gordon Wild Rivers National Park. The crater is expressed as a rimless circular flat-floored depression, in diameter, within mountainous and heavily forested terrain. It is east of the West Coast Range and the former North Mount Lyell Railway formation. Discovery and description The crater was discovered by the geologist R. J. Ford in 1972, after a search for the source of Darwin glass, an impact glass found over more than of southwestern Tasmania. Geophysical investigations and drilling have shown that the crater is filled with up to of breccia capped by Pleistocene lake sediments. Although definitive proof of an impact origin of the crater is lacking, the impact hypothesis is strongly supported by the relationship of the glass to the crater, as well as the stratigraphy and deformation of the crater-filling material. If the crater is indeed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau
In geology and physical geography, a plateau (; ; : plateaus or plateaux), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wider ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, plate tectonics movements, and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. They may be formed by upwelling of volcanic magma or extrusion of lava. The underlining mechanism in forming p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charles Darwin
Charles Robert Darwin ( ; 12 February 1809 – 19 April 1882) was an English Natural history#Before 1900, naturalist, geologist, and biologist, widely known for his contributions to evolutionary biology. His proposition that all species of life have descended from a Common descent, common ancestor is now generally accepted and considered a fundamental scientific concept. In a joint presentation with Alfred Russel Wallace, he introduced his scientific theory that this Phylogenetics, branching pattern of evolution resulted from a process he called natural selection, in which the struggle for existence has a similar effect to the artificial selection involved in selective breeding.. Darwin has been described as one of the most influential figures in human history and was honoured by Burials and memorials in Westminster Abbey, burial in Westminster Abbey. Darwin's early interest in nature led him to neglect his medical education at the University of Edinburgh Medical Schoo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Coast, Tasmania
The West Coast of Tasmania is one of the regions of Tasmania in Australia. It is mainly isolated rough country and is associated with wilderness, mining and tourism. It served as the location of an early convict settlement in the early history of Van Diemen's Land, and contrasts sharply with the more developed and populous northern and eastern parts of the island state. Climate The west coast has a much cooler and wetter climate when compared to the east coast. Frequent low pressure systems hit the west coast causing heavy rain, snow, and ice. The West Coast Range blocks these systems from impacting the east, therefore making the West Coast a rain catchment with some areas receiving over of rain a year. In winter temperatures at sea level hover around , and when not raining, morning frost is common. The temperatures are much lower inland from the coast with maximums in winter often failing to surpass . Typically, the snow line in winter is around 900 metres (3000 ft), h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
