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Chapman, Australian Capital Territory
Chapman is a suburb of Canberra, Australian Capital Territory, Australia, where many diplomats and some of the wealthier citizens of Canberra chose to take their residency. It is located in the Weston Creek area. The suburb is named after Sir Austin Chapman (1864–1926), the member for Eden-Monaro from 1901 to 1926 who held portfolios in the Deakin and Bruce governments. The theme for the street names in Chapman is the Australian film industry. The local primary school in Chapman is the government run Chapman Primary School on Perry Drive. The school caters for students from Preschool to Year 6 and runs a before and afterschool care program. Geology Laidlaw Volcanics pale to dark grey dacitic tuff covers most of Chapman. Shale, sandstone, ashstone and tuff is found near the west end of Rafferty Street. Quaternary alluvium Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weston Creek (district)
The District of Weston Creek is one of the original eighteen districts of the Australian Capital Territory used in land administration. The district is subdivided into divisions (suburbs), sections and blocks. The district of Weston Creek lies entirely within the bounds of the city of Canberra, the capital city of Australia. The district comprises eight residential suburbs, situated to the west of the Woden Valley district and approximately southwest of the Canberra City centre. Situated adjacent to the district was the large Stromlo Forest pine plantation until the forest was destroyed by bushfires in 2001 and 2003. Weston Creek was named in honour of Captain George Edward Weston, a former officer of the East India Company who arrived in Australia in 1829, and was Superintendent of the Hyde Park Convict Barracks in Sydney. In 1841, Weston was granted land in the district now known as Weston Creek. At the , the population of the district was . Establishment and governance F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Division Of Eden-Monaro
The Division of Eden-Monaro is an Australian electoral division in the state of New South Wales. The previous member, Mike Kelly resigned due to ill health on 30 April 2020. The seat was filled at a by-election on 4 July 2020. Geography Since 1984, federal electoral division boundaries in Australia have been determined at redistributions by a redistribution committee appointed by the Australian Electoral Commission. Redistributions occur for the boundaries of divisions in a particular state, and they occur every seven years, or sooner if a state's representation entitlement changes or when divisions of a state are malapportioned. History The division was proclaimed in 1900, and was one of the original 65 divisions to be contested at the first federal election. It is named for the town of Eden and the Monaro district of southern New South Wales. Its boundaries have changed very little throughout its history, and it includes the towns of Yass, Bega and Cooma and the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desnoye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ashstone
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock containing 25% to 75% ash is described as tuffaceous (for example, ''tuffaceous sandstone''). Tuff composed of sandy volcanic material can be referred to as volcanic sandstone. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Because it is common in Italy, the Romans used it often for construction. The Rapa Nui people used it to make most of the ''moai'' statues on Easter Island. Tuff can be classified as either igneous or sedimentary rock. It is usually studied in the context of igneous petrology, although it is sometimes described using sedimentological terms. Tuff is often erroneously called tufa in guidebooks and in television programmes. Volcanic ash The material that is expelled in a volcanic e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tuff
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock containing 25% to 75% ash is described as tuffaceous (for example, ''tuffaceous sandstone''). Tuff composed of sandy volcanic material can be referred to as volcanic sandstone. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Because it is common in Italy, the Romans used it often for construction. The Rapa Nui people used it to make most of the ''moai'' statues on Easter Island. Tuff can be classified as either igneous or sedimentary rock. It is usually studied in the context of igneous petrology, although it is sometimes described using sedimentological terms. Tuff is often erroneously called tufa in guidebooks and in television programmes. Volcanic ash The material that is expelled in a volcanic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Australian Film Industry
The cinema of Australia had its beginnings with the 1906 production of '' The Story of the Kelly Gang'', arguably the world's first feature film. Since then, Australian crews have produced many films, a number of which have received international recognition. Many actors and filmmakers with international reputations started their careers in Australian films, and many of these have established lucrative careers in larger film-producing centres such as the United States. Commercially successful Australian films include: ''Crocodile Dundee'', George Miller's '' Mad Max: Fury Road'', Baz Luhrmann's ''Moulin Rouge!'', and Chris Noonan's ''Babe''. Award-winning productions include ''Picnic at Hanging Rock'', ''Gallipoli'', ''The Tracker'', ''Shine'' and ''Ten Canoes''. Australian actors of renown include Errol Flynn, Peter Finch, Rod Taylor, Paul Hogan, Jack Thompson, Bryan Brown, Judy Davis, Jacki Weaver, Geoffrey Rush, Hugo Weaving, Eric Bana, Guy Pearce, Hugh Jackman, C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stanley Bruce
Stanley Melbourne Bruce, 1st Viscount Bruce of Melbourne, (15 April 1883 – 25 August 1967) was an Australian politician who served as the eighth prime minister of Australia from 1923 to 1929, as leader of the Nationalist Party. Born into a briefly wealthy Melbourne family, Bruce studied at the University of Cambridge and spent his early life tending to the importing and exporting business of his late father. He served on the front lines of the Gallipoli Campaign in World War I and returned to Australia wounded in 1917, becoming a spokesperson for government recruitment efforts. He gained the attention of the Nationalist Party and prime minister Billy Hughes, who encouraged a political career. He was elected to the House of Representatives in 1918, becoming a member of parliament (MP) for the seat of Flinders. He was appointed as treasurer in 1921, before replacing Hughes as prime minister in 1923, at the head of a coalition with the Country Party. In office, Bruce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alfred Deakin
Alfred Deakin (3 August 1856 – 7 October 1919) was an Australian politician who served as the second Prime Minister of Australia. He was a leader of the movement for Federation, which occurred in 1901. During his three terms as prime minister over the subsequent decade (1903–1904, 1905–1908, 1909–1910), he played a key role in establishing national institutions. Deakin was born in Melbourne to middle-class parents. He was elected to the Victorian Legislative Assembly in 1879, aged 23, additionally working as a barrister and journalist. He held ministerial office sporadically beginning in 1883, serving twice as Attorney-General of Victoria and aligning himself with liberal and radical reformers. In the 1890s Deakin became one of the leading figures in the movement for the federation of the Australian colonies. He was a delegate to the federal conventions and served on the committees that drafted the federal constitution. He later campaigned at a series of referendums ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austin Chapman
Sir Austin Chapman (10 July 186412 January 1926) was an Australian politician who served in the House of Representatives from 1901 until his death in 1926. He held ministerial office in the governments of Alfred Deakin and Stanley Bruce, serving as Minister for Defence (1903–1904), Postmaster-General (1905–1907), Minister for Trade and Customs (1907–1908, 1923–1924), and Minister for Health (1923–1924). Early life Chapman was born on 10 July 1864 in Bong Bong, New South Wales. He was the son of Monica (née Cain; also spelt Kean or Kein) and Richard Chapman, his father being a wheelwright and publican. His mother was born in Ireland. His given name was spelled "Austen" until 1897. Chapman attended the state school in Marulan until the age of 14, when he was apprenticed to a saddler working in Goulburn and Mudgee. By 1885 he was operating Chapman's Hotel in Bungendore, close to the eventual site of Canberra. Chapman moved to Sydney in 1887 and went into partnership ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Murrumbidgee Electorate
The Murrumbidgee electorate is one of the five electorates for the unicameral 25-member Australian Capital Territory Legislative Assembly. It elected five members at the 2016 ACT election. History Murrumbidgee was created in 2016, when the five-electorate, 25-member Hare-Clark electoral system was first introduced for the Australian Capital Territory (ACT) Legislative Assembly, replacing the previous three-electorate, 17-member system. The electorate is named after the Murrumbidgee River which flows through the electorate, with the word "Murrumbidgee" meaning "big water" in the Aboriginal Wiradjuri language. Location The Murrumbidgee electorate consists of the Woden Valley suburbs of Chifley, Curtin, Farrer, Garran, Hughes, Isaacs, Lyons, Mawson, O'Malley, Pearce, Phillip, Torrens, the Weston Creek suburbs of Chapman, Duffy, Fisher, Holder, Rivett, Stirling, Waramanga, Weston, the Molonglo Valley suburbs of Coombs, Denman Prospect, Whitlam and Wright, the South Canb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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