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Bethanga
Bethanga is a town in north-eastern Victoria (Australia), Victoria, Australia in the Shire of Towong Local government in Australia, local government area, from the state capital, Melbourne. At the 2016 Australian census, 2016 census, Bethanga had a population of 471 and gives its name to the Bethanga Bridge. Mining History Mining prior to 1876 Prior to 1876 gold mining in the Bethanga district occurred to the north of the town and were known as the 'Talgarno diggings'. Reports of alluvial gold date back to 1852. Early gold fields were worked at Ruby Creek, Gold Creek and Jarvis Creek. The opening of the Bethanga goldfields began with the discovery of a gold-bearing quartz reef on New Years Day 1876. The 'Gift' mine site is located south east of Kurrajong Gap lookout to the west of Bethanga township. Mining 1876 - 1910 Bethanga was established as a result of the Victorian gold rush, discovery of gold. Gold was first reported in the Bethanga area in 1852, but it was not unt ...
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Bethanga August 2012
Bethanga is a town in north-eastern Victoria, Australia in the Shire of Towong local government area, from the state capital, Melbourne. At the 2016 census, Bethanga had a population of 471 and gives its name to the Bethanga Bridge. Mining History Mining prior to 1876 Prior to 1876 gold mining in the Bethanga district occurred to the north of the town and were known as the 'Talgarno diggings'. Reports of alluvial gold date back to 1852. Early gold fields were worked at Ruby Creek, Gold Creek and Jarvis Creek. The opening of the Bethanga goldfields began with the discovery of a gold-bearing quartz reef on New Years Day 1876. The 'Gift' mine site is located south east of Kurrajong Gap lookout to the west of Bethanga township. Mining 1876 - 1910 Bethanga was established as a result of the discovery of gold. Gold was first reported in the Bethanga area in 1852, but it was not until 1876 that the discovery of a reef led to the development of the Bethanga goldfields. Th ...
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Bethanga Gold Field
Bethanga is a town in north-eastern Victoria, Australia in the Shire of Towong local government area, from the state capital, Melbourne. At the 2016 census, Bethanga had a population of 471 and gives its name to the Bethanga Bridge. Mining History Mining prior to 1876 Prior to 1876 gold mining in the Bethanga district occurred to the north of the town and were known as the 'Talgarno diggings'. Reports of alluvial gold date back to 1852. Early gold fields were worked at Ruby Creek, Gold Creek and Jarvis Creek. The opening of the Bethanga goldfields began with the discovery of a gold-bearing quartz reef on New Years Day 1876. The 'Gift' mine site is located south east of Kurrajong Gap lookout to the west of Bethanga township. Mining 1876 - 1910 Bethanga was established as a result of the discovery of gold. Gold was first reported in the Bethanga area in 1852, but it was not until 1876 that the discovery of a reef led to the development of the Bethanga goldfields. The Gr ...
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Bethanga Bridge
The Bethanga Bridge is a steel truss road bridge that carries the Riverina Highway across Lake Hume, an artificial lake on the Murray River in Australia. The dual heritage-listed bridge crosses the border between the Australian states of New South Wales and Victoria, linking the Victorian towns of Bellbridge and Bethanga with the regional New South Wales city of Albury. History Context The first crossing of the Murray River by white men occurred in November 1824 when Hamilton Hume and William Hovell led an expedition from Yass in search of an overland route to Westernport Bay. Their crossing point was some distance up river from Albury and an obelisk near the river commemorates this. Hume and Hovell came upon the river on 16 November 1824, naming it the Hume River, and inscribing a tree near the riverbank the next day before moving on to the south. In 1829, the explorer Captain Charles Sturt discovered the Hume River downstream at its junction with the Murrumbidgee River. Not ...
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Wodonga Saints Football Club
The Wodonga Saints Football Netball Club is an Australian rules football and netball club playing their home games at Martin Park in Wodonga, Victoria, Australia. Originally established as the Bethanga Football Club in 1907, with the club was based at the Bethanga Park Recreation Reserve, Bethanga, Victoria, Australia up until 2001. Following the 1999 Victorian Country Football League report that stated a number of clubs, including Bethanga, were on the verge of collapsing if some kind of action was not taken. After playing a handful of matches at Wodonga's Martin Park to see if there would be enough local support to support the club moving there, the club made the decision in 2002 and Bethanga FC relocated fully to Martin Park, Wodonga & were renamed as the Wodonga Saints Football Club. History Bethanga Football Club The Bethanga Football Club was established in 1907 and initially played in the Mitta Mitta Football League (Tallangatta Football Association) with its first mat ...
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Bellbridge, Victoria
Bellbridge is a small town in the state of Victoria. Overlooking the Lake Hume and located near the Bethanga Bridge, Bellbridge is a popular destination for local tourists, especially from the nearby towns of Albury and Wodonga Wodonga ( Waywurru: ''Wordonga'') is a city on the Victorian side of the border with New South Wales, north-east of Melbourne, Australia. It is located wholly within the boundaries of the City of Wodonga LGA. Its population is approximately 35 ... who often come to the Weir to water ski. The local Hume Boat Club holds an annual get-together for water skiers from across Victoria. The township itself developed from farming land in the 1960s. At the 2021 census, Bellbridge had a population of 393. References * https://web.archive.org/web/20130420101642/http://www.filmnortheastvictoria.com.au/region/index.php?town=bellbridge Towns in Victoria (Australia) Shire of Towong {{Hume-geo-stub ...
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Lake Hume
Hume Dam, formerly the Hume Weir, is a major dam across the Murray River downstream of its junction with the Mitta River in the Riverina region of New South Wales, Australia. The dam's purpose includes flood mitigation, hydroelectricity, hydro-power, irrigation, water supply and conservation. The impounded reservoir is called Lake Hume, formerly the Hume Reservoir. It is a gated gravity dam, concrete gravity dam with four embankment dam, earth embankments and twenty-nine Spillway#Types, vertical undershot gated concrete overflow spillways. Location Constructed over a 17-year period between 1919 and 1936, the Hume Dam is located approximately east of the city of Albury. The dam was built, involving a workforce of thousands, by a consortium of Government of New South Wales, NSW and Victoria State Government, Victorian government agency, government agencies that included the Water Resources Commission of New South Wales, the Public Works Department of New South Wales, and the State ...
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Quartz
Quartz is a hard, crystalline mineral composed of silica ( silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold. There are many different varieties of quartz, several of which are classified as gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia. Quartz is the mineral definin ...
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Schists
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture reflects a high content of platy minerals, such as micas, talc, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is usually given a name reflecting its protolith, such as ''schistose me ...
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