Buckland River (Victoria)
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Buckland River (Victoria)
The Buckland River, a perennial river of the North-East Murray catchment of the Murray-Darling basin, is located in the alpine region of Victoria, Australia. It flows from the eastern slopes of the Buffalo Range in the Australian Alps, joining with the Ovens River at Porepunkah. Location and features Formed by the east and west branches of the river, the headwaters of the Buckland River rise in the Barry Mountains below Mount Selwyn and The Twins at an elevation exceeding above sea level. The east and west branches of the river reach their confluence upstream of Beveridges Station, where the watercourse becomes Buckland River. The river flows generally north, much of its course through the remote Mount Buffalo National Park, joined by eight minor tributaries, before reaching its confluence with the Overs River near the small settlement of Porepunkah, located within the Alpine Shire. The river descends over its course. The catchment area to the off-take weir at the Bucklan ...
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Mount Buffalo National Park
The Mount Buffalo National Park is a national park in the alpine region of Victoria, Australia. The national park is located approximately northeast of Melbourne in the Australian Alps. Within the national park is Mount Buffalo, a moderately high mountain plateau, with an elevation of above sea level. On 4 November 1898 an area of was reserved around the plateau and Eurobin Falls as Mount Buffalo National Park, making it one of the oldest national parks in Australia. In 1908 a road was opened to the plateau and the park was expanded to ; and in 1980 to its current size to take in most of the surrounding foothill country. On 7 November 2008, the park was added to the Australian National Heritage List as one of eleven areas constituting the Australian Alps National Parks and Reserves. Location and features Mount Buffalo is a moderately tall mountain plateau on the west side of the Victorian Alpine region. The top of the mountain has striking granite boulders and rock formati ...
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Australian Alps
The Australian Alps is a mountain range in southeast Australia. It comprises an interim Australian bioregion,IBRA Version 6.1
data
and is the highest mountain range in Australia. The range straddles the borders of eastern , southeastern , and the . It contains Australia's only peaks exceeding in elevation, and is the only bioregion on the Australian main ...
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Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ...
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Silurian
The Silurian ( ) is a geologic period and system spanning 24.6 million years from the end of the Ordovician Period, at million years ago ( Mya), to the beginning of the Devonian Period, Mya. The Silurian is the shortest period of the Paleozoic Era. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by a few million years. The base of the Silurian is set at a series of major Ordovician–Silurian extinction events when up to 60% of marine genera were wiped out. One important event in this period was the initial establishment of terrestrial life in what is known as the Silurian-Devonian Terrestrial Revolution: vascular plants emerged from more primitive land plants, dikaryan fungi started expanding and diversifying along with glomeromycotan fungi, and three groups of arthropods (myriapods, arachnids and hexapods) became fully terrestrialized. A significant evolutionary milestone during ...
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Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ...
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Upper Ordovician
The Ordovician ( ) is a geologic period and system, the second of six periods of the Paleozoic Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. The Ordovician, named after the Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official period of the Paleozoic Era by the International Geological Congress. Life continued to flourish during the Ordovician as it did in the earlier Cambrian Per ...
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Siltstone
Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility.Blatt ''et al.'' 1980, pp.381-382 Although its permeability and porosity is relatively low, siltstone is sometimes a tight gas reservoir rock, an unconventional reservoir for natural gas that requires hydraulic fracturing for economic gas production. Siltstone was prized in ancient Egypt for manufacturing statuary and cosmetic palettes. The siltstone quarried at Wadi Hammamat was a hard, fine-grained siltstone that resisted flaking and was almost ideal for such uses. Description There is not complete agreement on the definition of siltstone. One definition is that siltstone is mudrock ( clastic sedimentary rock containing at least 50% clay and silt) in which at least 2/3 of the clay and silt fraction is composed of silt-sized particles. Silt is defined a ...
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Bureau Of Meteorology
The Bureau of Meteorology (BOM or BoM) is an executive agency of the Australian Government responsible for providing weather services to Australia and surrounding areas. It was established in 1906 under the Meteorology Act, and brought together the state meteorological services that existed before then. The states officially transferred their weather recording responsibilities to the Bureau of Meteorology on 1 January 1908. History The Bureau of Meteorology was established on 1 January 1908 following the passage of the ''Meteorology Act 1906''. Prior to Federation in 1901, each colony had had its own meteorological service, with all but two colonies also having a subsection devoted to astronomy. In August 1905, federal home affairs minister Littleton Groom surveyed state governments for their willingness to cede control, finding South Australia and Victoria unwilling. However, at a ministerial conference in April 1906 the state governments agreed to transfer responsibility for m ...
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Government Of Victoria (Australia)
The Victoria State Government, also referred to as just the Victorian Government, is the state-level authority for Victoria, Australia. Like all state governments, it is formed by three independent branches: the executive, the judicial, and the parliament. As a parliamentary constitutional monarchy, the State Government was first formed in 1851 when Victoria first gained the right to responsible government. The Constitution of Australia regulates the relationship between the Victorian Government and the Australian Government, and cedes legislative and judicial supremacy to the federal government on conflicting matters. The Victoria State Government enforces acts passed by the parliament through government departments, statutory authorities, and other public agencies. The Government is formally presided over by the Governor, who exercises executive authority granted by the state's constitution through the Executive Council, a body consisting of senior cabinet ministers. In re ...
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Henry Winneke
Sir Henry Arthur Winneke, (20 October 1908 – 28 December 1985) was a Chief Justice of Victoria and the 21st Governor of Victoria, from 1974 to 1982. Early life and career Winneke was born on 20 October 1908 to the descendants of German immigrants to Victoria. His father, Henry Christian Winneke, was a judge of the County Court of Victoria. Winneke was educated at Ballarat Grammar School, Scotch College and the University of Melbourne, from which he graduated with a Bachelor of Laws in 1929 and a Master of Laws in 1930. He was a hockey player while at university, and was awarded a University Blue as well as playing in an Australian Universities team. From 1930 to 1932, he also held a lieutenant's commission in the Melbourne University Rifles. After doing articles at the solicitors firm Gair & Brahe, he was admitted to practice in the Supreme Court of Victoria on 1 May 1931 and called to the Victorian Bar on 30 July 1931. He read as a pupil of Wilfred Fullagar, who was late ...
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Governor Of Victoria
The governor of Victoria is the representative of the monarch, King Charles III, in the Australian state of Victoria. The governor is one of seven viceregal representatives in the country, analogous to the governors of the other states, and the governor-general federally. The governor is appointed by the monarch on the advice of the premier of Victoria. The governor's role is to represent the Crown in right of Victoria. This role mainly includes performing ceremonial functions, such as opening and dissolving Parliament, appointing the Cabinet, and granting royal assent. The governor's office and official residence is Government House next to the Royal Botanic Gardens and surrounded by Kings Domain in Melbourne. The current governor of Victoria is Linda Dessau, Victoria's first female governor. Powers In accordance with the conventions of the Westminster system of parliamentary government, the governor nearly always acts solely on the advice of the head of the elected gover ...
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