Avon River (Grampians, Victoria)
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Avon River (Grampians, Victoria)
The Avon River, an inland intermittent river of the Wimmera catchment, located in the Grampians and Wimmera regions of the Australian state of Victoria. Rising on the northern slopes of the Great Dividing Range, the Avon River flows north-westerly to reach its confluence with the Richardson River. The rivers of the Wimmera catchment drain into a series of ephemeral lakes that, whilst they do not directly empty into a defined watercourse, form part of the Murray River catchment of the Murray-Darling basin. Location and features The Avon River rises on the northern slopes of the Great Dividing Range, near Beazleys Bridge, west of . The rivers flows in a highly meandering course generally west by north, joined by one minor tributary, before reaching its mouth to flow into the Richardson River at Banyena; northwest of . The Avon River descends over its course. Etymology In a western Kulin Aboriginal language the river and surrounding country is named ''Wityellibar'', fro ...
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Northern Grampians Shire
The Shire of Northern Grampians is a local government area in the Wimmera region of Victoria, Australia, located in the western part of the state. It covers an area of and in June 2018 had a population of 11,431, having fallen from 12,087 in 2008. It includes the towns of Stawell, St Arnaud, Great Western, Marnoo, Glenorchy, Stuart Mill, Navarre and the tourist town of Halls Gap. It was formed in 1995 from the amalgamation of the City of Stawell, Town of St Arnaud, Shire of Stawell, Shire of Kara Kara and parts of the Shire of Wimmera, Shire of Dunmunkle and Shire of Donald. The Shire is governed and administered by the Northern Grampians Shire Council; its seat of local government and administrative centre is located at the council headquarters in Stawell, it also has a service centre located in St Arnaud. The Shire is named after the major geographical feature in the region, The Grampians, and that the northern part of this feature occupies the southern part of the LGA. ...
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Ephemeral Lake
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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Australian Government
The Australian Government, also known as the Commonwealth Government, is the national government of Australia, a federal parliamentary constitutional monarchy. Like other Westminster-style systems of government, the Australian Government is made up of three branches: the executive (the prime minister, the ministers, and government departments), the legislative (the Parliament of Australia), and the judicial. The legislative branch, the federal Parliament, is made up of two chambers: the House of Representatives (lower house) and Senate (upper house). The House of Representatives has 151 members, each representing an individual electoral district of about 165,000 people. The Senate has 76 members: twelve from each of the six states and two each from Australia's internal territories, the Australian Capital Territory and Northern Territory. The Australian monarch, currently King Charles III, is represented by the governor-general. The Australian Government in its executive ca ...
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List Of Rivers In Australia
This is a list of rivers of Australia. Rivers are ordered alphabetically, by state. The same river may be found in more than one state as many rivers cross state borders. Longest rivers nationally Longest river by state or territory Although the Murray River forms much of the border separating New South Wales and Victoria, it is not Victoria's longest river because the New South Wales border is delineated by the river's southern bank rather than by the middle of the river. The only section of the river formally within Victoria is a stretch of approximately where it separates Victoria and South Australia. At this point, the middle of the river forms the border. Rivers by state or territory The following is a list of rivers located within Australian states and territories. Where a river crosses a state or territory boundary, it is listed in both states and territories. Where a river has a name that includes the word creek, it has been officially designated as a river. Aus ...
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Djadjawurrung Language
Djadjawurrung (also Jaara, Ngurai-illam-wurrung) is an Aboriginal Australian language spoken by the Dja Dja Wurrung people of the Kulin nation of central Victoria. Djadjawurrung was spoken by 16 clans around Murchison, the central highlands region, east to Woodend, west to the Pyrenees, north to Boort and south to the Great Dividing Range. Phonology Consonants Vowels There are four vowels noted: . They may also be phonetically written as .Blake, Barry. 2016 References External links Bibliography of Djadja Wurrung people and language resources at the Australian Institute of Aboriginal and Torres Strait Islander Studies The Australian Institute of Aboriginal and Torres Strait Islander Studies (AIATSIS), established as the Australian Institute of Aboriginal Studies (AIAS) in 1964, is an independent Australian Government statutory authority. It is a collecting, ... Dialects of Western Kulin, Western Victoria Yartwatjali, Tjapwurrung, Djadjawurrung Kulin lan ...
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Kulin Nation
The Kulin nation is an alliance of five Aboriginal nations in south central Victoria, Australia. Their collective territory extends around Port Phillip and Western Port, up into the Great Dividing Range and the Loddon and Goulburn River valleys. Before British colonisation, the tribes spoke five related languages. These languages are spoken by two groups: the Eastern Kulin group of Woiwurrung, Boonwurrung, Taungurung and Ngurai-illam-wurrung; and the western language group of just Wathaurung. The central Victoria area has been inhabited for an estimated 40,000 years before European settlement. At the time of British settlement in the 1830s, the collective populations of the Woiwurrung, Boonwurrung and Wathaurong tribes of the Kulin nation was estimated to be under 20,000. The Kulin lived by fishing, cultivating murnong (also called yam daisy; ''Microseris'') as well as hunting and gathering, and made a sustainable living from the rich food sources of Port Phillip and the sur ...
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Mouth (river)
A river mouth is where a river flows into a larger body of water, such as another river, a lake/reservoir, a bay/gulf, a sea, or an ocean. At the river mouth, sediments are often deposited due to the slowing of the current reducing the carrying capacity of the water. The water from a river can enter the receiving body in a variety of different ways. The motion of a river is influenced by the relative density of the river compared to the receiving water, the rotation of the earth, and any ambient motion in the receiving water, such as tides or seiches. If the river water has a higher density than the surface of the receiving water, the river water will plunge below the surface. The river water will then either form an underflow or an interflow within the lake. However, if the river water is lighter than the receiving water, as is typically the case when fresh river water flows into the sea, the river water will float along the surface of the receiving water as an overflow. Alon ...
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Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream."opposite to a tributary"
PhysicalGeography.net, Michael Pidwirny & S ...
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Watercourse
A stream is a continuous body of surface water flowing within the bed and banks of a channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighted subterranean water, and surfaced groundwater (spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes that respond to geological, geomorphological, hydrological and biotic controls. Streams are important as conduits in the water cycle, instruments in groundwater ...
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Meander
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank ( cut bank) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ''Fundamentals ...
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