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Mitchell River (Victoria)
The Mitchell River is a perennial river of the East Gippsland catchment, located in the Australian state of Victoria. The unregulated river provides a unique example of riparian ecology, flowing generally south with the catchment area drawing from the steep mountains of the Victorian Alps to enter Lake King, one of the Gippsland Lakes, and then empty into the Bass Strait. Course and features Formed by the confluence of the Wentworth and Wonnangatta rivers and Swamp Creek near Horseshoe Bend, north of the national park that bears its name, the Mitchell River rises in Lake Tabberabbera, drained by runoff from the southern Victorian Alps of the Great Dividing Range. The river flows generally south in a highly meandering course in its upper reaches through the Mitchell River National Park, and then south by east as it spills onto the fertile Gippsland Plain west of . The river then flows generally east towards and empties into Jones Bay, part of Lake King, within the Gi ...
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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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Mitchell River National Park (Victoria)
The Mitchell River National Park is a national park located in the Gippsland region of Victoria, Australia. The national park is situated approximately east of Melbourne via the Princes Highway, and approximately northwest of Bairnsdale. The northern portion of the park may be accessed via . Mitchell River The park's central feature is the Mitchell River, which is the largest unregulated river in Victoria and provides a unique example of riparian ecology. According to a Land Conservation Council Rivers & Streams Special Investigation completed in 1990, "It is an important example of the large-scale biological systems that were once widespread in south-eastern Australia." In 1992 the Mitchell River was listed as a Heritage River. The park The national park surrounds the spectacular Mitchell River where it has cut its way through rock strata creating high cliffs and several gorges. The park originated as the ''Glenaladale National Park'' in 1963 following a donation of o ...
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Confluence
In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); or where two streams meet to become the source of a river of a new name (such as the confluence of the Monongahela and Allegheny rivers at Pittsburgh, forming the Ohio); or where two separated channels of a river (forming a river island) rejoin at the downstream end. Scientific study of confluences Confluences are studied in a variety of sciences. Hydrology studies the characteristic flow patterns of confluences and how they give rise to patterns of erosion, bars, and scour pools. The water flows and their consequences are often studied with mathematical models. Confluences are relevant to the distribution of living organisms (i.e., ecology) as well; "the general pattern ownstream of confluencesof increasing stream flow and decreasing s ...
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Bass Strait
Bass Strait () is a strait separating the island state of Tasmania from the Australian mainland (more specifically the coast of Victoria, with the exception of the land border across Boundary Islet). The strait provides the most direct waterway between the Great Australian Bight and the Tasman Sea, and is also the only maritime route into the economically prominent Port Phillip Bay. Formed 8,000 years ago by rising sea levels at the end of the last glacial period, the strait was named after English explorer and physician George Bass (1771-1803) by European colonists. Extent The International Hydrographic Organization defines the limits of Bass Strait as follows: :''On the west.'' The eastern limit of the Great Australian Bight eing a line from Cape Otway, Australia, to King Island (Tasmania)">King Island and thence to Cape Grim, the northwest extreme of Tasmania]. :''On the east.'' The western limit of the Tasman Sea between Gabo Island and Eddystone Point eing a line fr ...
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Victorian Alps
The Victorian Alps, also known locally as the High Country, is a large mountain system in the southeastern Australian state of Victoria. Occupying the majority of eastern Victoria, it is the southwestern half of the Australian Alps (the other half being the Snowy Mountains), the tallest portion of the Great Dividing Range. The Yarra and Dandenong Ranges, both sources of rivers and drinking waters for Melbourne (Victoria's capital, largest city and home to three quarters of the state's population), are branches of the Victorian Alps. The promise of gold in the mid-1800s, during the Victorian Gold rush led to the European settlement of the area. The region's rich natural resources brought a second wave of agricultural settlers; the foothills around the Victorian Alps today has a large agrarian sector, with significant cattle stations being sold recently for over thirty million dollars. The Victorian Alps is also the source of many of Victoria's water ways, including Murray ...
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Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ...
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Riparian
A riparian zone or riparian area is the interface between land and a river or stream. Riparian is also the proper nomenclature for one of the terrestrial biomes of the Earth. Plant habitats and communities along the river margins and banks are called riparian vegetation, characterized by hydrophilic plants. Riparian zones are important in ecology, environmental resource management, and civil engineering because of their role in soil conservation, their habitat biodiversity, and the influence they have on fauna and aquatic ecosystems, including grasslands, woodlands, wetlands, or even non-vegetative areas. In some regions, the terms riparian woodland, riparian forest, riparian buffer zone, riparian corridor, and riparian strip are used to characterize a riparian zone. The word ''riparian'' is derived from Latin '' ripa'', meaning " river bank". Characteristics Riparian zones may be natural or engineered for soil stabilization or restoration. These zones are important natural b ...
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Perennial Stream
A perennial stream is a stream that has continuous flow of surface water throughout the year in at least parts of its catchment during seasons of normal rainfall, Water Supply Paper 494. as opposed to intermittent river, one whose flow is intermittent. In the absence of irregular, prolonged or extreme drought, a perennial stream is a watercourse, or segment, element or emerging body of water which continually delivers groundwater. For example, an damming, artificial disruption of stream, variability in flow or stream selection associated with the activity in hydropower installations, do not affect this status. Perennial streams do not include stagnant water (stream pool, pools and puddle, waterholes), reservoirs, oxbow lake, cutoff lakes and ponds that persist throughout the year. All other streams, or parts of them, should be considered seasonal rivers or lakes. The stream can cycle from intermittent to perpetual through multiple iterations. Stream Definition The basic conc ...
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National Park
A national park is a nature park, natural park in use for conservation (ethic), conservation purposes, created and protected by national governments. Often it is a reserve of natural, semi-natural, or developed land that a sovereign state declares or owns. Although individual nations designate their own national parks differently, there is a common idea: the conservation of 'wild nature' for posterity and as a symbol of national pride. The United States established the first "public park or pleasuring-ground for the benefit and enjoyment of the people", Yellowstone National Park, in 1872. Although Yellowstone was not officially termed a "national park" in its establishing law, it was always termed such in practice and is widely held to be the first and oldest national park in the world. However, the Tobago Main Ridge Forest Reserve (in what is now Trinidad and Tobago; established in 1776), and the area surrounding Bogd Khan Mountain, Bogd Khan Uul Mountain (Mongolia, 1778), wh ...
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Latrobe River
The Latrobe River (or sometimes La Trobe or LaTrobe) is a perennial river of the West Gippsland catchment, located in the West Gippsland region of the Australian state of Victoria. The Latrobe River and its associated sub-catchment is an important source for the Gippsland Lakes, draining the south eastern slopes of the Great Dividing Range. Course and features The Latrobe River rises below Dick Hill, from the southern slopes of the Baw Baw plateau, part of the Great Dividing Range, between Powelltown and Noojee where it shares a watershed with the Little Yarra River, in a state forestry area. The river flows generally in an easterly direction, then south, and then east again through the Latrobe Valley, joined by seventeen tributaries including the Ada, Toorongo, Loch, Tanjil, Morwell, Tyers, and Thomson rivers, before reaching its mouth in Lake Wellington east of where it forms its confluence with the Avon. It then goes to flow out of Lake Wellington and into Lake V ...
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Woolshed Creek
Hatton Vale is a rural locality in the Lockyer Valley Region, Queensland, Australia. In the , Hatton Vale had a population of 1,521 people. Geography Hatton Vale is in South East Queensland and on the Warrego Highway, west of the state capital Brisbane and west of the regional centre of Ipswich. History Hatton Vale, originally known as "Tarampa Woolshed" was settled by German migrants in the 1870s as part of a closer settlement arrangement. The migrants established a Lutheran church in 1881 and an Apostolic church in 1889. The evangelist Heinrich Friedrich Niemeyer established Hatton Vale as the centre of the Apostolic Church of Queensland. Hatton Vale Provisional School opened in 1881. On 18 October 1886, it became Hatton Vale State School. Hatton Vale Post Office opened by 1903 (a receiving office had been open from 1881, known as Woolshed Creek until 1889) and closed in 1974. The locality remained overwhelmingly German in character. A survey in 1902 identified 90% of th ...
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Mississippi Creek
Mississippi Creek is a tributary stream to Pacheco Creek in Santa Clara County, California. Its mouth is located at an elevation of at its confluence with the North Fork Pacheco Creek. Its source is located at on the south flank of Bear Mountain in the Diablo Range in Santa Clara County. The upper part of the creek, at the Valle Atravesado was subsequently flooded when Mississippi Creek, that runs southward through it, was dammed in the 20th century on the valleys south side. It is now a reservoir, originally named Murray Lake, on the upper reach of Mississippi Creek. The lake was originally named after its builder Murray Hopkins who not only built the reservoir, but the 40 miles of County Line Road along the crest of the Diablo Range between San Antonio Valley and Fifield Ranch. Today the reservoir is called Mississippi Lake and the dam Mississippi Dam.Frank F. Latta, JOAQUIN MURRIETA AND HIS HORSE GANGS, Bear State Books, Santa Cruz, California. 1980.
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