Snowy Mountains Highway
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Snowy Mountains Highway
Snowy Mountains Highway is a state highway located in New South Wales, Australia. Its two sections connect the New South Wales South Coast to the Monaro region, and the Monaro to the South West Slopes via the Snowy Mountains. The higher altitude regions of this road are subject to snow over the winter months, and the road also provides access to many parts of the Snowy Mountains Scheme. The highway bears the B72 shield along its entire length. The highway originally bore the name Monaro Highway until 1958, when it received its current name. It originally ran from to Wagga Wagga but has been shortened to run from Princes Highway to Hume Highway instead. Part of the roadway was reallocated to what is now known as Monaro Highway in 1955. Reservoirs created as a result of dams built in the 1950s and 1960s as part of the Snowy Mountains Scheme required the creation of major realignments to avoid submerged areas. Previous to New South Wales' conversion to alphanumeric route markers ...
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Adelong
Adelong is a small town in the Riverina region of New South Wales, Australia, situated on the banks of the Adelong Creek. Adelong sits on the Snowy Mountains Highway and is a part of the Snowy Valleys Council. At the , Adelong had an urban population of 943. Etymology Adelong's name is said to be derived from the local Aboriginal language meaning "along the way" or "plain with a river". History The area now known as Adelong lies on the traditional lands of the Wiradjuri people. In 1852 during the Australian Gold Rush, gold was discovered at Upper Adelong. Records around the time indicated a yield of 198 kg of precious metals. In 1855 Adelong was declared a gold field. The Adelong township, which was first established in 1836, came alive when in 1857 William Willams discovered a gold bearing reef ore on Charcoal Hill. Alluvial mining and panning along the Adelong Creek was followed by mines being staked in the surrounding hills and water and steam powered stamper batterie ...
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South West Slopes
The South Western Slopes, also known as the South West Slopes, is a region predominantly in New South Wales, Australia. It covers the lower inland slopes of the Great Dividing Range, extending from north of Dunedoo through central NSW and into northeast Victoria, meeting its southwestern end around Beechworth. More than 90% of the region is in the state of New South Wales and it occupies about 10% of that state. Bioregion The South Western Slopes bioregion covers the lower inland slopes of the Great Dividing Range extending from north of Dunedoo through central NSW and into northeast Victoria, meeting its southwestern end around Beechworth. More than 90% of the region is in the state of New South Wales and it occupies about 10% of that state ā€“ more than 80,000 km2.NSW NPWS Map ...
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South East Forest National Park
The South East Forests National Park is a national park located in between the Monaro and South Coast regions of New South Wales, Australia. The national park is situated southwest of Sydney. It features high quality old growth eucalyptus forest and remnant patches of temperate rainforest. History The park was created in 1997 by the amalgamation of Genoa, Tantawangalo, Bemboka, Yowaka and Coolangubra National Parks, all of which had been gazetted in 1994. Genoa National Park in turn was the result of the amalgamation of Nalbaugh and Nungatta National Parks, which had been established in 1972 and 1973 respectively. Until 1968, much of the inland southeastern corner of New South Wales was rugged forest terrain known as the Wallagaraugh Wilderness, and was vacant crown land. At the time, a scientific committee appointed by the New South Wales state government recommended the area of around be protected as a national park, however the Japanese company Harris-Daishowa sought to lo ...
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Escarpment
An escarpment is a steep slope or long cliff that forms as a result of faulting or erosion and separates two relatively level areas having different elevations. The terms ''scarp'' and ''scarp face'' are often used interchangeably with ''escarpment''. Some sources differentiate the two terms, with ''escarpment'' referring to the margin between two landforms, and ''scarp'' referring to a cliff or a steep slope. In this usage an escarpment is a ridge which has a gentle slope on one side and a steep scarp on the other side. More loosely, the term ''scarp'' also describes a zone between a coastal lowland and a continental plateau which shows a marked, abrupt change in elevation caused by coastal erosion at the base of the plateau. Formation and description Scarps are generally formed by one of two processes: either by differential erosion of sedimentary rocks, or by movement of the Earth's crust at a geologic fault. The first process is the more common type: the escarpment is a t ...
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Great Dividing Range
The Great Dividing Range, also known as the East Australian Cordillera or the Eastern Highlands, is a cordillera system in eastern Australia consisting of an expansive collection of mountain ranges, plateaus and rolling hills, that runs roughly parallel to the east coast of Australia and forms the fifth-longest land-based mountain chain in the world, and the longest entirely within a single country. It is mainland Australia's most substantial topographic feature and serves as the definitive watershed for the river systems in eastern Australia, hence the name. The Great Dividing Range stretches more than from Dauan Island in the Torres Strait off the northern tip of Cape York Peninsula, running the entire length of the eastern coastline through Queensland and New South Wales, then turning west across Victoria before finally fading into the Wimmera plains as rolling hills west of the Grampians region. The width of the Range varies from about to over .Shaw, John H., ''Col ...
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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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Nunnock River
The Nunnock River, a perennial stream of the Bega River catchment, is located in the Monaro region of New South Wales, Australia. Course and features The Nunnock River rises below Bull Mountain in the South Coast Range, that is part of the Great Dividing Range, about east of Brown Mountain; and flows generally southeast and northeast before reaching its confluence with the Bemboka River near the locale of Kallarney, adjacent to the Snowy Mountains Highway, approximately west by north of Bemboka. The river descends over its course. See also * List of rivers of Australia * List of rivers of New South Wales (Lā€“Z) * Rivers of New South Wales This page discusses the rivers and hydrography of the state of New South Wales, Australia. The principal topographic feature of New South Wales is the series of low highlands and plateaus called the Great Dividing Range, which extend from nor ... References External links * Rivers of New South Wales {{NewSouthWa ...
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Bemboka
Bemboka is a town in the South Coast region of New South Wales, Australia. The town is located on the Snowy Mountains Highway, in the Bega Valley Shire local government area, south of the state capital, Sydney. At the , the Bemboka gazetted locality had a population of 577. Geography The Aboriginal meaning of the name Bemboka (originally Benbooka) is thought to be "High Peak". Positioned at the eastern head of the Bega Valley, 25 kilometres (15 miles) from the base of Brown Mountain (1241m), a spur of the Great Dividing Range, the locality is bordered by the mountains and ridges of the South East Forests National Park. Prominent features in the Bemboka section to the north include Indian Head, Pigeon Box, Bemboka Peak and Numbugga Walls. History The first inhabitants of the region were a sub-group of the Thaua people of the Yuin nation. The first European settlers were squatters grazing sheep and cattle on crown land beyond the limits of location set by the NSW Government in ...
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Bemboka River
The Bemboka River, a perennial stream of the Bega River catchment, is located in the Monaro and South Coast regions of New South Wales, Australia. Course and features The Bemboka River rises in the Kybeyan Range, that is part of the Great Dividing Range, about east of the village of Nimmitabel; and flows generally south southwest, south southeast, and east southeast, joined by three tributaries including the Nunnock River, before reaching its confluence with the Tantawangalo Creek to form the Bega River at Morans Crossing, adjacent to the Snowy Mountains Highway. The river descends over its course. In its upper reaches, the Bemboka River is impounded by the Cochrane Dam to form the Cochrane Lake. The main purpose of the dam is to supply water for a run-of-the-river hydroelectric power station at the downstream Brown Mountain Power Station, and for irrigation purposes. The Bemboka River was previously the name given to the Bega River. The name Bemboka River now only ...
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T-intersection
A three-way junction (or three-way intersection) is a type of road intersection with three arms. A Y junction (or Y intersection) generally has three arms of equal size coming at an acute or obtuse angle to each other; while a T junction (or T intersection) also has three arms, but one of the arms is generally a smaller road joining a larger road at right angle. Right-of-way Some three-way junctions are controlled by traffic lights, while others rely upon drivers to obey right-of-way rules, which vary from place to place: *In some jurisdictions, chiefly in European countries except the U.K. and Ireland, a driver is always obliged to yield right-of-way for every vehicle oncoming from the right at a junction without traffic signals and priority signs (including T junctions). *In other jurisdictions (mainly in the U.K., USA, Australia and Taiwan), a driver turning in a three-way junction must yield for every vehicle approaching the junction (on the way straight ahead) and, if the ...
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Kiandra
Kiandra is an abandoned gold mining town and the birthplace of Australian skiing. The town is situated in the Snowy Mountains of New South Wales, Australia, in the Snowy Monaro Regional Council inside the Kosciuszko National Park. Its name is a corruption of Aboriginal 'Gianderra' for 'sharp stones for knives'. It was earlier called Gibson's Plains, named after a Dr. Gibson, a settler in the district in 1839. For a century (until the establishment of Cabramurra), Kiandra was Australia's highest town. Kiandra lies approximately north-west of Cooma on the Snowy Mountains Highway between Adaminaby and Talbingo. It sits at above sea level and is situated on a high, treeless ridge on the banks of the Eucumbene River, which is snow-covered during winter and is subject to high winds. It lies in the Australian Alps montane grasslands bioregion according to Interim Biogeographic Regionalisation for Australia. After decades of decline, restoration work on the remaining buildin ...
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Yarrangobilly Caves
The Yarrangobilly Caves are located in a karst region along the Yarrangobilly River valley in the north of Kosciuszko National Park, New South Wales, Australia. Discovered to British colonists by a cattleman, the Yarrangobilly Caves system includes several independent limestone caves formed over different time periods, from several million to a few hundred thousand years old. The older examples are in higher strata and have more speleothem decoration. The caves are administered by the National Parks and Wildlife Service. Three lit show caves are regularly open to visitors, two for guided tours and the third for a self-guided tour. The caves complex also includes a and up to thermal pool, fed by natural warm-water springs, and a number of walking tracks. History The cave was formed in 440-million-year-old limestone, and was first discovered by Europeans in 1834 when a stockman John Bowman came across the complex. Leo James Hoad was associated with the caves from 1904ā€“ ...
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