Bettowynd Creek
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Bettowynd Creek
Bettowynd Creek, a partly perennial stream of the Moruya River catchment, is located in the Southern Tablelands and South Coast regions of New South Wales, Australia. Course and features Bettowynd Creek rises below Benmanang Range, about south southwest of the village of Majors Creek, on the eastern slopes of the Great Dividing Range. The river flows generally northeast and then southeast before reaching its confluence with the Deua River in remote country south of the Monga National Park. The river descends over its course. See also * Rivers of New South Wales * List of rivers of New South Wales (A-K) 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 nort ... * List of rivers of Australia References External links * Rivers of New South Wales Southern Tablelands
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Australian Aboriginal Languages
The Indigenous languages of Australia number in the hundreds, the precise number being quite uncertain, although there is a range of estimates from a minimum of around 250 (using the technical definition of 'language' as non-mutually intelligible varieties) up to possibly 363. The Indigenous languages of Australia comprise numerous language families and isolates, perhaps as many as 13, spoken by the Indigenous peoples of mainland Australia and a few nearby islands. The relationships between the language families are not clear at present although there are proposals to link some into larger groupings. Despite this uncertainty, the Indigenous Australian languages are collectively covered by the technical term "Australian languages", or the "Australian family". The term can include both Tasmanian languages and the Western Torres Strait language, but the genetic relationship to the mainland Australian languages of the former is unknown, while the latter is Pama–Nyungan, thoug ...
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Deua River
The Deua River, being the main perennial river of the Moruya River catchment, is located in the South Coast region of New South Wales, Australia. Course and features The Deua River rises about southeast of Bendethera Mountain, on the eastern slopes of the Badja Range, part of the Great Dividing Range, within Deua National Park, in rugged and thickly forested ranges south of Braidwood. The river flows generally south, west, north, northeast, south southeast and east, making almost a complete circle, and is joined by fourteen minor tributaries, before becoming the Moruya River near Kiora. The river descends over its course. The lower reaches of the river are estuarine by nature and are called the Moruya River, while the freshwater reaches are called the Deua River. The upper catchment of the Deua River is suspected to be in a rain shadow, so the Deua River is on the whole a small river, and naturally experiences periods of very low flow. Heavy use of groundwater and riverwa ...
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List Of Rivers Of 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 States and territories of Australia, 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 Stream, creek, it has ...
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List Of Rivers Of New South Wales (A-K)
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 north to south roughly parallel to the coast of the Coral and Tasman seas of the South Pacific Ocean. The two main categories of rivers in New South Wales, are those that rise in the Great Dividing Range and flow eastwards to the sea, the Coastal NSW Rivers; and those that rise on the other side of the crest of the range and flow westward, the Inland NSW Rivers. Most of the inland rivers eventually combine into the Murray-Darling network of rivers, which drains to the sea in South Australia. Major rivers The following rivers are the longest river systems, by length. Coastal rivers Due to the relatively close proximity of the Great Dividing Range to the eastern coast of New South Wales, in general, the coastal rivers are short, navigable ...
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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 north to south roughly parallel to the coast of the Coral and Tasman seas of the South Pacific Ocean. The two main categories of rivers in New South Wales, are those that rise in the Great Dividing Range and flow eastwards to the sea, the Coastal NSW Rivers; and those that rise on the other side of the crest of the range and flow westward, the Inland NSW Rivers. Most of the inland rivers eventually combine into the Murray-Darling network of rivers, which drains to the sea in South Australia. Major rivers The following rivers are the longest river systems, by length. Coastal rivers Due to the relatively close proximity of the Great Dividing Range to the eastern coast of New South Wales, in general, the coastal rivers are short, navigabl ...
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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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South Coast (New South Wales)
The South Coast refers to the narrow coastal belt from Shoalhaven district in the north to the border with Victoria in the south in the south-eastern part of the State of New South Wales, Australia. It is bordered to the west by the coastal escarpment of the Southern Tablelands, and is largely covered by a series of national parks, namely Jervis Bay National Park, Eurobodalla National Park, and Beowa National Park. To the east is the coastline of the Pacific Ocean, which is characterised by rolling farmlands, small towns and villages along a rocky coastline, interspersed by numerous beaches and lakes. The South Coast includes Shoalhaven district in the north and the Bega Valley in the more remote south as well as the Eurobodalla Shire and the Commonwealth Jervis Bay Territory which is adjacent to the City of Shoalhaven Local Government Area. Some definitions of the region include the Illawarra, but it is often seen as a separate and distinct region of New South Wales. Climate ...
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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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Moruya River
The Moruya River is an open and trained mature wave dominated barrier estuary or tidal river is located in the South Coast region of New South Wales, Australia. In its upper freshwater reaches, the river is known as the Deua River. Course and features The headwaters of the Deua River rise south of Braidwood and flow to the village of Kiora where the Deua River forms its confluence with the Moruya River. The Moruya River flows generally east, joined by two minor tributaries, past the town of Moruya, before reaching its mouth of the Tasman Sea at Moruya Heads. The river descends over its course. Barrier entrance The river has a bar at its confluence with the Tasman Sea. Work on the river training walls was concentrated in 1907, following extensive siltation of the river opening. The dredge ''Antleon'' was based there during the 1920s, when in 1924, the steamer ''Benandra'' was wrecked at the entrance. Work on the break walls was completed in 1925 when huge storms req ...
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Monga National Park
The Monga National Park is a national park located south west of Sydney, New South Wales, Australia. The closest town nearby is Braidwood. Monga features outstanding high altitude eucalyptus forest and temperate rainforest. It contains the Corn Trail, a historic bridle-track, built in the 1830s, that has been restored and reopened as a walking track. In the park you can find many cultural sites of the ancient Aboriginal peoples of Yuin and Walbunja. The park has an elevation of 686 meters. Gallery Image:Eucryphia moorei & Dicksonia Monga.jpg, Pinkwood growing as a hemiepiphyte on a Soft Tree Fern at ''Monga National Park'' Image:Atherosperma moschatum Monga.jpg, Southern Sassafras at ''Monga National Park''; a seldom seen plant in New South Wales Image:Telopea mongaensis at Monga National Park.jpg, The Monga Waratah at ''Monga National Park'' Image:A stand of ancient trees at Monga National Park.jpg, A stand of Eucalyptus trees at Monga National park See also * Protec ...
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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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