Clyde River, New South Wales
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Clyde River, New South Wales
The Clyde River ( Dhurga: ''Bhundoo'') is an open intermediate tide dominated drowned valley estuary, or perennial river that flows into the Tasman Sea at Batemans Bay, located in the South Coast region of New South Wales, Australia. Course and features The Clyde River rises below Kangaroo Hill in the Budawang Range, part of the Great Dividing Range, within Budawang National Park, south of the locality of Sassafras, and flows generally southwards parallel to the east coast, joined by nine tributaries including the Bimberamala, Yadboro, and Buckenbowra rivers, before turning east and reaching its mouth of the Tasman Sea at Batemans Bay. The river descends over its course. The lower reaches of the Clyde River form a substantial estuary up to from its mouth which is navigable by small vessels to Nelligen, with a tidal ebb of up to . The coastal estuary covers a catchment area of and contains approximately of water over an estimated surface area of ; and at an average de ...
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River Clyde
The River Clyde ( gd, Abhainn Chluaidh, , sco, Clyde Watter, or ) is a river that flows into the Firth of Clyde in Scotland. It is the ninth-longest river in the United Kingdom, and the third-longest in Scotland. It runs through the major city of Glasgow. Historically, it was important to the British Empire because of its role in shipbuilding and trade. To the Romans, it was , and in the early medieval Cumbric language, it was known as or . It was central to the Kingdom of Strathclyde (). Etymology The exact etymology of the river's name is unclear, though it is known that the name is ancient: It was called or by the Britons and by the Romans. It is therefore likely that the name comes from a Celtic language—most likely Old British. But there is more than one old Celtic word that the river's name could plausibly derive from. One possible root is the Common Brittonic , meaning 'loud' or 'loudly'. More likely, the river was named after a local Celtic goddess, '' Clōta ...
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Bimberamala River
Bimberamala River, a perennial river of the Clyde River catchment, is located in the Southern Tablelands and the upper ranges of the South Coast regions of New South Wales, Australia. Course and features Bimberamala River rises below Mount Budawang, on the eastern slopes of the Budawang Range, part of the Great Dividing Range and within Budawang National Park. The river generally flows northeast, then south, then east northeast, and finally north northeast, through Bimberamala National Park and Yadbro State Forest, joined by one minor tributary, before reaching its confluence with the Clyde River, north of the village of Brooman. The river descends over its course. See also * Rivers of New South Wales * List of rivers of New South Wales (A–K) * 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 ...
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Batemans Bay Bridge Post Construction Northern Foreshore July 2022
Bateman's is a 17th-century house located in Burwash, East Sussex, England. It was the home of Rudyard Kipling from 1902 until his death in 1936. The house was built in 1634. Kipling's widow Caroline bequeathed the house to the National Trust on her death in 1939. The house is a Grade I listed building. History Bateman's is a Jacobean Wealden mansion constructed in 1634. There is debate as to the original builder. Historic England follows the tradition favoured by Kipling of ascribing the construction to a Sussex ironmaster, John Britten. The historian Adam Nicolson reports the tradition in the National Trust's guidebook, but notes that Britten was a dealer in iron, rather than a manufacturer. Pevsner attributes the construction to a lawyer, William Langham. By the early twentieth century, the house had descended to the status of a farmhouse, and was in a poor state of repair. The Kiplings first saw it in 1900, on returning to England from America, following the death of the ...
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Clyde River National Park
Clyde River is a national park in south-eastern New South Wales (Australia) between Batemans Bay and Nelligen. It includes 9 km of river frontage to the Clyde River, bounded on three sides by the Clyde River and on the northeast by the Kings Highway. It was created from a part of Benandarah State Forest; in 2000 10.91 km2 of the state forest was set aside as a national park. The park forms part of the Ulladulla to Merimbula Important Bird Area, identified as such by BirdLife International because of its importance for swift parrots. This national park is a natural playground, where you can go fishing, kayaking, canoeing, swimming and at the same time enjoy the beautiful landscape. Primarily, this is the land of the Walbunja people, the Clyde River has been an inexhaustible source of food for them for thousands of years. See also * Protected areas of New South Wales The Protected areas of New South Wales include both terrestrial and marine protected areas. ...
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Nelligen, New South Wales
Nelligen is a village on the Clyde River on the South Coast of New South Wales, Australia. It is located on the Kings Highway. Location and services The village is situated on the river's western bank near a junction with Nelligen Creek, and inland from Batemans Bay. Local services include a general store, hotel, and general cemetery. History The original inhabitants of the land were Aborigines of the Walbanga, Murrinjari and Bergalia clans. The origin of the name is unclear and was already in use at the time of the first survey in 1828. The surveyor Robert Hoddle described the site of the future township as of "good forest land at Nellican Creek" and by the 1830s timber cutters had cleared a site for settlement and work had begun on a road to Batemans Bay. The village of Nelligen was gazetted in 1854 and a road inland to Braidwood was completed two years later. No bridges existed across the Clyde at the time, so produce and minerals from southern New South Wales ...
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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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River Mouth
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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Sassafras, New South Wales
Sassafras is a locality in the City of Shoalhaven in New South Wales, Australia. It lies on the Braidwood Road (which was originally built as the Wool Road), where it passes over the coastal escarpment on the road between Nowra and Nerriga. This road continues southwest to Braidwood, but this involves a section of unsealed road. The sealed Oallen Ford Road branches off south of Nerriga, which connects via various sealed roads to Canberra and Goulburn Goulburn ( ) is a regional city in the Southern Tablelands of the Australian state of New South Wales, approximately south-west of Sydney, and north-east of Canberra. It was proclaimed as Australia's first inland city through letters pate .... Sassafras is a small community of orchards in an area of extensive national parks. At the , it had a population of 31. References Further reading * City of Shoalhaven Localities in New South Wales {{SouthCoastNSW-geo-stub ...
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Budawang Range
The Budawang Range, commonly called The Budawangs, a rugged mountain range within the Budawang National Park and the Morton National Park, are part of a spur off the Great Dividing Range and are located in the South Coast region of New South Wales, Australia. The highest mountain in the range is Mount Budawang that has an elevation of above sea level. Location and features Commmencing between the headwaters of the Clyde and Endrick rivers, The Budawangs extend in a generally south southwest direction for about to Mount Budawang about southeast of . The range consists of mountains and escarpments, generally at an elevation of , forming most of the western watershed of the Clyde River. The range comprises a series of hills extending generally west northwest from the north end of Budawang Range near Sassafras for about to above the junction of the Shoalhaven and Endrick rivers. The Pigeon House Range forms the watershed between the northeast waters of Endrick River and those ...
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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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Tide
Tides are the rise and fall of sea levels caused by the combined effects of the gravity, gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables can be used for any given locale to find the predicted times and amplitude (or "tidal range"). The predictions are influenced by many factors including the alignment of the Sun and Moon, the #Phase and amplitude, phase and amplitude of the tide (pattern of tides in the deep ocean), the amphidromic systems of the oceans, and the shape of the coastline and near-shore bathymetry (see ''#Timing, Timing''). They are however only predictions, the actual time and height of the tide is affected by wind and atmospheric pressure. Many shorelines experience semi-diurnal tides—two nearly equal high and low tides each day. Other locations have a diurnal cycle, diurnal tide—one high and low tide each day. A "mixed tide"—two uneven magnitude ...
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