query: where does the murray river enter the ocean

pos: Murray River Murray River The Murray River (or River Murray) (Ngarrindjeri: "Millewa", Yorta Yorta: "Tongala") is Australia's longest river, at in length. The Murray rises in the Australian Alps, draining the western side of Australia's highest mountains, and then meanders across Australia's inland plains, forming the border between the states of New South Wales and Victoria as it flows to the northwest into South Australia. It turns south at Morgan for its final , reaching the ocean at Lake Alexandrina. The water of the Murray flows through several terminal lakes that fluctuate in salinity (and were often fresh until recent decades) including

pos: Murray River Lake Alexandrina and The Coorong before emptying through the Murray Mouth into the southeastern portion of the Indian Ocean, often referenced on Australian maps as the Southern Ocean, near Goolwa. Despite discharging considerable volumes of water at times, particularly before the advent of largescale river regulation, the mouth has always been comparatively small and shallow. As of 2010, the Murray River system receives 58 percent of its natural flow. It is perhaps Australia's most important irrigated region, and it is widely known as the food bowl of the nation. The Murray River forms part of the long combined Murray–Darling river

pos: European land exploration of Australia discovered—the Darling, Macquarie, Murray and Murrumbidgee rivers—all of which flowed west, a theory was developed of a vast inland sea into which these rivers flowed. Another reason behind the idea of an inland sea was that Matthew Flinders, who had very carefully mapped much of Australia's coast had discovered no great river delta where these rivers should have emerged by had they reached the coast. The Murray-Darling basin actually drains into Lake Alexandrina. Matthew Flinders had noted this on his maps but viewed from the sea does not look like the outfall of a large watershed, but instead as a

pos: Wellington East, South Australia Wellington East, South Australia Wellington East (also historically known as East Wellington or part of Wellington) is a locality in the Murray Mallee on the east (left bank) of the Murray River in South Australia where the river opens into Lake Alexandrina, the largest of the lakes at the end of the Murray-Darling system. Wellington East is the eastern end of the Wellington Ferry, the furthest downstream crossing of the Murray River on Route B45. It is mostly low-lying land and development is predominantly shacks and holiday homes associated with the river and lagoons. The eastern boundary is the Princes

pos: Wellington East, South Australia Highway between Tailem Bend and Meningie. Wellington East, South Australia Wellington East (also historically known as East Wellington or part of Wellington) is a locality in the Murray Mallee on the east (left bank) of the Murray River in South Australia where the river opens into Lake Alexandrina, the largest of the lakes at the end of the Murray-Darling system. Wellington East is the eastern end of the Wellington Ferry, the furthest downstream crossing of the Murray River on Route B45. It is mostly low-lying land and development is predominantly shacks and holiday homes associated with the river and lagoons.

pos: History of New South Wales expedition in 1829, Sturt followed the Murrumbidgee River into a 'broad and noble river', the Murray River, which he named after Sir George Murray, secretary of state for the colonies. His party then followed this river to its junction with the Darling River, facing two threatening encounters with local Aboriginal people along the way. Sturt continued down river on to Lake Alexandrina, where the Murray meets the sea in what is now South Australia. Suffering greatly, the party had to then row back upstream hundreds of kilometers for the return journey. Surveyor General Sir Thomas Mitchell conducted a series of

pos: Diane Bell Greens on 21.4 (+10.4) percent and the Liberals on 41.3 (–9.8) percent. The seat became marginal for the Liberals on a 53.0 (–4.0) two-candidate vote. Bell campaigned for fresh water flows for the River Murray, Lakes Alexandrina and Albert and the Coorong. In 2007, she was a co-founder of the 'StoptheWeir' website and worked with the River, Lakes and Coorong Action Group Inc to stop the construction of a weir across the River Murray at Pomanda Island (at the point where the river enters Lake Alexandrina). She administered the "Hurry Save The Murray" website and has been a frequent speaker

pos: Lake Alexandrina (South Australia) end. Loveday Bay is an inlet located at the south-east of Lake Alexandrina, adjacent to Tauwitchere Channel. The lake empties into the sea via a channel known as the Murray Mouth south-east of the town of Goolwa, however when the river flow is low the mouth is often blocked by a sand-bar. Originally subjected to tidal and storm inflows of seawater, the lake is now maintained as fresh water by a series of barrages known as the Goolwa Barrages which cross five channels between the mainland and three islands near the Murray Mouth. Though connected to the ocean historically the

neg: Hindmarsh Island a dried up salt lake, that does become full of water in winter. Area: 1 Perimeter: Hindmarsh Island Weather Receiver (35°31'10.20"S 138°49'4.17"E) is a weather receiver located next to the Hindmarsh Island Marina. It provides the Bureau of Meteorology with Hindmarsh Islands weather. Surrounded by a steel fence, it is out of bounds to the general public. The weather receiver was built in 2006. Height: Hindmarsh Island River Murray Mouth Lookout (35°32'58.23"S 138°52'58.03"E) is a lookout on the south-west area of the Island. An observation of the Murray Mouth; where the river meets the ocean. Area: Perimeter: Lake Cloud (35°31'12.51"S

neg: Murray River (Western Australia) shore where the Murray River enters the estuary. The group then exited through the ocean bar and sailed south along the coast as far as the Collie and Preston Rivers and the Leschenault Inlet before returning to the Peel-Harvey estuary on 28 November 1829. From there they explored the Murray River delta, which at the time included five entrances into the estuary. The boats managed to navigate about up the river before returning to Fremantle after the 12-day trip. This was the first actual encounter with the Murray River and it was named by Governor James Stirling after the Secretary

neg: Jordan River (Utah) and Murray and South Salt Lake on the east. The river flows underneath Interstate 215 in Murray. Little and Big Cottonwood Creeks enter from the east in Murray, and from the mouth respectively. Mill Creek enters on the east in South Salt Lake, from the mouth. The river runs through the middle of Salt Lake City, where the river travels underneath Interstate 80 a mile west of downtown of Salt Lake City and again underneath Interstate 215 in the northern portion of Salt Lake City. Interstate 15 parallels the river's eastern flank throughout Salt Lake County. At from the mouth,

neg: Avoca River , and . Although the Avoca River basin is part of the Murray-Darling basin, the Avoca River does not empty into the Murray. Nowhere a large stream, it dwindles as it flows north, eventually terminating in the Kerang Lakes, a network of ephemeral swamps west of Kerang and about south of the Murray River. Although the Avoca River has a substantial catchment area, the fifth largest in Victoria, most of that area is on the northern plains where rainfall averages only about per year, and where there is little runoff as the terrain is very flat. The mean annual runnoff

neg: Murray River (Western Australia) of the Murray and for some time was confused with the Murray, which was not encountered until later that year. In November, Dr Alexander Collie and Lieutenant William Preston and crew from piloted two whaleboats out of Cockburn Sound and at midday on 17 November 1829 crossed the ocean bar at present day Mandurah. After camping overnight, they sailed south down the Peel-Harvey Estuary to the southern extreme near the delta of the Harvey River, where they had an amicable encounter with some local aborigines. Due to strong winds, they sailed north out of the estuary without exploring the Eastern

neg: Murray Taylorsville MAX the route which have a single stop, this "stop" will have separate stops for each direction of travel. After reaching West 4800 South it will turn east along that road to cross over the Jordan River and the Jordan River Parkway Trail. Upon crossing over the Jordan River Parkway Trail, the Murray Taylorsville MAX will leave Taylorsville and enter Murray. Continuing east along West 4800 South it will immediately cross over the Jordan River Parkway Trail and then the intersection with Murray Boulevard/Riverside Drive at about 500 West. It will then turn south on Murray Boulevard and, after crossing over

neg: Murray Mouth Murray Mouth Murray Mouth is the point at which the River Murray meets the Southern Ocean. The Murray Mouth's location is changeable. Historical records show that the channel out to sea moves along the sand dunes over time. At times of greater river flow and rough seas, the two bodies of water would erode the sand dunes to create a new channel leaving the old one to silt and disappear. The mouth of the Murray River is located about south east of Goolwa and about south south-east of the Adelaide city centre in the gazetted localities of Coorong and Goolwa

neg: Clayton Bay the Lachlan River on the 7 January 1830. The crew, besides Sturt and Macleay were Harris, Hopkinson, and Frasier (soldiers), and Mulholland, Macnamee, and Clayton (convicts). Around the 9th of February 1830, Captain Charles Sturt sighted seagulls. Aboriginals told them that the ocean was nearby and so they sailed into a lake which Sturt named Alexandrina. A few days later, they found the point where the Murray flowed into the sea. The town of Clayton was named by Governor MacDonnell in 1858 and is located on the Lower Murray River. Blocks were first offered for sale in 1859. These were

neg: Portland Gale end. The area surrounding and including Fourth Cliff is called Humarock. Prior to the Portland Gale, the North River flowed south between Fourth Cliff and Marshfield, Massachusetts, joining the South River and entering the ocean two kilometers to the south of the current opening. A thin strip of beach, which connected Third Cliff to Fourth Cliff, was breached by the storm, leaving Fourth Cliff an island. Eventually the old inlet has silted in, forcing the South River to flow north between Marshfield and Fourth Cliff, where it now joins the North River to enter the ocean between Third and Fourth

neg: Killary Harbour does not take full account of the underwater sides of the valley, and the shape of its bed. The matter was considered in a dedicated peer-reviewed paper, "An Oceanographical Survey of Killary Harbour...," that concluded that Killary was a fjord. The landform was shaped by a massive glacier, carving its way from the land to the Atlantic Ocean. The Erriff River flows into the head of the inlet, and multiple smaller rivers and streams enter along its length. These include the Bunanakee River flowing across Uggool Beach near the mouth, the Bundorragha River (with tributaries including the Owennaglogh, Sruhaunboy, Owengar

neg: Coquille River (Oregon) a time lag between the high tide at sea and the effect pushing upstream. This varies according to the number of miles from the ocean. The tidal-effect is observed as far as Myrtle Point, some upriver. The head of tide is upriver from the mouth at Bandon. But some salt water does enter across the bar. The salt water intrusion was once minor. Today, however, sometimes traces of salinity appear only a few miles below the town of Coquille. This phenomenon affects industry along the river, as mills and other sites need fresh water intakes on the river in order

neg: River mouth sand bars, spits, and tie channels. Many places in England take their names from their positions at the mouths of rivers, such as Plymouth (River Plym), Sidmouth (River Sid), and Great Yarmouth (River Yare). River mouth A river mouth is the part of a river where the river flows into another river, a lake, a reservoir, a sea, or an ocean. 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

neg: River mouth River mouth A river mouth is the part of a river where the river flows into another river, a lake, a reservoir, a sea, or an ocean. 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

neg: Seal culling in South Australia Reef with a gun or a dog, or to take seals on any of the islands or reefs within St. Vincent or Spencer Gulf north of a line from Cape Catastrophe to Cape Borda, continued to Cape Hart at the south-eastern corner of Kangaroo Island, thence to the mouth of the River Murray." Seals were known to enter inland river systems and were seen as far up the Murray-Darling system as Deniliquin, 1,000 miles from the mouth of the Murray. A hotel at Conargo once displayed the skin of a seal shot in the river nearby. Other accounts of inland

neg: Water Witch (1835 cutter) Water Witch (1835 cutter) Water Witch was a single-masted vessel rigged as a cutter built during 1835 in Van Diemen's Land and sunk in 1842 whilst moored in the River Murray at Moorundie, south of Blanchetown in South Australia (SA). Her wreck site was discovered in 1982 and received statutory protection as a historic shipwreck in 1983. The wreck site was the subject of an underwater survey in March 1984. She is notable for being the first European vessel to enter the River Murray via its mouth, her role in the charting of the lower reaches of the River Murray

neg: Big Bend, South Australia Big Bend, South Australia Big Bend in South Australia is the longest single bend in the Murray River. The area is known for its spectacular riverside cliffs, which are the tallest along the Murray River. The limestone cliffs are rich with millions of ocean fossils and are home to colonies of bats. Caves in the area have been continuously occupied for at least 8,000 years and are sacred to the local aboriginal community. There is a collection of holiday shacks located on the banks. The gazetted locality of Big Bend is on the left bank of the Murray River, upstream

neg: Murray River (Western Australia) had been granted to established settlers. Peel was offered an alternative grant from Woodman Point to the north bank of the Murray River and from the ocean to the Darling Scarp. Peel's remaining settlers arrived shortly after and settled initially at Clarence before moving to the site of present-day Mandurah, which he named "Peeltown". Despite many problems faced by the settlers, the area was gradually expanded and a settlement at Pinjarra had been established by late 1830. Pinjarra was approximately the upper limit of navigable water along the Murray River. It also had a natural ford for travellers at nearby

neg: Great Dividing Range Great Dividing Range creates the drainage basins of the Australian south-east coast drainage division and the Australian north-east coast drainage division, whose water flows to the east coast and into the Pacific Ocean, Tasman Sea, and Bass Strait with the westerly Murray–Darling basin which flow inland, away from the coast into the interior plains. Some of the rivers which flow west of the ranges includes the Condamine River, Flinders River, Herbert River, Lachlan River, Macdonald River, Macintyre River and Namoi River. Rivers that flow north into the Murray–Darling Basin from Victoria include the Goulburn, Mitta Mitta, Kiewa, Ovens, King, Loddon

neg: Delaware River Delaware River The Delaware River is a major river on the Atlantic coast of the United States. It drains an area of in five U.S. states: Delaware, Maryland, New Jersey, New York, Pennsylvania. Rising in two branches in New York state's Catskill Mountains, the river flows into Delaware Bay where its waters enter the Atlantic Ocean near Cape May in New Jersey and Cape Henlopen in Delaware. Not including Delaware Bay, the river's length including its two branches is . The Delaware River is one of nineteen "Great Waters" recognized by the America's Great Waters Coalition. The Delaware River rises

neg: Mudrock most abundant source of mudrocks, behind marine mudrocks. Ancient lakes owe their abundance of mudrocks to their long lives and thick deposits. These deposits were susceptible to changes in oxygen and rainfall, and offer a robust account of paleoclimate consistency. A delta is a subaerial or subaqueous deposit formed where rivers or streams deposit sediment into a water body. Deltas, such as the Mississippi and Congo, have massive potential for sediment deposit, and can move sediments into deep ocean waters. Delta environments are found at the mouth of a river, where its waters slow as they enter the ocean, and

neg: Delaware River designating sixteen rivers as endangered habitat for the Atlantic Sturgeon which would require more attention to be given to uses of the rivers that affect the fish. The river is part of the National Wild and Scenic Rivers System. Delaware River The Delaware River is a major river on the Atlantic coast of the United States. It drains an area of in five U.S. states: Delaware, Maryland, New Jersey, New York, Pennsylvania. Rising in two branches in New York state's Catskill Mountains, the river flows into Delaware Bay where its waters enter the Atlantic Ocean near Cape May in New

neg: Tributary 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. A confluence, where two or more bodies of water meet together, 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

neg: Murray Mouth located within a special purpose area within the Encounter Marine Park and is immediately adjoined on its northern and eastern sides by the boundary of the Coorong National Park. The Murray mouth is adjoined on its northern and eastern sides by the boundary of the Coorong Important Bird Area which is an area considered by Birdlife International to be a place of ‘international significance for the conservation of birds and other biodiversity.’ Murray Mouth Murray Mouth is the point at which the River Murray meets the Southern Ocean. The Murray Mouth's location is changeable. Historical records show that the channel

neg: Steamboats of the Coquille River Steamboats of the Coquille River The Coquille River starts in the Siskiyou National Forest and flows hundreds of miles through the Coquille Valley on its way to the Pacific Ocean. Bandon, Oregon, sits at the mouth of the Coquille River on the Pacific Ocean. Before the era of railroads and later, automobiles, the steamboats on the Coquille River were the major mode of transportation from Bandon to Coquille and Myrtle Point in southern Coos County, Oregon, United States. Jetty construction at the two jetties at the Coquille River entrance allowed ocean-going ships to enter the mouth of the river and

neg: Doce River near Governador Valadares, and flows in a southeastern direction passing through Conselheiro Pena, to enter the Atlantic Ocean near Linhares in Espírito Santo state. Its main tributaries are the Piracicaba, Casca, Matipó, Caratinga-Cuieté, Manhuaçu, Santo Antônio and Suaçuí Grande, in Minas Gerais; the Pancas, Guandu, and São José, in Espírito Santo. Part of the river basin is contained in the Augusto Ruschi Biological Reserve, a fully protected area. South of the point where the Piracicaba enters the river near Ipatinga the river forms the eastern boundary of the Rio Doce State Park. The Doce river has great economic importance for

neg: North River (Massachusetts Bay) forcing the South River to flow north between Marshfield and Humarock, where it now joins the North River to enter the ocean between Third and Fourth Cliffs. Although Humarock is now connected by land to Marshfield, North of Rexhame Beach, there are no roads across the old inlet. As a result, Humarock is only accessible via the Marshfield Avenue and Julian Street bridges from Marshfield. The change to the course of the North River also increased the salinity of the large marsh area surrounding the current outlet, resulting in the loss of the valuable salt haying business. North River (Massachusetts

neg: Coos River within Oregon. The river enters the bay about from where the bay—curving east, north, and west of the cities of Coos Bay and North Bend and passing by the communities of Barview and Charleston—meets the ocean. About 30 other tributaries also enter the bay directly. Most of the Coos River watershed of is in Coos County, but are in eastern Douglas County. Commercial forests cover about 85 percent of the basin. The river supports populations of chinook and coho salmon, shad, steelhead, and coastal cutthroat trout. Since public river-bank access is limited, fishing is often done by boat. Flowing west

neg: Murray River states of Victoria and New South Wales. Where it does, the border is the top of the bank of the Victorian side of the river (i.e., none of the river itself is actually in Victoria). This was determined in a 1980 ruling by the High Court of Australia, which settled the question as to which state had jurisdiction in the unlawful death of a man who was fishing by the river's edge on the Victorian side of the river. This boundary definition can be ambiguous, since the river changes its course over time, and some of the river banks have

neg: Murray River Queen Murray River Queen Murray River Queen is an Australian paddle ship built at Hindmarsh Island in 1974 as a luxury passenger cruise boat. She was a tourist boat carrying passengers on the Murray River in South Australia. For many years, her home port was Goolwa where she offered week-long cruises operated by her builders, the Veenstra family. She was the first of several large boats built by the Veenstras for the Murray River, they later also built the M.V. Murray Explorer and PS Murray Princess. Murray River Queen retired from regular service in 1993, and spent ten years initially as

neg: Lacustuary less saline, as lacustuaries are freshwater bodies. Additionally lacustuaries tend to be less saline the closer to the lake, where as estuaries are more saline the closer to the ocean. Lacustuaries, where river and lake waters meet and mix, have different functions than estuaries. Their physical and biological characteristics are also much different from the free-flowing water further upstream, and they play important roles in the ecology of both lake and river ecosystems. Lacustuary vegetation is also markedly different from shoreline and upland habitats. Not all streams which enter a lake have a lacustuary. Man-made ship channels may also be

neg: Trout cod projects it is important that Murray cod are not stocked into sites where Trout Cod and Murray cod are not already coexisting sympatrically. Trout cod were once common and abundant throughout the Murray-Darling Basin but are now listed on the IUCN as endangered due to overfishing, degradation of habitat and the introduction of invasive Trout species. The species is now totally protected. Only one wild, naturally occurring trout cod population remains in the Murray River in a region where the river is basically an extended transition zone from upland river habitat to lowland river habitat. In more lowland river habitats,

neg: Humarock and Marshfield, joined the South River, and entered Massachusetts Bay two kilometers to the south of the current opening. A thin strip of beach which connected Third Cliff to Fourth Cliff was breached by the storm surge of the Portland Gale of 1898, separating Humarock from the rest of Scituate. Eventually the old inlet silted in, forcing the South River to flow north between Marshfield and Fourth Cliff where it now joins the North River to enter the ocean. Although Humarock is now connected by land to the Rexhame section of Marshfield, there are no roads across the old inlet.

neg: Victor Harbor railway line Victor Harbor railway line The Victor Harbor railway line is a broad gauge line in South Australia. It branches from the Adelaide to Wolseley line at Mount Barker Junction and then runs south to Victor Harbor. South Australia's first railway venture was the opening of the Goolwa on the Murray River to the ocean harbour at Port Elliot horse tramway in 1854. It was later extended to a safer harbour at Victor Harbor. This line was used to move freight between the shallow-draft vessels navigating the Murray, and coastal and ocean-going vessels, without either having to traverse the narrow and

neg: Murray River Edward River which exists today and through which much of the Murray River's waters still flow. Then the natural dam on the Goulburn River failed, the lake drained, and the Murray River avulsed to the south and started to flow through the smaller Goulburn River channel, creating "The Barmah Choke" and "The Narrows" (where the river channel is unusually narrow), before entering into the proper Murray River channel again. This complex series of events, however, diverts attention from the primary result of the Cadell Fault — that the west-flowing water of the Murray River strikes the north-south fault and diverts

neg: Lake Mulwala replaced an earlier wooden bridge built in 1889-1891. The bridge was started from both ends, each by the respective state government. Unfortunately, they didn't coordinate their efforts, and the bridge has a dip and a bend in the middle to make the two ends meet. The Yarrawonga weir is the farthest downstream obstruction across the Murray that does not have a navigation lock through it. When full, the lake is above sea level. The weir is upriver from the river mouth. Lake Mulwala is a renowned fishery for the native Murray Cod and is one of the few places where

neg: Murray River been modified. West of the line of longitude 141°E, the river continues as the border between Victoria and South Australia for approximately , where this is the only stretch where a state border runs down the middle of the river. This was due to a miscalculation during the 1840s, when the border was originally surveyed. Past this point, the Murray River is entirely within the state of South Australia. The following major settlements are located along the course of the river, with population figures from the 2011 Census: The Murray River (and associated tributaries) support a variety of river life

neg: Wakool River Wakool River Wakool River, an anabranch of the Edward River that is part of the Murray River catchment within the Murray-Darling basin, is located in the western Riverina region of south western New South Wales, Australia. The Wakool River splits from the Edward River (itself an anabranch of the Murray) near Deniliquin, and flows generally to the west, southwest, northwest, and then west, joined by eleven minor tributaries, including the Niemur River. The Wakool is rejoined by the Edward River near Kyalite, not far from where it runs back into the main channel of the Murray, at Wakool Junction; dropping

neg: Murray, Utah zones. City policies are in place to minimize the potential impacts on structures. The Jordan River is the largest water feature within Murray. It traverses the western edge of Murray, where it eventually reaches the Great Salt Lake. Murray administers a trail and green area that borders the river through the whole city. Big Cottonwood and Little Cottonwood Creeks join the Jordan River within Murray City boundaries, following routes between properties, along streets, and through parks and open spaces. Significant wetlands adjoin the river and these two creeks. Murray contains only small lakes. Willow Pond and Turner Pond are the

neg: Riverland (introduced to Renmark), Bush Stone Curlews and Carpet Pythons (rated 'vulnerable' to extinction in the region). Riverlanders share an interest in the health of the River Murray. The Riverland region lies in the southern part of the Murray Darling Basin where the broad River Murray floodplain and its river meanders for approximately through red sandy Mallee dune landscapes. Several conservation reserves protect biodiversity and provide for conservation and wise use activities. Protected area associated with the River Murray include Murray River National Park, Loch Luna Game Reserve and Moorook Game Reserve. Mallee landscape reserves include Chowilla Regional Reserve, Billiatt Conservation

neg: Bidyanus bidyanus and close to 8 kg, but today wild river specimens are typically 30–40 cm and 1.0–1.5 kg. The silver perch is the only major representative of the family Terapontidae in the southern Murray-Darling system, compared to northern tropical systems where terapontid species are common. Another small terapontid, the spangled perch ("Leiopotherapon unicolor"), does occur sporadically in the northern Murray-Darling Basin. The silver perch is a large grunter with a small head, small eyes, a small mouth at the end of a pointed 'beak-like' snout. The species is streamlined and laterally compressed, with a spiny dorsal fin of medium height, angular

neg: Short-finned eel northern New South Wales. Unable to scale the Great Divide, and not extending as far west as the outlet of the Murray River, they are excluded from the thousands of miles of waterways that drain inland eastern Australia. "A. Australis" is the most widely distributed longitudinally of the Anguillid eels where its larvae can be found just south of Fiji to the North-west of Australia in the SEC region (14.5-21°S, 154-179.5°E) (For a comparison with northern hemisphere eels, in particular the European eel, see eel life history.) The larvae drift on the ocean currents and eventually reach coastal waters, where

neg: Murray River and Darling rivers, compiling a list of birds and mammals. The lack of an estuary means that shipping cannot enter the Murray from the sea. However, in the 19th century the river supported a substantial commercial trade using shallow-draft paddle steamers, the first trips being made by two boats from South Australia on the spring flood of 1853. The "Lady Augusta", captained by Francis Cadell, reached Swan Hill while another, "Mary Ann", captained by William Randell, made it as far as Moama (near Echuca). In 1855 a steamer carrying gold-mining supplies reached Albury but Echuca was the usual turn-around point

neg: Aneto and flow underground to the east where they resurface to empty into the Aran Valley and the Garonne river, flowing north into France and the Atlantic Ocean. The waters of the western and southern sides, flow into the Coronas and Llosas lakes respectively before draining separately into the river Ballibierna, which flows into the Esera, then the Cinca before joining the Ebro and flowing to the Mediterranean. Thus although Aneto does not lie on the main ridge of the Pyrenees, it does lie on the watershed between the Atlantic and the Mediterranean. This agglomeration of summits, all markedly Alpine, is

neg: South West African Zwillinge River gorge, the gradient was 1 in 19 (5¼%) with curves of . In 1905, a branch line was constructed from Karibib on the "Nordbahn" to Onguati near Usakos, where it connected with the new Otavi line from Swakopmund to Tsumeb. This created an alternative line from Windhoek to the Atlantic Ocean at times when the section through the Khan River gorge suffered from the occasional flooding. The "Nordbahn" section between Swakopmund and Karibib was later abandoned and, between 1911 and 1913, the section between Karibib and Windhoek was regauged to Cape gauge. "Zwillinge" locomotives, the first engines to enter

neg: Surf break disappear or change with storms. The 'Outer Banks' in North Carolina is an example. They can also be made of more permanent rocky reefs. Numerous tidal bore waves are known, some of which have also been surfed for several kilometres or more and many kilometres from the ocean, making them the longest rideable waves in the world. They are formed where stronger and larger tides enter a river or deltaic system, allowing the tide to forcefully push and extend up the river, sometimes forming rideable waves. The waves can be singular or multiple crested. They form at specific times of

neg: Big Bend, South Australia straight section, continues the right turn through another 90 degrees before the left turn round Ngaut Ngaut Conservation Park. Big Bend, South Australia Big Bend in South Australia is the longest single bend in the Murray River. The area is known for its spectacular riverside cliffs, which are the tallest along the Murray River. The limestone cliffs are rich with millions of ocean fossils and are home to colonies of bats. Caves in the area have been continuously occupied for at least 8,000 years and are sacred to the local aboriginal community. There is a collection of holiday shacks located

neg: Rail transport in South Australia It was later extended to a safer harbour at Victor Harbor. This line was used to move freight between the shallow-draft vessels navigating the Murray, and coastal and ocean-going vessels, without either having to traverse the narrow and shallow mouth of the river with unpredictable currents. The first of the Railways in Adelaide was built in 1856 between the city and the port. The Adelaide railways were all built as broad gauge of . Gradually, a network of lines spread out from Adelaide. These were initially built to carry ore, particularly copper, then later freight from the Murray River, and

neg: Rail transport in South Australia the Murray, and coastal and ocean-going vessels, without either having to traverse the narrow and shallow mouth of the river with unpredictable currents. It was later extended from Port Elliot to Victor Harbor in 1864 and from Goolwa to Strathalbyn in 1869. It was extended to Mount Barker Junction on the South Line in 1884 and strengthened to carry steam trains. A branch from the South Line between the Mount Lofty Ranges and Murray River was built to Monarto and Cambrai in 1886. It was shortened to Apamurra near Palmer before being closed due to the standardisation of the Adelaide

neg: Murray Grey cattle books. In Paraguay Murray Grey cattle have been used in crossbreeding programs involving Zebu and Charolais cattle. The Zebu and Charolais cattle there lacked the dark skins and early maturing traits of the Murray Greys. This crossbreeding program improved the fertility, calving ease and weight gains of the progeny produced there. Murray Grey cattle Murray Grey is a breed of Australian polled beef cattle that was developed in the upper Murray River valley on the New South Wales /Victorian border. They have evolved into a versatile breed that does well in a wide range of environments and produces top quality

neg: Lynches River few months for cleanup and repair. The river drops off the Piedmont between Bethune and McBee, cutting through the sand hills region, an old ocean shoreline with hills that are thought to be former beach dunes, now used for peach orchards and pine plantations. Near the river is the Carolina Sandhills National Wildlife Refuge and the Sandhills State Forest both in Chesterfield County. At Bethune, South Carolina you'll find the only bridge in the world that crosses the same river three times and the river does not fork. The Lynches River forms a large 'S" at the place where US

neg: Murray River (Western Australia) Oakley Brook. More land allocations along the southern bank of the river were made; however, settlement seemed to be limited to no further south that the Murray River grants, partly because of continuing and increasing conflicts with local aborigines. These conflicts culminated in the infamous Battle of Pinjarra in October 1834 where up to 40 Noongar people of the local Pindjarup tribal group were killed by white settlers. The battle had followed a raid in Perth by members of the Murray River tribe. The following year, a formal truce was made between the Murray River and the Swan River Noongars

neg: Murray Grey cattle Murray Grey cattle Murray Grey is a breed of Australian polled beef cattle that was developed in the upper Murray River valley on the New South Wales /Victorian border. They have evolved into a versatile breed that does well in a wide range of environments and produces top quality carcasses. The Murray Grey breed was developed from an initial chance mating of a black Aberdeen Angus bull and a roan Shorthorn cow in 1905 during the Federation drought. The resulting thirteen dun-grey calves from these matings were kept as curiosities and then bred on the "Thologolong" property along the Murray

neg: Jindabyne Dam Work to modify the dam spillway commenced in 1994 and was ongoing as at July 2009. Lake Jindabyne receives the flow from the Snowy River as well as its tributaries, the Thredbo River and Eucumbene River. The Jindabyne pumping station pumps the water from the rivers into the Snowy-Murray tunnel where it flows west through Murray 1 and Murray 2 Power Stations before entering the Swampy Plains River and then the Murray River. The flow of water into Lake Jindabyne is particularly strong during the spring months of October and November. The idea of the Snowy Mountains Scheme was developed

neg: Wyoming Divide spans north-south across the central portion of the state. Rivers east of the divide drain into the Missouri River Basin and eventually the Gulf of Mexico. They are the North Platte, Wind, Big Horn and the Yellowstone rivers. The Snake River in northwest Wyoming eventually drains into the Columbia River and the Pacific Ocean, as does the Green River through the Colorado River Basin. The Continental Divide forks in the south central part of the state in an area known as the Great Divide Basin where the waters that flow or precipitate into this area remain there and cannot

neg: River Ayr practitioners of hillwalking and other related activities are probably aware that the river is pathed for upwards of 90% of its length. Due to disputes with estate owners and weather damage, the walk does temporarily abandon the river in a couple of locations. The path begins in the former village of Glenbuck, now a casualty of opencast mining and general industry decline. It follows the river from its source at Glenbuck Loch and ends at the coastal town of Ayr, where the river empties into the ocean at the Firth of Clyde. Typically the walk is done in 2 or

neg: Wakool River over the course of its length. Wakool River Wakool River, an anabranch of the Edward River that is part of the Murray River catchment within the Murray-Darling basin, is located in the western Riverina region of south western New South Wales, Australia. The Wakool River splits from the Edward River (itself an anabranch of the Murray) near Deniliquin, and flows generally to the west, southwest, northwest, and then west, joined by eleven minor tributaries, including the Niemur River. The Wakool is rejoined by the Edward River near Kyalite, not far from where it runs back into the main channel of

neg: Bruce Murray (soccer) the metals trading industry, but in 2001, he decided to re-enter soccer with the Atlanta Silverbacks youth program. In 2002, Murray became the Director of coaching with the Roswell Soccer Club in Georgia. On September 17, 2004, Harvard University announced that Murray had been hired as an assistant coach with the men's soccer team. He was with Harvard for two seasons, then moved to the Capital Area Soccer League in Raleigh, NC where he was a staff coach. On March 20, 2011, Murray was elected to the National Soccer Hall of Fame. Bruce Murray is currently coaching at the Center

neg: Murray River rafts, they are known as "Lalangengall" or "the two watercraft". Remarkably, this story of a hunter pursuing a Murray cod that carved out the Murray persists in numerous forms in various language groups that inhabit the enormous area spanned by the Murray system. The Wotojobaluk people of Victoria tell of Totyerguil from the area now known as Swan Hill who ran out of spears while chasing Otchtout the cod. The first Europeans to encounter the river were Hamilton Hume and William Hovell, who crossed the river where Albury now stands in 1824: Hume named it the "Hume River" after his

neg: Squidward Tentacles he joined the Ocean Institute, an ocean education organization, where he had the idea to create a comic book titled "The Intertidal Zone", which led to the creation of "SpongeBob SquarePants". In 1987, Hillenburg left the Institute to pursue a career in animation. Several years after studying experimental animation at the California Institute of the Arts, Hillenburg met Joe Murray, creator of "Rocko's Modern Life", at an animation festival. Murray offered Hillenburg a job as a director of the series. Martin Olson, one of the writers for "Rocko's Modern Life", read "The Intertidal Zone" and encouraged Hillenburg to create a

neg: Eucalyptus camaldulensis Green Gully. The Goulburn River was dammed by the southern end of the fault to create a natural lake. The Murray River flowed to the north around the Cadell Fault, creating the channel of the Edward River which exists today and through which much of the Murray River's waters still flow. Then the natural dam on the Goulburn River failed, the lake drained, and the Murray River avulsed to the south and started to flow through the smaller Goulburn River channel, creating "The Barmah Choke" and "The Narrows" (where the river channel is unusually narrow), before entering into the proper

neg: Water Witch (1835 cutter) European crossing, on horseback, of Northern Yorke Peninsula. From June 1840 to January 1841, she supplied Eyre’s expedition at locations such as the head of Spencer Gulf, Streaky Bay and Fowlers Bay. In 1841, her range was restricted to Gulf St Vincent due to her leaky condition. On Pullen's suggestion, she was sent to Encounter Bay where on 8 May 1841, she became the first European vessel to successfully enter the River Murray mouth. E. B. Scott, a friend of Eyre, who had assisted Pullen in his task of surveying Lake Albert acted as mate, and negotiated her from Wellington

neg: Pinjarra massacre they crossed the Serpentine River and went forward to the Murray delta where tracks of a sizable group of Aboriginal men women and children were discovered heading towards Pinjarra. In the late afternoon, they camped at Jinjanuk, 10 miles from the mouth of the Murray River, so that they could begin the attack early next morning when they judged the Aboriginal group would be least prepared. The group was awoken two hours before dawn on 28 October, and ate breakfast in the dark. By 8:00 am, the party had rejoined the Murray where the river was 30 metres wide, between

neg: HMS Ocean (1898) small craft were armed to enter the Shatt al-Arab, the river leading to Basra. The first objective was to silence the old fortress at Al-Faw. On 5 November, Britain declared war on the Ottoman Empire, and the next morning, "Ocean" began the bombardment of Al-Faw. A landing party of 600 men, some of whom came from "Ocean"s detachment of Royal Marines, stormed the fortress and captured it, having encountered no resistance. By December 1914, the ground forces "Ocean" supported had advanced to Al-Qurnah, at the juncture of the Euphrates and Tigris, allowing the Admiralty to recall "Ocean" for other purposes.

neg: PS Pride of the Murray as a tourist attraction in Echuca. She runs daily hour long journeys up and down the river. She is also available for 2 or 3 hour charters. The "Pride of the Murray" is operated by Murray River Paddlesteamers in Echuca where she were originally built. The "Pride of the Murray" has dimensions 25.1m x 4.9m x 1.5m. Its paddle-wheels came from the "PS Hero". PS Pride of the Murray The Pride of the Murray, like many other paddle steamers, started out life as a timber logging barge. It was built at Echuca in 1924. The "Pride of the Murray" was

neg: Greenough River the southern side, where the adjacent dune is more stable. Evidence from wind gaps suggests that, thousands of years ago, the Greenough River turned to the north-west a few kilometres further from the coast than it does at present, at the present-day site of Walkaway. It then ran along the inside of a limestone ridge, following what is now the path of the Geraldton–Dongara railway line, to the vicinity of Rudds Gully. Both watercourses then flowed north to discharge into the Chapman River. Later, Rudds Gully cut its own path to the ocean, and the Greenough River discharged into it;

neg: Killary Harbour of Leenane. In its innermost section, it becomes very narrow, widens where a small river comes in from the south, and ends with the line of the valley of the Erriff River. The river itself does not enter on the main line of the Harbour but curves northwards and then runs south into the inlet. The northern shore rises sharply to a much greater extent than the southern, which is in places merely hilly. On that northern shore lies the mountain Mweelrea, Connacht's highest, rising to 814 metres, and the sides of which fall steeply into the inlet, with Uggool

neg: Revelle factor / (Δ[DIC] / [DIC]) where DIC is dissolved inorganic carbon. Δ[] / [] is the instantaneous change in p and Δ[DIC] / [DIC] is the instantaneous change in DIC. In order to enter the ocean, carbon dioxide gas has to partition into one of the components of carbonic acid: carbonate ion, bicarbonate ion, or protonated carbonic acid, and the product of these many chemical dissociation constants factors into a "back-pressure" that limits how fast the carbon dioxide can enter the surface ocean. The species of DIC present in ocean waters is dependent on the system's alkalinity, and is illustrated by

neg: Bush River (South Carolina) flows generally southeastwardly into Newberry County, past Joanna. It joins into the Saluda River about 11 mi (17 km) south of Newberry as part of Lake Murray, which is formed on the Saluda by Saluda Dam. Bush River (South Carolina) The Bush River is a tributary of the Saluda River, 30 mi (48 km) long, in the Piedmont region of western South Carolina in the United States. Via the Saluda and Congaree Rivers, it is part of the watershed of the Santee River, which flows to the Atlantic Ocean. According to the Geographic Names Information System, it has also been

neg: Cottonwood River (Minnesota) river was formerly dammed to form a lake in the state park, but the dam was not rebuilt after being washed out by floods in 1965 and 1969. Due to the northeastward slope of the Coteau des Prairies and the presence of a terminal moraine along the northern side of the river, very few tributaries enter the Cottonwood River from the north. The largest is Sleepy Eye Creek, 51 miles (82 km) long, which flows eastwardly through Redwood and Brown Counties, past Cobden. Tributaries from the south include Plum Creek, 35 miles (56 km) long, which flows northeastwardly through Murray

neg: Molonglo River tailings collapses into the river between the 1930s and 1950s, eradicating all native fish and most other aquatic life downstream from the site. Despite government funded rehabilitation programs in 1976, some toxic leachates still enter the river from the Captain's Flat mine site. Consequently, when Lake Burley Griffin was built upon the Molonglo and filled in 1964, the waters were devoid of native fish. Restocking commenced in the 1970s and continued through 1980s have re-established Murray Cod and Golden Perch in the lake and a short stretch of river upstream. A large stretch of the Molonglo still holds nothing but

neg: Diseases and parasites in salmon where the salmon is one of two hosts. The fish releases the spores after spawning. In the "Henneguya" case, the spores enter a second host, an invertebrate, in the spawning stream. When juvenile salmon migrate to the Pacific Ocean, the second host releases a stage infective to salmon. The parasite is then carried in the salmon until the next spawning cycle. The myxosporean parasite that causes whirling disease in trout has a similar life cycle. However, as opposed to whirling disease, the "Henneguya" infestation does not appear to cause significant incapacitation of the host salmon — even heavily infected fish

neg: Magic Pengel: The Quest for Color Zoe and Taro's homeland. Zoe and Taro don't know where Galileo went, and have been searching for their father by throwing notes in a bottle into the ocean. You must enter tournaments to get the money Zoey and Taro need to pay off the mortgage on their Homeland, help them search for their father, and eventually defeat the Doodle King himself. "Magic Pengel" is known for its flexibility in characters - the player can create his or her own. Unlike "Graffiti Kingdom", the second game in the "Rakugaki Oukoku" series, the "main character" does not exist: the storyline revolves around

neg: Humboldt River Humboldt River The Humboldt River runs through northern Nevada in the western United States. At approximately long it is the third longest river in the Great Basin, after the Bear and Sevier Rivers. It has no outlet to the ocean, but instead empties into the Humboldt Sink. It is the fifth largest river in the United States, in terms of discharge, that does not ultimately reach the ocean, while it is the largest in terms of area drained. Through its tributaries the river drains most of sparsely populated northern Nevada, traversing the state roughly east to west, and passing through

neg: Younghusband Peninsula Younghusband Peninsula Younghusband Peninsula is a long narrow peninsula in South Australia. It separates the Coorong Channel, the Tauwitchere Channel and the Coorong which are part of the estuary of the River Murray from the Southern Ocean which including water bodies such as Encounter and Lacepede Bays. It lies entirely within the Coorong National Park. The peninsula is over long, but less than wide at its widest point. Its narrowest point is less than wide. The Younghusband Peninsula, together with the Sir Richard Peninsula on the western side of the Murray Mouth, are the coastal dune system that forms the

neg: Murbko, South Australia of Chaffey while the northern third is in the Mid Murray Council. The entire locality is in the federal Division of Barker. The modern locality of Murbko includes a number of historic landings and homesteads along the river from the time when riverboats provided the most reliable transport. These include Woods Flat which had a school and institute. Murbko, South Australia Murbko is a locality in the Murray Mallee region of South Australia. It is located on the left bank of the Murray River downstream of the northwest bend where the river turns to flow roughly south. The river forms

neg: Albury Not realising it was the same river, he named it the Murray River. Both names persisted for some time, Hume falling into disuse eventually in favour of Murray. The aboriginal name for the river was "Millewa". A crossing place for the Murray became popular close to where Hovell inscribed the tree. In summer it was usually possible to cross the river by foot. Among the first squatters to follow in the steps of the explorers and settle in the district were William Wyse and Charles Ebden. The first European buildings erected at the crossing place were a provisions store and

neg: Georgia v. South Carolina (1990) wall, even though it was on the South Carolina side of the river. This new land was called "Denwill and Horseshoe Shoal". Given the valuable natural resources off the Atlantic Ocean shore, the two states also contested where the off-shore boundary between the two states is located. The typical procedure would be to locate the mouth of the Savannah River and then draw a line perpendicular to the shore from the midpoint of the river's mouth. However, the river does not have a clearly defined mouth. Tybee Island forms the southern edge of its mouth, but there is no highlands

neg: Ribeira de Iguape River the Ribeira de Iguape runs through the mountains of the Serra do Mar, and has turbulent waters that are popular for rafting. In the first it drops about through the mountains to the region near Itapeuna. From there it descends in to the city of Registro, where it is only above sea level, although still from its mouth. From the port town of Registro the river flows quietly through the coastal plain, reaching the Atlantic Ocean in Barra do Ribeira near Iguape, São Paulo. It is navigable along this section. Near the river mouth, some of the water does not

neg: Open and closed lakes lake. Open and closed lakes Open and closed lakes refer to the major subdivisions of lakes - bodies of water surrounded by land. Exorheic, or open lakes drain into a river, or other body of water that ultimately drains into the ocean. Endorheic basins fall into the category of endorheic or closed lakes, wherein waters do not drain into the ocean, but are reduced by evaporation, and/or drain into the ground. An open lake is a lake where water constantly flows out under almost all climatic circumstances. Because water does not remain in an open lake for any length of

neg: Open and closed lakes Open and closed lakes Open and closed lakes refer to the major subdivisions of lakes - bodies of water surrounded by land. Exorheic, or open lakes drain into a river, or other body of water that ultimately drains into the ocean. Endorheic basins fall into the category of endorheic or closed lakes, wherein waters do not drain into the ocean, but are reduced by evaporation, and/or drain into the ground. An open lake is a lake where water constantly flows out under almost all climatic circumstances. Because water does not remain in an open lake for any length of time,

neg: European maritime exploration of Australia commanded by Lieutenant John Bowen, sailed from Port Jackson on 31 August 1803 to establish a settlement in Van Diemen's Land, and on 10 October 1803 a convoy of two ships and "Ocean" led by Captain David Collins carrying 402 people entered Port Phillip and formed a settlement near Sorrento. The first British to enter the bay were the crews of , commanded by John Murray and, ten weeks later, "Investigator", commanded by Flinders, in 1802. "Investigator" was declared unseaworthy, so in 1803 Flinders was compelled to return to England as a passenger on , together with his charts and

neg: Deschutes River (Oregon) River, southwest of Biggs Junction and from the Columbia's mouth on the Pacific Ocean. Named tributaries of the Deschutes River from source to mouth include Snow Creek then the Cultus River, Cultus Creek and Deer Creek, which enter at Crane Prairie Reservoir. Further downstream come the Fall River, the Little Deschutes River, and the Spring River followed by Tumalo Creek and Whychus Creek. The Metolius River and the Crooked River are next, both entering at Lake Billy Chinook. Then come Seekseequa Creek and Willow Creek followed by Dry Hollow and Campbell, Shitike and Trout creeks, after which comes the Warm

neg: Mercury pollution in the ocean group). Mercury can enter seas and the open ocean as a result of the down-stream movement and re-deposition of contaminated sediments from urban estuaries. For example, high total Hg content up to 5 mg/kg and averaging about 2 mg/kg occur in the surface sediments and sediment cores of the tidal River Mersey, UK, due to discharge from historical industries located along the banks of the tidal river including industries such as historical chlor-alkali industry. Sediments along a 100 km stretch of the Thames Estuary have also been shown to have total Hg contents of up to 12 mg/kg and a

neg: Humboldt River and livestock and protecting populations of native trout. Maggie Creek has a Beaver Creek tributary which flows from Beaver Peak in the Tuscarora Mountains. Humboldt River The Humboldt River runs through northern Nevada in the western United States. At approximately long it is the third longest river in the Great Basin, after the Bear and Sevier Rivers. It has no outlet to the ocean, but instead empties into the Humboldt Sink. It is the fifth largest river in the United States, in terms of discharge, that does not ultimately reach the ocean, while it is the largest in terms of

neg: Water resources management in Argentina River and the Uruguay River originate in Brazil. The Uruguay River runs north to south and forms a border with Argentina, Brazil, and Uruguay. The Parana River together with the Uruguay river form the Río de la Plata estuary. Only a few of the Argentine rivers such as the Futaleufú River flow to the Pacific, while the majority of rivers originate on eastern slopes of the Andes and run towards the Atlantic ocean. Argentina is home to at least three major endorheic basins or closed water drainage basins e.g. water does not flow to the ocean. Both the northwest and

neg: Murray Maxwell and Amherst and his retinue had to retire to Whampoa with their mission incomplete. At the mouth of the Pearl, "Alceste" was refused permission to enter the river and perfunctorily ordered to halt by a local mandarin, who threatened to sink the frigate if it tried to force passage. Responding angrily that he would pass the river with or without the mandarin's permission, Maxwell attacked the Chinese defences, breaking through a blockade of junks and firing on the forts guarding the river mouth, scattering their defenders. He sailed on to Whampoa without further impediment, without casualties; Chinese losses were reportedly

neg: Little Murray River (Victoria) Little Murray River (Victoria) The Little Murray River, an anabranch of the Murray River and part of the Murray-Darling basin, is located in the Mallee district of north western Victoria, in eastern Australia. The anabranch leaves the Murray River near Fish Point and flows generally northwest in a highly meandering course, joined by the Loddon River, before it rejoins the Murray near Swan Hill; descending over its course. Little Murray River and the Murray River enclose Pental Island. The traditional custodians of the land surrounding Little Murray River, the Aboriginal people of the Wemba-Wemba clan, called the river Parnimilli, meaning

neg: Hardhead catfish dirty gray color on top, with white undersides. Hardhead catfish are found mostly in the near-shore waters of the Western Atlantic Ocean, around the southeast coast of the United States, around the Florida Keys and the coast of the Gulf of Mexico. Hardhead catfish are also found in brackish estuaries and river mouths where the bottom is sandy or muddy, but only occasionally enter freshwater. It tends to move from shallower to deeper waters in the winter months. The species is generally common to abundant within its range. The hardhead catfish has four barbels under the chin, with two more

neg: Atlantic Ocean parts per thousand (3.3 – 3.7%) by mass and varies with latitude and season. Evaporation, precipitation, river inflow and sea ice melting influence surface salinity values. Although the lowest salinity values are just north of the equator (because of heavy tropical rainfall), in general the lowest values are in the high latitudes and along coasts where large rivers enter. Maximum salinity values occur at about 25° north and south, in subtropical regions with low rainfall and high evaporation. The high surface salinity in the Atlantic, on which the Atlantic thermohaline circulation is dependent, is maintained by two processes: the Agulhas

neg: Schistosoma dam prevented ocean water to enter and allowed new forms of agriculture. Human migration, increasing number of livestock and sites where human and cattle both contaminate the water facilitated mixing between the different schistosomes in Nder e.g. The same hybrid was identified during the 2015 investigation of a schistosomiasis outbreak on Corsica, traced to the Cavu river. A cladogram based on 18S ribosomal RNA, 28S ribosomal RNA, and partial cytochrome c oxidase subunit I (COI) genes shows phylogenic relations of species in the genus "Schistosoma": Geographical areas associated with schistosomiasis by the World Health Organization as of January 2017 include

neg: Rivers of Queensland north-westward, towards the Gulf of Carpentaria, the Gulf rivers; those that also rise on the other side of the crest of the range and flow south-westward, forming part of the Murray–Darling basin, the Murray–Darling rivers; and those that generally rise in the west of the state and flow south-westward, towards the Lake Eyre basin, the Lake Eyre rivers. One river is isolated and does not flow towards any other basin or sea. The following rivers are the longest river systems, by length. Rivers of Queensland This page discusses the rivers and hydrography of the state of Queensland, Australia. The principal

neg: Macquarie perch to damming of their habitat and subsequent encroachment of legally and illegally stocked fish species. The Hawkesbury-Nepean population appears to be threatened by introduced trout and other exotic fish, river damming and regulation, siltation, and urban encroachment, but does not appear to be as threatened as the Murray-Darling species. Information on this page relates primarily to the Murray-Darling population. There is also a translocated self-sustaining breeding population of Macquarie Perch located in the middle and upper reaches of the Yarra River on the outskirts of Melbourne. They highest numbers are found lowest reaches, which also support a mix of translocated