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River Esk (other)
River Esk is the name of: United Kingdom England *River Esk, North Yorkshire, in the North York Moors National Park and the county of North Yorkshire * River Esk (Ravenglass), in the Lake District National Park and the county of Cumbria * River Esk (Solway Firth), in the north of the county of Cumbria and along the border with Scotland, also known as the ''Border Esk'' Scotland * River Esk (Solway Firth), in Dumfries and Galloway and along the border with England, also known as the ''Border Esk'' *River Esk, Lothian, which runs for much of its length as two separate tributaries, the North Esk and the South Esk *River North Esk, in Angus and Aberdeenshire *River South Esk, in Angus Australia * Esk River (New South Wales), a tributary of the Clarence River * Esk River (Queensland) * North Esk River a river in Tasmania, Australia * South Esk River a river in Tasmania, Australia New Zealand *Esk River (Canterbury), New Zealand * Esk River (Hawke's Bay), New Zealand See also *No ...
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River Esk, North Yorkshire
The River Esk is a river in North Yorkshire, England that empties into the North Sea at Whitby after a course of around through the valley of Eskdale, named after the river itself. The river's name is derived from the Brythonic word "isca" meaning "water". The Esk is the only major river in Yorkshire that flows directly into the North Sea; all other watercourses defined as being major rivers by the Environment Agency, either flow to the North Sea via the River Tees or the Humber Estuary. Overview Due to its rural nature, the river is clean and healthy, supporting a wealth of wildlife. Salmon spawn right up through Eskdale, and a number of " leaps" are provided to enable them to travel through weirs on the course. There are clearly visible examples at Ruswarp, where the tidal stretch through to Whitby begins and at Sleights. Around Whitby the Esk has a large population of sea trout, and the river is noted for freshwater pearl mussels (the only river in Yorkshire to hav ...
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River Esk (Ravenglass)
The River Esk, sometimes called the Cumbrian Esk, is a river in Cumbria, England. It flows for approximately 25 km (15.5 miles) from its source in the Scafells range of mountains to its estuary at Ravenglass. The valley it flows through is known as Eskdale. It is one of two Rivers Esk in Cumbria, and not to be confused with the Border Esk which flows into Cumbria from Scotland. In his book ''The Origins Of English Place Names'', P. H. Reaney says that the river's name is derived from the Brythonic word ''*Iska'' ("abounding in fish") and cognate with the modern Welsh word ''Pysg'' ("fishes"). This derivation applies to many similarly named rivers throughout Britain including the Axe, Exe and Usk, the names evolving local distinctions over the centuries. Gives details of etymology (second paragraph). The Esk is, in part, paralleled by the narrow-gauge Ravenglass and Eskdale Railway and as a consequence the railway has named one of its steam locomotives after the river. ...
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River Esk (Solway Firth)
The River Esk ( gd, Easg), also known as the Border Esk, is a river that rises in the Scottish region of Dumfries and Galloway before crossing the border to the English county of Cumbria and flowing into the Solway Firth. Course The river rises in the hills to the east of Moffat and its two main tributaries, the Black Esk and the White Esk, merge at the southern end of Castle O'er Forest. It flows south east through Eskdale past Langholm. Near Langholm the river is crossed by the Duchess Bridge which is said to be the oldest iron bridge in Scotland. The Esk merges with Liddel Water (which defines the border between Scotland and England). Before passing Longtown the river enters England and merges with the River Lyne and enters the Solway Firth near the mouth of the River Eden. It was formerly one of the boundaries of the Debatable Lands as marked by the Scots' Dike. Tributaries The various tributaries of the Esk are described proceeding downstream. The White Esk arise ...
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River Esk, Lothian
The River Esk ( Brythonic: Isca (water), gd, Easg (water)), also called the Lothian Esk, is a river that flows through Midlothian and East Lothian, Scotland. It initially runs as two separate rivers: the North Esk and the South Esk. Route The North Esk rises in the North Esk Reservoir in the Pentland Hills, in Midlothian, a mile (1.6 km) north of the village of Carlops. It flows north-east past Penicuik and Auchendinny, where it is joined by the Glencorse Burn, flowing in a south-easterly direction from the Glencorse Reservoir.Ordnance Survey, 1:25000 map The reservoir was built by the Edinburgh Water Company in the 1820s, to supply compensation water to millowners on the Esk when they started to take water from the Glencorse Burn for drinking water supplies. The river continues through Roslin Glen and the Penicuik–Dalkeith Walkway, past Hawthornden Castle, Polton, Lasswade and Melville Castle. The South Esk rises at the southernmost extremity of Midlothian, on th ...
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River North Esk
The North Esk ( gd, Easg Thuath) is a river in Angus and Aberdeenshire, Scotland. It is formed by the meeting of the Water of Mark (from Glen Mark) and the Water of Lee (from Loch Lee), and enters the North Sea four miles north of Montrose. It forms the boundary between Angus and Aberdeenshire at certain stages in its course. It was also noted in the 19th century as a good point for fishing. Tributaries Downstream of the meeting of the headwaters referred to above, the River North Esk is joined by various other tributaries. The Water of Effock enters on its right side and then the Water of Tarf enters on its left bank at Tarfside. The West Water is a considerable right bank tributary which enters near Stracathro in Strathmore. Its upper reaches are known as the Water of Saughs. The Luther Water is the last significant tributary of the North Esk; it enters on the left bank near North Water Bridge. The Luther Water drains the Howe of the Mearns. Glen Esk Villages Tarfside ...
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River South Esk
:''Note: the southern headwater of the River Esk in Lothian is also known as the South Esk.'' The South Esk ( gd, Easg Dheas) is a river in Angus, Scotland. It rises in the Grampian Mountains at Loch Esk in Glen Doll and flows through Glen Clova to Strathmore at Cortachy, 5 km north of Kirriemuir. Its course takes it past Brechin and enters the North Sea at Montrose. The river gives its name to the title of Earl of Southesk, held by the Carnegie family Carnegie may refer to: People *Carnegie (surname), including a list of people with the name *Clan Carnegie, a lowland Scottish clan Institutions Named for Andrew Carnegie * Carnegie Building (Troy, New York), on the campus of Rensselaer Polyte .... References South Esk {{Scotland-river-stub ...
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Esk River (New South Wales)
Esk River, a perennial stream that is part of the Clarence River catchment, is located in the Northern Rivers region of New South Wales, Australia. Course and features Esk River rises below Richmond Range, southeast of Tabbimoble, and flows generally to south through Bundjalung National Park towards its confluence with the northern arm of the Clarence River, northwest of the coastal fishing village of Iluka. The river descends over its course. The river is an increasingly popular kayak fishing location that is home to a variety of fish species such as yellowfin bream, dusky flathead and sand whiting in its lower brackish areas and has a good population of Australian bass in its fresh water reaches. The Esk River is considered the largest untouched coastal river system on the New South Wales North Coast. See also * List of rivers of Australia * List of rivers of New South Wales (A–K) * Rivers of New South Wales This page discusses the rivers and hydrography of th ...
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Esk River (Queensland)
The Esk River is a river located in the Wet Tropics of Far North Queensland, Australia. Course and features The river rises below Dowlings Hill, sourced by runoff from the Great Dividing Range, and flows north across the mostly uninhabited coastal plain. The Esk River enters the Annan Forest Reserve and flows through a wetland dominated by mangroves. At its river mouth, the Esk River is joined by the Annan River The Annan River ( Kuku Nyungkal: ''Yuku Baja'') is a river located in the Wet Tropics of Far North Queensland, Australia. Course and features The river rises in the Yorkey Range below Mount Romeo near , north-northwest of . The river flows g ... and together the two rivers discharge into Walker Bar and then onto the Coral Sea approximately south of . The river descends over its course. Much of the Esk River catchment lies within protected area tenure. the river appeared to be in a healthy condition with limited siltation and only infrequent pockets of ...
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North Esk River
The North Esk River is a major perennial river located in the northern region of Tasmania, Australia. Location and features It is one of the tributaries of the Tamar River together with the South Esk River. It starts in the Northallerton Valley below Ben Nevis in the states North East, joining with the St Patricks River before flowing through Launceston. Launceston's Old Seaport tourist feature is located on the North Esk River. The river becomes tidal downstream of Hoblers Bridge to where it meets the Tamar. It is sometimes subject to flooding, especially in East Launceston suburbs. The largest tributary of the North Esk is the St Patricks River, with others including the Ford River which flows from the skifields of Ben Lomond and down stream of the Corra Linn Gorge, the Roses Rivulet and Distillery Creek. History Indigenous history The North Esk River forms part of the traditional lands of the Tasmanian Aborigines. The upper reaches of the river, and its watershed, is cou ...
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South Esk River
The South Esk River, the longest river in Tasmania, is a major perennial river located in the northern region of Tasmania, Australia. Location and features The South Esk springs from the eastern foothills of the Ben Lomond plateau near Mathinna and the river's course describes an arc around the entire southern promontory of the mountain – running through Fingal, Avoca and Evandale before winding its way northwest through Perth, Longford and Hadspen. The river merges with the tributary Meander River, then flows through the narrows of the Cataract Gorge to finally meet the North Esk River at Launceston. From this confluence arises kanamaluka/Tamar River, which runs to the Bass Strait. The natural river flow is interrupted by the Trevallyn Dam, near Launceston, constructed as part of the Trevallyn Power Station hydroelectric power scheme. The river is subject to flooding which overflows at Lake Trevallyn to create the spectacle of high rapids coursing through the narrow ...
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Esk River (Canterbury)
Canterbury's Esk River is a tributary of the Waimakariri River. It rises in the Dampier Range near Esk Head, and flows southwest on the western side of the Puketeraki Range to reach the upper Waimakariri some north of Springfield. Brown and rainbow trout are available in the river, but fishing is restricted. Its tributaries include the Pūkio Stream, which prior to the Pleistocene epoch acted as an outlet for the Cox River into the Esk. See also * Esk River (Hawke's Bay) *List of rivers of New Zealand This is a list of all waterways named as rivers in New Zealand. A * Aan River * Acheron River (Canterbury) * Acheron River (Marlborough) * Ada River * Adams River * Ahaura River * Ahuriri River * Ahuroa River * Akatarawa River * Ākiti ... References Land Information New Zealand- Search for Place Names Hurunui District Rivers of Canterbury, New Zealand Rivers of New Zealand {{CanterburyNZ-river-stub ...
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Esk River (Hawke's Bay)
The Esk River of Hawke's Bay, in the eastern North Island of New Zealand, one of two rivers of that name in the country, is one of Hawke's Bay's major rivers. It flows south from the slopes of Taraponui in the Maungaharuru Range before turning east to reach Hawke Bay north of Napier. State Highway 5 follows the lower course of the river for several kilometres close to the settlement of Eskdale. The river is probably named after the Esk River in southern Scotland and north-west England. Where the river reaches the sea, it ponds behind a shingle bank. At times the sea drives up shingle that blocks the outlet until the ponding water breaks through. The outlet occasionally needs to be opened artificially to prevent flooding. Prior to the 1931 Hawke's Bay earthquake, the pond also flowed into the Petane Stream and south through Bay View into the northern end of Ahuriri Lagoon when the beach outlet was blocked. The earthquake raised the area, preventing the ponded water from flowi ...
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