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River Alwin
The River Alwin is a short, steep upland river that drains the Kidland Forest on the southern flanks of the Cheviot Hills, in the Northumberland National Park, England. It is a tributary of the River Coquet and in length. Course Rising as the Outer Sike at the edge of the Kidland Forest between the peaks of Yarnspath Law and Bloodybush edge. It flows south through the forest gaining various burns and cloughs, to become the White Burn, until it reaches the confluence of the Yoke Burn, where it forms the River Alwin to the north of Kidlandlee. From this point the river flows south to collect the Allerhope Burn at the edge of the forest, continuing through a steep sided valley before reaching Clennell Hall. It then passes to the south of Alwinton, finally reaching the hamlet of Low Alwinton where it joins the Coquet. Hydrology Between 1969 and 1983 the flow of the Alwin, was measured in its lower reaches at a weir near Clennel. The fourteen year record shows that the catchment o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United Kingdom
The United Kingdom of Great Britain and Northern Ireland, commonly known as the United Kingdom (UK) or Britain, is a country in Europe, off the north-western coast of the continental mainland. It comprises England, Scotland, Wales and Northern Ireland. The United Kingdom includes the island of Great Britain, the north-eastern part of the island of Ireland, and many smaller islands within the British Isles. Northern Ireland shares a land border with the Republic of Ireland; otherwise, the United Kingdom is surrounded by the Atlantic Ocean, the North Sea, the English Channel, the Celtic Sea and the Irish Sea. The total area of the United Kingdom is , with an estimated 2020 population of more than 67 million people. The United Kingdom has evolved from a series of annexations, unions and separations of constituent countries over several hundred years. The Treaty of Union between the Kingdom of England (which included Wales, annexed in 1542) and the Kingdom of Scotland in 170 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northumberland
Northumberland () is a county in Northern England, one of two counties in England which border with Scotland. Notable landmarks in the county include Alnwick Castle, Bamburgh Castle, Hadrian's Wall and Hexham Abbey. It is bordered by land on three sides; by the Scottish Borders region to the north, County Durham and Tyne and Wear to the south, and Cumbria to the west. The fourth side is the North Sea, with a stretch of coastline to the east. A predominantly rural county with a landscape of moorland and farmland, a large area is part of Northumberland National Park. The area has been the site of a number of historic battles with Scotland. Name The name of Northumberland is recorded as ''norð hẏmbra land'' in the Anglo-Saxon Chronicle, meaning "the land north of the Humber". The name of the kingdom of ''Northumbria'' derives from the Old English meaning "the people or province north of the Humber", as opposed to the people south of the Humber Estuary. History ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clennell, Northumberland
Clennell is a small village and as Clennel, a former civil parish, now in the parish of Alwinton, in Northumberland, England. It is about north-east of Alwinton. In 1951 the parish had a population of 37. Governance Clennell is in the British House of Commons, parliamentary constituency of Berwick-upon-Tweed (UK Parliament constituency), Berwick-upon-Tweed. Clennell was formerly a Township (England), township in Alwinton parish, from 1866 Clennel was a civil parish in its own right until it was abolished on 1 April 1955 and merged with Biddlestone. See also *Clennell Hall References External links Villages in Northumberland Former civil parishes in Northumberland, Clennel Alwinton {{Northumberland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kidland
Kidland is a former civil parish, now in the parish of Alwinton in Northumberland, England, about northwest of Alwinton village. In 1951 the parish had a population of 58. History From 1856 Kidland was a civil parish in its own right until it was merged with Alwinton on 1 April 1955. Governance Kidland is in the parliamentary constituency of Berwick-upon-Tweed Berwick-upon-Tweed (), sometimes known as Berwick-on-Tweed or simply Berwick, is a town and civil parish in Northumberland, England, south of the Anglo-Scottish border, and the northernmost town in England. The 2011 United Kingdom census reco .... References External links GENUKI(Accessed: 3 December 2008) Former civil parishes in Northumberland Alwinton {{Northumberland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cheviot Hills
The Cheviot Hills (), or sometimes The Cheviots, are a range of uplands straddling the Anglo-Scottish border between Northumberland and the Scottish Borders. The English section is within the Northumberland National Park. The range includes The Cheviot (the highest hill), plus Hedgehope Hill to the east, Windy Gyle to the west, and Cushat Law and Bloodybush Edge to the south. The hills are sometimes considered a part of the Southern Uplands of Scotland as they adjoin the uplands to the north. Since the Pennine Way runs through the region, the hills are also considered a part of the northern Pennines although they are separated from the Cheviot Hills by the Tyne Gap, part of which lies within the southern extent of the Northumberland National Park. The Cheviot Hills are primarily associated with geological activity from approximately 480 to 360 million years ago, when the continents of Avalonia and Laurentia collided, resulting in extensive volcanic activity (the Caledonian o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northumberland National Park
Northumberland National Park is the northernmost national park in England. It covers an area of more than between the Scottish border in the north to just south of Hadrian's Wall, and it is one of least visited of the National Parks. The park lies entirely within Northumberland, covering about a quarter of the county. The park covers several distinct areas. In the north are the Cheviot Hills, a range of hills that mark the border between England and Scotland. Further south, the hills give way to areas of rolling moorland, some of which have been covered by forestry plantations to form Kielder Forest. The southernmost part of the park covers the dramatic central section of Hadrian's Wall, dating from the Roman occupation. The 10,000-year history of human habitation of the region is explored through the many archaeological sites, ranging from prehistoric monuments and Roman remains to Pele towers, constructed as a defence against invading Scots and Border Reivers. The Park's ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Coquet
The River Coquet runs through the county of Northumberland, England, discharging into the North Sea on the east coast at Amble. It rises in the Cheviot Hills on the border between England and Scotland, and follows a winding course across the landscape ("Coquetdale"). The upper reaches are bordered by the Otterburn Ranges military training ground, and are crossed by a number of bridges built in the 20th century. It passes a number of small villages and hamlets, and feeds one of the lakes created by extraction of gravel that form the Caistron Nature Reserve, before reaching the town of Rothbury, where it is crossed by a grade II listed bridge. Below the town is Thrum Mill, the restoration of which was featured on Channel 4 television. It loops around Brinkburn Priory, founded in the 1130s for Augustinian Canons, and its associated mill. At Felton it is crossed by two bridges, one dating from the 15th century, and its replacement, built in 1927, both of which are listed structu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clennell Hall
Clennell Hall is an historic manor house, now operated as a country hotel, situated at Clennell, Northumberland, Clennell, near Alwinton, Northumberland, England. It is a Grade II listed building. The Clennell family held the manor of Clennell from the 13th century. In a survey of 1541 the tower house at Clennell was described as 'a little tower of Percival Clennell' then newly repaired with a barmkin under construction. In 1715 it was the seat of Luke Clennell, (High Sheriff of Northumberland in 1727) and comprised an old tower on the east, a double wing at the west and a small court to the south with a 'handsome gateway'. In 1749 Philadelphia Clennell, the heiress of the estate married William Wilkinson, (High Sheriff in 1758). In 1895 their great grandson Anthony Wilkinson greatly extended the property by the addition of a large Tudor style mansion. The present building incorporates a Peel tower, pele tower of 1589, much altered. References * ''History of the Commoners of Gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alwinton
Alwinton (previously named "Allenton" and sometimes still referred to as this) is a village and former parish in Northumberland, England. Alwinton is named after the nearby River Alwin, and means farm on the River Alwin. Alwinton lies at the head of the Coquet valley, on the edge of both the Otterburn Army Training Estate and the Northumberland National Park. The village is roughly from the border with Scotland, and about to the west of Alnwick. The neighbouring village of Harbottle and Harbottle Castle are about from Alwinton. A road continues past Alwinton into the Cheviot Hills where it terminates at the ancient Roman military encampment of Chew Green. Having no shops, Alwinton's social life centres on the Rose and Thistle Inn, a public house owned by the Latchams. Regular Church of England services are offered at St. Michael and All Angels, which traditionally serves the parish of Alwinton encompassing the nearby townships of Biddlestone, Burradon, Clennell, Fairha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catchment
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the ''drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar but no ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gauging Station
A stream gauge, streamgage or stream gauging station is a location used by hydrologists or environmental scientists to monitor and test terrestrial bodies of water. Hydrometric measurements of water level surface elevation ("stage") and/or volumetric discharge (flow) are generally taken and observations of biota and water quality may also be made. The locations of gauging stations are often found on topographical maps. Some gauging stations are highly automated and may include telemetry capability transmitted to a central data logging facility. Measurement equipment Automated direct measurement of streamflow discharge is difficult at present. In place of the direct measurement of streamflow discharge, one or more surrogate measurements can be used to produce discharge values. In the majority of cases, a stage (the elevation of the water surface) measurement is used as the surrogate. Low gradient (or shallow-sloped) streams are highly influenced by variable downstream c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Water Framework Directive
The Water Framework Directive 2000/60/EC is an EU directive which commits European Union member states to achieve good qualitative and quantitative status of all water bodies (including marine waters up to one nautical mile from shore) by 2015. It is a framework in the sense that it prescribes steps to reach the common goal rather than adopting the more traditional limit value approach. The Directive's aim for 'good status' for all water bodies will not be achieved, with 47% of EU water bodies covered by the Directive failing to achieve the aim. Objectives of the Directive The Directive aims for 'good status' for all ground and surface waters (rivers, lakes, transitional waters, and coastal waters) in the EU. The ecological and chemical status of surface waters are assessed according to the following criteria (see also: freshwater environmental quality parameters): * Biological quality (fish, benthic invertebrates, aquatic flora) * Hydromorphological quality such as river b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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