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River Trent
The Trent is the third Longest rivers of the United Kingdom, longest river in the United Kingdom. Its Source (river or stream), source is in Staffordshire, on the southern edge of Biddulph Moor. It flows through and drains the North Midlands into the Humber Estuary. The river is known for dramatic flooding after storms and spring snowmelt, which in the past often caused the river to change course. The river passes through Stoke-on-Trent, Stone, Staffordshire, Rugeley, Burton-upon-Trent and Nottingham before joining the River Ouse, Yorkshire at Trent Falls to form the Humber Estuary, which empties into the North Sea between Kingston upon Hull in Yorkshire and Immingham in Lincolnshire. The wide Humber estuary has often been described as the boundary between the Midlands and the north of England. Name The name "Trent" is possibly from a Romano-British word meaning "strongly flooding". More specifically, the name may be a contraction of two Romano-British words, ''tros'' ("over" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
A drainage basin is an area of land in which 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 the drainage divide line. A drainage basin's boundaries are determined by watershed delineation, a common task in environmental engineering and science. In a closed drainage basin, or endorheic basin, rather than flowing to the ocean, water converges toward the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trent Falls
Trent Falls is the confluence of the River Ouse and the River Trent which forms the Humber between Lincolnshire and the East Riding of Yorkshire in England. Location The River Ouse flows to the east where it turns into the Humber, and the River Trent flows northwards. It curves to the east near the confluence, although this is largely engineered, rather than natural. A training wall was built on the western bank of the Trent after the First World War, in an attempt to keep the channel in a known position. The rivers deposit large volumes of silt in this area, and charts for coastal shipping have to be updated monthly, but for smaller vessels, the channel can be considered to be reasonably static. Despite the training wall and a mini-lighthouse called ' Apex Light' which is situated at the end of the wall, navigation at Trent Falls is not simple. There are no real waterfalls, but there is a very rapid race of water at difficult stages of the tide (especially spring tides), and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Mease
The River Mease is a lowland clay river in the Midlands area of England. It flows through the counties of Leicestershire, Derbyshire and Staffordshire and forms the administrative border between these counties for parts of its length. The river and the lower part of one of its tributaries, the Gilwiskaw Brook (pronounced ''jill-a-whiskey'') are both protected as "one of the best examples of an unspoilt meandering lowland river". The river receives protection under European Union law as a Special Area of Conservation (SAC), and protection under UK law as a Site of Special Scientific Interest (SSSI). Description The Mease is formed by a confluence of smaller streams near the village of Norton Juxta Twycross in North West Leicestershire. It flows westwards for approximately 16 miles (25 km) across a largely rural and agricultural landscape to its confluence with the River Trent at Croxall in Staffordshire, with its waters eventually reaching the North Sea via the Trent an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Tame, West Midlands
The River Tame is a river in the West Midlands of England, and one of the principal tributaries of the River Trent. The Tame is about long from the source at Oldbury to its confluence with the Trent near Alrewas, but the main river length of the entire catchment, i.e. the Tame and its main tributaries, is about . It forms part of the Severn-Trent flyway, a route used by migratory birds to cross Great Britain. Etymology The name derives from the Celtic language, although it may have even earlier roots. It is usually thought to mean "dark", by analogy with the Sanskrit word ''tamas'' meaning darkness. Other possibilities are "slow-moving" or "flowing", although the precise meaning is uncertain. The name is shared with the River Tame, Greater Manchester, and it is likely that the River Thame, the River Thames, the River Teme, the River Team, and the River Tamar all share the derivation. Historic significance Birmingham and the parishes in the centre and north of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Sow
The River Sow is a tributary of the River Trent in Staffordshire, England, and is the river that flows through Stafford. Course The river rises to the south of Loggerheads, Staffordshire, Loggerheads, near Broughton Hall, Staffordshire, Broughton and flows south-east beside the villages of Fairoak, Bishop's Offley and Walk Mill until it reaches Cop Mere. East of the Mere the river is joined by the Brockton Brook before it flows past Eccleshall and its castle. The Sow continues south-east passing Chebsey, where it is joined by the Meece Brook before reaching the mill at Worston and then Little and Great Bridgeford. The river then flows through the nature reserve of Doxey Marshes until it reaches Stafford, where it flows through Victoria park. Beyond the town at Baswich the Sow is joined by its largest tributary the River Penk, it then continues beneath the bridge between Milford, Staffordshire, Milford and Tixall until it flows through the grounds of Shugborough Hall to meet the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Torne (England)
The River Torne is a river in the north of England, which flows through the counties of South Yorkshire and North Lincolnshire. It rises at the Upper Lake at Sandbeck Hall, in Maltby in South Yorkshire, and empties into the River Trent at Keadby pumping station. Much of the channel is engineered, as it plays a significant role in the drainage of Hatfield Chase, which it crosses. The first major change occurred around 1628, when the drainage engineer Cornelius Vermuyden cut a new channel for the river across the Isle of Axholme, and built a sluice at Althorpe where it entered the River Trent. Nearly 90 years of civil unrest followed, before the issues of flooding were finally resolved. Drainage of the land bordering the river was carried out in the 1760s and 1770s. A new sluice was built at Keadby, lower downstream on the Trent in the 1780s, but the Torne was not re-routed to it until much later. The sluice at Keadby became a pumping station in 1940, and the option to pump ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Idle
The River Idle is a river in Nottinghamshire, England, formed by the confluence of the River Maun and the River Meden near Markham Moor. It flows north from its source through Retford and Bawtry before joining the River Trent at West Stockwith. Its main tributaries are the River Poulter and the River Ryton. The river is navigable as far as Bawtry, with a statutory right of navigation extending to Retford. Much of the land surrounding the Idle consists of broad flood plain, and the river is significant for conservation, with several Sites of Special Scientific Interest being designated along its course. Etymology The origin of the name is not known. River Idle is commonly taken to mean 'slow river' but this is unlikely as river names tend to be even older than settlement names, and the modern name is also at odds with the fact that it is known as a very fast flowing river. The Survey of English Placenames suggests that Idle (Idel) can mean an empty or uncultivated place. Thi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Greet
The River Greet is a small river in Nottinghamshire, England. Rising close to the village of Kirklington, the Greet flows in a southeasterly direction past Southwell and Rolleston to meet the River Trent at Fiskerton. Hydrology The river has a catchment of and an average flow of 6.08 million gallons (27.65 Megalitres) per day, measured at the gauging station in Southwell. The catchment receives of rainfall in an average year. Above Southwell, the underlying geology is mainly Sherwood and Mercia sandstone, with some Mercia mudstone along the southern edge of the catchment. Below Southwell, the geology is predominantly Mercia mudstone. There is a layer of clay, sand and gravel alluvium overlaying this in the river channel. The river is greatly affected by rainfall, raising levels and muddying the water. Course The river rises as a series of springs to the west of Kirklington, close to the contour. It is joined by Cotton Mill Dyke and Edingley Beck, and to the east of Kirk ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Leen
The River Leen is a 15-mile (24 km) long tributary of the River Trent that flows through Nottinghamshire, and the city of Nottingham in the East Midlands of England. The name Leen developed through various renderings of the Celtic word meaning "lake" or "pool" (''Llyn'' in modern Welsh). Some of the surrounding villages derived their name from the River Leen. Lenton, ''ton'' being the Saxon word for "village"; and Linby, ''by'' being the Danish equivalent of ''ton.'' Course The Leen rises as a series of springs at the foot of the Robin Hood Hills just outside Annesley. It then flows through the grounds and lakes of Newstead Abbey, passing Papplewick and meeting the Whyburn as it passes through Bestwood Country Park, following the route of the Leen Valley into suburban and urban Nottingham. Within the city it flows through the centre of Bulwell, and passes Basford where it is joined by the Day Brook. The Leen then flows through Radford, and Lenton before pass ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Erewash
The River Erewash is a river in England, a tributary of the River Trent that flows roughly southwards through Derbyshire and Nottinghamshire, forming the boundary between the two counties for much of its length. It rises near Kirkby-in-Ashfield, and passes close to Pinxton, Ironville, Langley Mill, Eastwood, Ilkeston, Trowell, Stapleford, Sandiacre, Toton and Long Eaton to reach the River Trent near Beeston. It shares its valley with a railway line from Kirkby-in-Ashfield to Pye Bridge Junction, and the Erewash Valley line below the junction. The Pinxton Branch of the Cromford Canal runs parallel to the upper reaches, and below Ironville the main line of the abandoned Cromford Canal enters the valley. At Langley Mill, both the Erewash Canal and the abandoned Nottingham Canal fit into the valley, with the Nottingham Canal turning to the east at Trowell, and the Erewash Canal continuing through Long Eaton when the river turns to the east to reach its mouth. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Derwent, Derbyshire
The Derwent is a river in Derbyshire, England. It is long and is a tributary of the River Trent, which it joins south of Derby. Throughout its course, the river mostly flows through the Peak District and its foothills. Much of the river's route, with the exception of the city of Derby, is rural. However, the river has also seen many human uses, and between Matlock and Derby was one of the cradles of the Industrial Revolution. It is the site of the Derwent Valley Mills, the first industrial-scale cotton mills. Today it provides a water supply to several surrounding cities, and its steep-sided valley is an important communications corridor through the uplands of the Peak District. The scenery of the Derwent valley attracts many tourists. The upper reaches pass through the Peak District National Park, whilst the middle reaches around the old spa town of Matlock Bath offer souvenir shops and amusement arcades, together with attractions such as the Heights of Abraham and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
