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Trent Valley
The Trent is the third-longest river in the United Kingdom. Its source is in Staffordshire, on the southern edge of Biddulph Moor. It flows through and drains the North Midlands. 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, Rugeley, Burton upon Trent and Nottingham before joining the River Ouse at Trent Falls to form the Humber Estuary, which empties into the North Sea between 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") and ''hynt'' ("way"). This may indeed indicate a river that is prone to flooding. However, a more likely explanation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Muskham
North Muskham is a village and civil parish in Nottinghamshire, England, close to the border with Lincolnshire. It is located between the River Trent and the A1 road, north of Newark-upon-Trent. The parish has a population of 943 (2001 census) with around 360 properties, increasing to 985 at the 2011 census. St Wilfrid's Church is the parish church, a medieval building which is Grade I listed. It was restored during 1906 and 1907. There is currently one public house: 'The Muskham Ferry'. History The village appears in the Domesday Book as ''Muscham'' in the hundred of Lythe. North Muskham was a large ancient parish, which also included the villages of Bathley and Holme. Until about 1575 the River Trent ran further east, but there was then a cataclysmic flood which changed the course of the river. Holme was therefore separated by the river from the rest of the parish. In 1866 Holme and Bathley became separate civil parishes. Between 1870 and 1872 John Marius Wilson' ... [...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, near 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 and Tixall until it flows through the grounds of Shugborough Hall to meet the Trent near Essex Bridge. Navigation Between 1816 and the 1920s, the section ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Torne
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 wat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Idle
The River Idle is a river in Nottinghamshire, England whose source is the confluence of the River Maun and River Meden near Markham Moor. The Idle flows north from its source through Retford and Bawtry before entering the River Trent at West Stockwith. Its main tributaries are the River Poulter and the River Ryton. The river is navigable to Bawtry, and there is a statutory right of navigation to Retford. Most of the land surrounding the river is a broad flood plain and the river is important for conservation, with 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. This would fit with the f ... [...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 on 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 passing under the Nottingham Canal an ... [...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, close to its eastern border with Nottinghamshire. Etymology The approximate meaning of the name is not in doubt, but there is room for debate about the precise derivation and its connotations. Brewer gives the commonly accepted explanation that it comes from the Old English words ("wandering") and ("wet meadow"). This is accepted by Kenneth Cameron, a leading placename expert and Derbyshire specialist, who interprets the name as "wandering, marshy river". Gelling, who specialises in seeking precise topographical equivalents for toponymic elements, confirms that signifies a marshy meadow but gives only southern examples. She conjectures that there is an element, ''wæsse'', perhaps Old English, that signifies very specifically "land by a meandering river which floods and drains quickly", and her examples are primarily Midland and northern. This seems to ... [...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 its ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Dove, Derbyshire
The River Dove (, ) is the principal river of the southwestern Peak District, in the Midlands of England and is around in length. It rises on Axe Edge Moor near Buxton and flows generally south to its confluence with the River Trent at Newton Solney. From there, its waters reach the North Sea via the Humber Estuary. For almost its entire course it forms the boundary between the counties of Staffordshire (to the west) and Derbyshire (to the east). The river meanders past Longnor and Hartington and cuts through a set of deep limestone gorges, Beresford Dale, Wolfscote Dale, Milldale and Dovedale. The river is a famous trout stream. Charles Cotton's Fishing House, which was the inspiration for Izaak Walton's ''The Compleat Angler'', stands in the woods by the river near Hartington. The river's name is now usually pronounced to rhyme with "love", but its original pronunciation rhymed with "rove". This pronunciation is still used by some residents of the lower reaches of the r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Swarbourn
The River Swarbourn is a minor tributary of the River Trent that flows for in Staffordshire, England. Geography Its catchment lies between that of the River Blithe to the West, and the River Dove to the north, in a part of the county known as Needwood Forest. The Swarbourn and its tributaries, which include the Eland Brook, Mare brook and Lin Brook, drain a catchment area of . The source is near to the village of Marchington Woodlands, it flows southeast, and passes through Newborough, Hoar Cross, Woodmill, and Yoxall until it joins the River Trent between Wychnor Park and Alrewas. The Staffordshire long distance footpath called the Way for the Millennium follows the Swarbourn from Yoxall to its confluence with the Trent. Ecology The Swarbourn has been classed as having moderate ecological quality under the Water Framework Directive. This is the middle band on the five part framework scale, which ranges from high, good, and moderate, through to poor and bad. The river is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Blithe
The River Blithe is a river in Staffordshire, England. It is a tributary of the River Trent and runs for around 18 miles from source to its confluence with the River Trent. Etymology The Origins of the name Blithe probably come from the Old English for gentle, cheerful, quiet or merry. This is probably rooted in fact as the River runs as a gentle stream for most of its journey to the River Trent. Course The Blithe rises in the Hills to the East of Stoke on Trent near to Heywood Grange Farm at around 800 feet above sea level. It is joined by several smaller streams as it makes its way towards Caverswall. The River though is still only a small stream at this stage. It passes the village of Blythe Bridge and roughly follows the Stoke to Derby Railway line until it reaches Church Leigh. The countryside is mainly agricultural and is intensively farmed. The River then turns south and flows into Blithfield Reservoir at Newton Hurst. On leaving the reservoir it flows south-east fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
