At Stoke-on-Trent in the upper reaches, the average flow is only 0.6m3/s (21cuft/s), which increases considerably to 4.4m3/s (160cuft/s), at Great Haywood, as it includes the flow of the upper tributaries draining the Potteries conurbation. At Drakelow upstream of Burton the flow increases nearly three-fold to 36.1m3/s (1,270cuft/s), due to the additional inflow from the largest tributary the Tame. Menu. . Commercial carrying above Nottingham ceased during the 1950s, to be replaced by pleasure cruising. They have also now been sighted at locations such as Wolseley, Willington, and Attenborough. The major proposals included a cut and lock at Cranfleet, where the River Soar joins the Trent, a cut, locks and weirs at Beeston, which would connect with the Nottingham Canal at Lenton, and a cut and lock at Holme Pierrepont. The work was completed by September 1787, and dividends of 5 per cent were paid on the capital during 1786 and 1787, increasing to 7 per cent, the maximum allowed by the Act, after that. [178] At one time these sites provided a quarter of the electricity needs of the UK, giving rise to the epithet 'Megawatt Valley'. Tolls were reduced to retain the traffic, wages were increased to retain the workforce, and they sought amalgamation with a railway company. 109. [77], Early bridges were vulnerable to floods, and in 1309 many bridges were washed away or damaged by severe winter floods, including Hethbeth Bridge. [177], Once these early stations reached the end of their functional life, they were usually demolished, although in some cases the sites have been retained and redeveloped as gas fired power stations. [119], From the 1960s onwards, there were gradual but steady improvements to the inadequate sewage works and sewers built during the Victorian era in the urban areas, but this was expensive, and took time to complete. Towns Stone, Rugeley, Burton upon Trent, Newark-on-Trent, Gainsborough Physical characteristics Source - location Biddulph Moor, Staffordshire, England - coordinates 530658N020825W / 53.11611N 2.14028W / 53.11611; -2 - elevation 275 m (902 ft) Mouth - location Trent Falls, Humber Estuary, Lincolnshire, England - coordinates [90], Between Trent Falls and Keadby, coastal vessels that have navigated through the Humber still deliver cargoes to the wharves of Grove Port, Neap House, Keadby, Gunness and Flixborough. Such was the case at Willington, Gunthorpe and Gainsborough. This ranges from moorland grazing of sheep in the upland areas, through to improved pasture and mixed farms in the middle reaches, where dairy farming is important. The river then continues south through the market town of Stone, and after passing the village of Salt, it reaches Great Haywood, where it is spanned by the 16th-century Essex Bridge near Shugborough Hall. The river turns north-east where it is joined by its largest tributary, the Tame (which is at this point actually the larger, though its earlier length shorter) and immediately afterwards by the Mease, creating a larger river that now flows through a broad floodplain. These consisted of V shaped alignments of stakes; wattle panels and a large wicker trap and demonstrate that passive fishing techniques were in use on the river. [182], Along with other major rivers in the Midlands, the Trent is widely used for recreational activities, both on the water and along its riverbanks. Downstream, the inflow of cleaner water from the Dove and then the Derwent meant that conditions improved enough to allow recreational coarse fishing in the lower reaches. Its source is in Staffordshire on the southern edge of Biddulph Moor. Today, exploring the lovely old riverside buildings provides a great family day out. There were corresponding increases in dissolved oxygen, an indicator of a healthy river environment. key towns of river bannmr patel neurosurgeon cardiff 27 februari, 2023 . These floods revealed the need for a tidal protection scheme, which would cope with the flows experienced in 1947 and the tidal levels from 1954, and subsequently the floodbanks and defences along the lower river were improved to this standard with the works being completed in 1965. Some 20,000 acres (81km2; 31sqmi) were flooded for a period of over three weeks.[23][81][82]. Its source is in Staffordshire, on the southern edge of Biddulph Moor. River levels dropped when the floodbank at Morton breached, resulting in the flooding of some 78sqmi (200km2; 50,000 acres) of farmland in the Trent valley. [27] At the end of the Wolstonian Stage (c. 130,000 years ago) a mass of stagnant ice left in the Vale of Belvoir caused the river to divert north along the old Lincoln river, through the Lincoln gap, along what is now the course of the Witham. Large parts of the city and surrounding areas were flooded with 9,000 properties and nearly a hundred industrial premises affected some to first floor height. For example, Birmingham lies at the upper end of the Tame, and Leicester is located towards the head of the Soar. [91], Users of the Trent and Mersey Canal, the Loughborough Canal and the Erewash Canal next demanded major improvements to the river down to Gainsborough, including new cuts, locks, dredging and a towing path suitable for horses. Contained within these terraces is evidence of the mega fauna that once lived along the river, the bones and teeth of animals such as the woolly mammoth, bison and wolves that existed during colder periods have all been identified. [37], Sand, gravels and alluvium deposits that overlie the mudstone bedrock occur almost along the entire length of the river, and are an important feature of the middle and lower reaches, with the alluvial river silt producing fertile soils that are used for intensive agriculture in the Trent valley. The Trent is the third-longest river in the United Kingdom. It was a Viking winter camp. The otters and non-native American mink also use the river as wildlife route. and the town was also a key place on long-distance routeways . [11][12], It then reaches the town of Gainsborough with its own Trent Bridge. This combination can produce a water-logged catchment that can respond rapidly in terms of runoff, to any additional rainfall. He suggested that dredging, deepening, and restricting the width of the channel could make significant improvements to the navigable depth, although cuts would be required at Wilford, Nottingham bridge and Holme. Tolls decreased from 11,344 (equivalent to 1,060,000 in 2021),[93] during 1839 to 3,111 (equivalent to 310,000 in 2021),[93] in 1855. At Newark, the last bridge on the Trent until modern times, the bridge was rebuilt in 1775. [54][55][56], Another meteorological risk, although one that occurs less often, is that related to the rapid melting of snow lying in the catchment. The Trent drains a large portion of south-central Ontario, including most of the Kawartha Lakes and their supplying watersheds. Further north at Littleborough is the site of the Roman town of Segelocum, where a Roman road once crossed the river. The lower river occupies a peaty depression in the . [11], Downstream of Nottingham it passes Radcliffe on Trent, Stoke Bardolph and Burton Joyce before reaching Gunthorpe with its bridge, lock and weir. [24], During the Pleistocene epoch (1.7 million years ago), the River Trent rose in the Welsh hills and flowed almost east from Nottingham through the present Vale of Belvoir to cut a gap through the limestone ridge at Ancaster and thence to the North Sea. River Trent has been used as a migration corridor for the wading birds and wildfowl. [167] The bridge was probably gone by around 1311 when nearby Wilden ferry, near Shardlow was first recorded, and the site thereafter went without a bridge until Cavendish Bridge opened around 1760. Intensive arable farming of cereals and root vegetables, chiefly potatoes and sugar beet occurs in the lowland areas, such as the Vale of Belvoir and the lower reaches of the Trent, Torne and Idle. key towns of river bann. Efird Commercial Real Estate. The river is known for dramatic flooding after storms and spring snowmelt, which in the past often caused the river to change course. elephant jokes from the 60's . After the confluence with the Swarbourn, it passes Alrewas and reaches Wychnor, where it is crossed by the A38 dual carriageway, which follows the route of the Roman Ryknild Street. The medieval bridges of Burton and Nottingham survived relatively intact until the 1860s, when both were replaced and demolished. In quantity equals not one of yours: The Trent and Tame River Valleys Futurescape includes rivers, farmland and wetlands,. The complex of three bridges provides evidence of attempts to keep a crossing open over slightly more than two hundred years from 1097, with three bridges constructed on the same site but felled by scouring, floods and course migration of the river to the south eroding the bridgehead. [47], Rainfall in the catchment generally follows topography[48] with the highest annual rainfall of 1,450mm (57in) and above occurring over the high moorland uplands of the Derwent headwaters to the north and west, with the lowest of 580mm (23in), in the lowland areas to the north and east. [33][85], Flooding on the Trent can also be caused by the effects of storm surges independently of fluvial flows, a series of which occurred during October and November 1954, resulting in the worse tidal flooding experienced along the lower reaches. Flowing for 143 miles, the vast waterway is the fourth-longest in the UK and its history is . [9] A traditional but almost certainly wrong opinion is that of Izaak Walton, who states in The Compleat Angler (1653) that the Trent is " so called from thirty kind of fishes that are found in it, or for that it receiveth thirty lesser rivers. These cities lie on the river Trent: Stoke-on-Trent. [154], By the 1970s the Trent was regarded as 'one of the most productive rivers in the British Isles'. The river in Burton is crossed by a number of bridges including the ornate 19th-century Ferry Bridge that links Stapenhill to the town. The river is known for dramatic flooding after storms and spring snowmelt, which in past times often caused the river to . It meanders almost 190 miles through this Futurescape, from the Tame in the heart of the Midlands to the Humber. Henry Hotspur's speech complaining about the river has been linked to the meanders near West Burton,[23] however, given the wider context of the scene, in which conspirators propose to divide England into three after a revolt, it is thought that Hotspur's intentions were of a grander design, diverting the river east towards the Wash such that he would benefit from a much larger share of the divided Kingdom. [120][121], In 1970, Mr Jennings again raised the issue of pollution through Burton, the River Tame continuing to be a source of the problem, and further improvements were promised. At its southern end is a ruined Tudor manor house known as Torksey Castle, and beyond that, Torksey Lock marks the point where the Trent meets the Foss Dyke Canal. [45], The topography, geology and land use of the Trent catchment all have a direct influence on the hydrology of the river. [67][68] Such conditions occurred in February 1977, with widespread flooding in the lower reaches of the Trent when heavy rain produced a peak flow of nearly 1,000m3/s (35,000cuft/s) at Nottingham. Lord Paget seems to have funded the work privately, building locks at King's Mill and Burton Mills and several cuts and basins. The river frontage in the town is lined with warehouses, that were once used when the town was an inland port, many of which have been renovated for modern use. These levels extend across the Trent valley, and include the lower reaches of the Eau, Torne and Idle. [73][74], The Trent is widely known for its tendency to cause significant flooding along its course, and there is a well documented flood history extending back for some 900 years. There are other big events each year like the Oxford and Cambridge University Boat Races . The Aegir occurs when a high spring tide meets the downstream flow of the river. The bridges at Wolseley, Wychnor and the main span at Swarkestone were all destroyed. The resulting surge overtopped the flood defences in the area near Keadby and Burringham, flooding 50 properties. [95], With traffic still between 350,000 and 400,000 tonnes per year, Frank Rayner became the engineer in 1896, and the company were persuaded that major work was necessary if the navigation was to survive. [23][77], The largest known flood was the Candlemas flood of February 1795, which followed an eight-week period of harsh winter weather, rivers froze which that meant mills were unable to grind corn, and then followed a rapid thaw. [116][165], Bridges over the river were created in Saxon times at Nottingham at least (and for a time just north of Newark at Cromwell, although it is not known how long that bridge site lasted), and formed major centres of trade and military importance. [117] Angling clubs in Burton used the Dove or local lakes for fishing, as the Trent through the town was absent of any fish. Some of the earliest floods can be assessed by using Spalford bank as a substitute measure for the size of a particular flood, as it has been estimated that the bank only failed when flows were greater than 1,000m3/s (35,000cuft/s), the bank was also breached in 1403 and 1795. The programme of monitoring also extended to taking biological samples, and one of the first biotic indices used for assessing the ecological rather than the chemical quality of rivers was developed by the local river board in the 1960s. And cuts me from the best of all my land Sir Ernest Jardine, who as vice-chairman had partly funded the first lock at Cromwell in 1908, died in 1947, and the company ceased to exist in 1948 when the waterways were nationalised. [41], The lower sequences of these terraces have been widely quarried for sand and gravel, and the extraction of these minerals continues to be an important industry in the Trent Valley, with some three million tonnes of aggregates being produced each year. Traffic increased from 620,000 tonnes during 1951 to 1,017,356 tonnes during 1964, but all of this was below Nottingham. The Trent River is a river in southeastern Ontario which flows from Rice Lake to empty into the Bay of Quinte on Lake Ontario.This river is part of the Trent-Severn Waterway which leads to Georgian Bay.The river is 90 kilometres (56 mi) long. The flood marks at Girton show that this flood was only 4 inches (100mm) lower than that of 1795, when the village was flooded to a depth of 3 feet (0.91m). Using invertebrates as an indicator of pollution levels, it was appropriately named the Trent Biotic index. The upper Bann rises in the Mourne Mountains and flows northwest to Lough (lake) Neagh. A survey in 2003 showed a doubling in the number of sites where evidence, such as spraints and footprints of these elusive animals were found. [51][52][53], Like other large lowland British rivers, the Trent is vulnerable to long periods of rainfall caused by sluggish low pressure weather systems repeatedly crossing the basin from the Atlantic, especially during the autumn and winter when evaporation is at its lowest. It shall not wind with such a deep indent, [119], John Jennings, the local MP for Burton highlighted these problems in a speech to the House when he stated in 1956, that as in previous years the river had been declared unsafe for swimming on advice from the medical officer, and how its unhealthy condition affected a local rowing club.
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