what are the key towns of the river trent

[23][75][76], One of the earliest recorded floods along the Trent was in 1141, and like many other large historical events was caused by the melting of snow following heavy rainfall, it also caused a breach in the outer floodbank at Spalford. I'll have the current in this place damm'd up; 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. In some areas, successive layers of peat were built up above the lacustrine deposits during the Holocene period, which created lowland mires such as the Thorne and Hatfield Moors. Nottingham seems to have been the ancient head of navigation until the Restoration, due partly to the difficult navigation of the Trent Bridge. [94], The arrival of the railways resulted in significant change for the company. [143], Improvements in water quality and subsequent fish stocks, in combination with the ban on the use of certain persistent pesticides have meant that otters have now returned to the Trent system, having been absent as recently as the 1980s. Not only do these provide baseflows to the major tributaries, the groundwater is an important source for public water supply. [89], In 1748, merchants from Nottingham attempted to end this monopoly by landing goods on the banks and into carts, but Fosbrooke used his ferry rope to block the river, and then created a bridge by mooring boats across the channel, and employing men to defend them. The last bridge over the river is at Keadby where it is joined by both the Stainforth and Keadby Canal and the River Torne. Tolls were increased, and a committee recommended improvements to the river. [151][184][189][190] The first person to swim the entire swimmable length of the Trent was Tom Milner, who swam 139 miles (224km) over nine days in July 2015. It flows through the bustling city of Nottingham, the market town of Newark and the rural Trent Vale. This may explain the presence of the Romano-British element rid (cf. The river is known for dramatic flooding after storms and spring snowmelt, which in the past often caused the river to change course. Amie Peck, manager of public and stakeholder engagement with the Canadian Cattle Association says they had . Domestic effluent and polluting discharges from the metal working industries in the upper reaches, combined to affect the whole length of the tributary River Tame. [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. The River Trent was a major working river until after the Second World War. The flood defences in Nottingham that protect 16,000 homes and those in Burton where they prevent 7,000 properties from flooding were reassessed after this flood, and were subsequently improved between 2006 and 2012.[84][88]. [13][14][15] At West Stockwith the Trent is joined by the Chesterfield Canal and the River Idle and soon after enters Lincolnshire fully, passing to the west of Scunthorpe. A plan to build six locks between Cromwell and Holme, and to dredge this section to ensure it was 60 feet (18m) wide and 5 feet (1.5m) deep was authorised by an Act of Parliament obtained in 1906. River Trent through Nottingham. At Colwick near Nottingham, the average flow rises to 83.8m3/s (2,960cuft/s), due to the combined inputs of the other major tributaries namely the Dove, Derwent and Soar. However, for practical purposes, navigation above the southern terminus of the Trent and Mersey Canal (at Shardlow) is conducted on the canal, rather than on the river itself. The river channel links the remaining, but fragmented wetland areas and nature reserves, providing a refuge for native and migrant species. konstantin guericke net worth; xaverian brothers high school nfl players; how is the correct gene added to the cells; hong kong supermarket flyer calgary; ben fogle: new lives in the wild do they get paid; In 2000 similar conditions occurred again, with above average rainfall in the autumn being followed by further rainfall, producing flood conditions in November of that year. Welsh rhyd, "ford") in various place names along the Trent, such as Hill Ridware, as well as the Old Englishderived ford. [11], The now tidal river meanders across a wide floodplain, at the edge of which are located riverside villages such as Carlton and Sutton on Trent, Besthorpe and Girton. This combination can produce a water-logged catchment that can respond rapidly in terms of runoff, to any additional rainfall. [94], The aim of the improvements was to increase the minimum depth from 2 feet (0.6m) to 3 feet (0.9m). Rugeley. During lower flows the Trent and its tributaries are heavily influenced by effluent returns from sewage works, especially the Tame where summer flows can be made up of 90% effluent. 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. Downstream of the reservoir it passes through Stoke-on-Trent and merges with the Lyme, Fowlea and other brooks that drain the six towns of the Staffordshire Potteries to become the River Trent. This can be a result of a sudden rise in temperature after a prolonged cold period, or when combined with extensive rainfall. [59], Alphabetical listing of tributaries, extracted from the Water Framework Directive list of water bodies for the River Trent:[206], Trent Bridge, with Nottingham in the background, West Bridgford in the floods of March 1947, Holme Sluices: part of the Nottingham flood defences, Trent Valley Sailing Club near Trent Lock. There is thought to be a complex succession of at least six separate gravel terrace systems along the river, deposited when a much larger Trent flowed through the existing valley, and along its ancestral routes through the water gaps at Lincoln and Ancaster. One effect of this pollution was that the upper and middle reaches were completely devoid of any fish life.[115]. They have also now been sighted at locations such as Wolseley, Willington, and Attenborough. [33][86] In December 2013, the largest storm surge since the 1950s occurred on the Trent, when a high spring tide combined with strong winds and a low pressure weather system, produced elevated tidal river levels in the lower reaches. 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. [134], Additional nature conservation areas were created beside the river in the 20th century, when a number of disused gravel pits, were rehabilitated as nature reserves. Wilmington, North Carolina, United States. [20][21] The river's propensity to change course is referred to in Shakespeare's play Henry IV, Part 1: Methinks my moiety, north from Burton here, This combined with the nearby supplies of fuel in the form of coal from the Nottinghamshire and Yorkshire coalfields, and the existing railway infrastructure meant that a string of twelve large power stations were originally constructed along its banks. At certain times of the year, the lower tidal reaches of the Trent experience a moderately large tidal bore (up to 5 feet [1.5m] high), commonly known as the Trent Aegir (named after the Norse sea god). [36][37], Downstream of Armitage the solid geology is primarily Mercia Mudstones, the course of the river following the arc of these mudstones as they pass through the Midlands all the way to the Humber. The only time it was settled was in the winter of 872 to 873 and, as a result, we can be pretty sure that all these finds date from that winter. [59], The River Soar which drains the majority of the county of Leicestershire, could also be considered as the second largest tributary, as it has a larger catchment area than the Dove or Derwent, but its discharge is significantly less than the Derwent, and lower than the Dove. The National Watersports Centre at Holme Pierrepont, near Nottingham combines facilities for many of these sports, including rowing, sailing and whitewater canoeing. [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. [122] The responsibility for sewage treatment works still belonged primarily to local authorities, which often meant an uncoordinated approach and a proliferation of small works. Beneath the alluvium are widespread deposits of sand and gravel, which also occur as gravel terraces considerably above the height of the current river level. Due to the size of the flood and the ice entrained in the flow, nearly every bridge along the Trent was badly damaged or washed away. These include the Sherwood sandstones that occur beneath much of eastern Nottinghamshire, the Permian Lower Magnesian limestone and the carboniferous limestone in Derbyshire. A loan from Nottingham Corporation and a grant from the Unemployment Grants Committee enabled the company to rebuild Newark Nether lock, which was opened on 12 April 1926. The Trent Aegir tidal bore. [44], During the end of the last Devensian glacial period the formation of Lake Humber in the lowest reaches of the river, meant that substantial lake bed clays and silts were laid down to create the flat landscape of the Humberhead Levels. Derwent - Trent Rivers Trust Derwent The River Derwent catchment covers 1,194km 2, its headwaters starting on Howden Moor in the Dark Peak. [193][194][195], Both whitewater and flat water canoeing is possible on the Trent, with published guides and touring routes being listed for the river. [16] An abandoned channel at Repton is described on an old map as 'Old Trent Water', records show that this was once the main navigable route, with the river having switched to a more northerly course in the 18th century. "[10], The Trent rises within the Staffordshire Moorlands district, near the village of Biddulph Moor, from a number of sources including the Trent Head Well. There are also a number of clubs that sail on the open water that has been created as a result of flooded gravel workings which include Hoveringham, Girton, and Attenborough. Agreement could not be reached, and so William Jessop was asked to re-assess the situation. [29], Land use is predominantly rural, with some three-quarters of the Trent catchment given over to agriculture. What is the River Trent used for? The resulting surge overtopped the flood defences in the area near Keadby and Burringham, flooding 50 properties. From its source in the Plynlimon Mountains in west Wales, the River Severn flows through the West Midlands counties of Shropshire, Worcestershire and Gloucestershire Wales (Powys) Llanidloes(165m above sea level) Caersws Newtown(103m above sea level) Welshpool(70m above sea level) England Shropshire Shrewsbury(county town and historic city) [125][144][145][146] Seals have been reported up to near the head of the tidal section at Newark. The mudstones are not exposed by the bed of the river, as there is a layer of gravels and then alluvium above the bedrock. [105] The funnel shape of the river mouth exaggerates this effect, causing a large wave to travel upstream as far as Gainsborough, Lincolnshire, and sometimes beyond. As water quality improved from the 1960s onwards, fish numbers recovered, and recreational coarse fishing became more popular. Hayne subsequently scuppered a barge in King's Lock, and for the next eight years goods had to be transhipped around it. These lower reaches are protected from tidal flooding by a series of floodbanks and defences. This led to increased investment, the closure of older and smaller works, with sewage treatment being combined at larger modern works such as Strongford and Minworth. 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. Later improvements such as the series of purification lakes that were constructed on the Tame in the 1980s, which allowed contaminated sediment to settle out from the river, also reduced pollution levels, and lessened the impact of first flush runoff events in the lower Tame and the middle Trent. 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