what are the key towns of the river trentwhat are the key towns of the river trent
[92], The first improvement of the lower river was at Newark, where the channel splits into two. 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. [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. Lichfield. 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. Some traces of the former division remain: the Trent marks the boundary between the provinces of two English Kings of Arms, Norroy and Clarenceux. [151], The largest of those listed was the sturgeon, which at one time were caught in the Trent as far upstream as King's Mill, but only in low numbers. https://en.wikipedia.org/w/index.php?title=River_Trent&oldid=1132366164, This page was last edited on 8 January 2023, at 14:59. [47][148] More definitive finds from the medieval period were also found at this site and near Colwick. [126][127], Although now considered cleaner, there are still problems with diffuse pollution from agricultural runoff and urban areas, as well as point source contamination from sewage works. [118] Written records show that in the 12th century landlords were paid in salmon, in lieu of rent at Burton upon Trent. [11], Downstream of Keadby the river progressively widens, passing Amcotts and Flixborough to reach Burton upon Stather and finally Trent Falls. To the north of Farndon, beside the Staythorpe Power Station the river splits, with one arm passing Averham and Kelham, and the other arm, which is navigable, being joined by the Devon before passing through the market town of Newark-on-Trent and beneath the town's castle walls. The River Trent is the third-longest river in the United Kingdom. Raising finance was difficult, but some was subscribed by the chairman and vice-chairman, and construction of Cromwell Lock began in 1908. [112] The collapse of the fishery was due to the rapid population increase of the towns that developed following the Industrial Revolution. 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. [115], The Tame pollution also reached the Trent as well, with one of the worse affected reaches being that downstream of the confluence with the Tame through Burton, this being exacerbated by its late introduction of sewage treatment, and the substantial wastewater arising from the breweries in the town. At 188 by 30 feet (57.3 by 9.1m), Cromwell lock could hold a tug and three barges, and was opened on 22 May 1911. The Travellers' Dictionary of Quotations: Who Said What, About Where? Many of the largest historical floods were caused by snowmelt, but the last such episode occurred when the bitter winter of 1946-7 was followed by a rapid thaw due to rain in March 1947 and caused severe flooding all along the Trent valley. [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. Recorded at 1230hrs on 8 November 2000 highest discharge since 1 September 1958. the polluted state of the Trent is a terror to Trentham. They have also now been sighted at locations such as Wolseley, Willington, and Attenborough. [54][57], At the other extreme, extended periods of low rainfall can also cause problems. Later, in 1699, the baron William Paget (Lord Paget), who owned coal mines and land in the area, obtained an Act of Parliament to extend navigation up to Fleetstones Bridge, Burton, despite opposition from the people of Nottingham. 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). [118], In the 17th century Izaak Walton described the River Trent as 'One of the finest rivers in the world and the most abounding with excellent salmon and all sorts of delicate fish. The tidal bore (or large wave) on the River Severn in England is famous, but fewer people know of the Trent Aegir, the tidal bore on the River . [23], On 1718 March 1947 the Trent overtopped its banks in Nottingham. The last bridge over the river is at Keadby where it is joined by both the Stainforth and Keadby Canal and the River Torne. 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. 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. It flows through and drains the North Midlands. 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. [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. [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. "[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. [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. [147], Evidence of fishing along the Trent can be traced back to the Neolithic period, with the possible remnants of a fish weir discovered in the abandoned river channels at Hemington. There is a canoe slalom course at Stone, a purpose built 700m (2,300ft) artificial course at Holme Pierrepont, and various weirs including those at Newark and Sawley are all used for whitewater paddling. These villages include West Stockwith and East Stockwith, Owston Ferry and East Ferry, and West Butterwick and East Butterwick. As it enters the city, it passes the suburbs of Beeston, Clifton and Wilford; where it is joined by the Leen. [158], Salmon, a species that became virtually extinct due to historic pollution, have been progressively reintroduced on the tributaries since 1998, with thousands of salmon parr being released into the Dove and its tributary the Churnet each year. William Jessop performed the survey, assisted by Robert Whitworth, and they published their report on 8 July 1793. The river now flows north-east below the Toot and Trent Hills before reaching Hazelford Ferry, Fiskerton and Farndon. [29][30], A distinctive feature of the catchment is the marked variation in the topography and character of the landscape, which varies from the upland moorland headwaters of the Dark Peak, where the highest point of the catchment is the Kinder Scout plateau at 634 metres (2,080ft); through to the intensively farmed and drained flat fenland areas that exist alongside the lower tidal reaches, where ground levels can equal sea level. [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. 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. 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 new Ferry Bridge was opened in 1889, although it needed the financial support of the brewer and philanthropist Michael Bass to pay for the construction, and later in 1898 to purchase the existing ferry rights so that it became free of tolls. [132][135] One of the most important of these is Attenborough Nature Reserve, a 226-hectare (560-acre) Site of Special Scientific Interest (SSSI) which is visited by wildfowl such as Eurasian wigeon and common teal. [2] Throughout its course, the river mostly flows through the Peak District and its foothills. John Jennings MP for Burton-upon-Trent, 1956. The UK's third longest river, the Trent, touches the lives of more than six million people. The Nottingham and Gainsborough Railway offered 100 per share during 1845, but this was rejected. Whilst this is not unique for an English river, it does mean that there is an ongoing legacy of issues relating to urban runoff, pollution incidents, and effluent dilution from sewage treatment, industry and coal mining. The two arms recombine at Crankley Point beyond the town, where the river turns due north to pass North Muskham and Holme to reach Cromwell Weir, below which the Trent becomes tidal. These cities lie on the river Trent: Stoke-on-Trent. The largest of these is the River Tame, which contributes nearly a quarter of the total flow for the Trent, with the other significant tributaries being the Derwent at 18%, Soar 17%, the Dove 13%, and the Sow 8%. [31][32][33], Elsewhere there is a distinct contrast between the open limestone areas of the White Peak in the Dove catchment, and the large woodland areas, including Sherwood Forest in the Dukeries area of the Idle catchment, the upland Charnwood Forest, and the National Forest in the Soar and Mease drainage basins respectively. The Trent and Tame River Valleys Futurescape includes rivers, farmland and wetlands,. The catchment is located between the drainage basins of the Severn and its tributary the Avon to the south and west, the Weaver to the north-west, the tributaries of the Yorkshire Ouse to the North and the basins of the Welland, Witham and Ancholme to the east. River Great Ouse. '[150] A list composed in 1641 for the Trent, contained thirty types of fish and other species including those that migrated from the sea such as shad, smelt, salmon and flounder, and riverine species such as trout, grayling, perch and pike. For example, the administration of royal forests was subject to a different justice in eyre north and south of the river, and the jurisdiction of the medieval Council of the North started at the Trent. More improvements followed between 1957 and 1960. The engineer for the Manchester Ship Canal, Sir Edward Leader Williams, was commissioned to survey the river, while negotiations with the North Staffordshire Railway, who owned the Trent and Mersey Canal and had maintained its viability, ensured that some of the clauses from previous Acts of Parliament did not prevent progress. [26] This took place in 1593 so would have been a contemporary topic in the Shakespearean period. 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. In a new channel, fair and evenly; During a following glaciation (Devensian, 70,000BC) the ice held back vast areas of water called Glacial Lake Humber in the current lower Trent basin. This resulted in the release of raw sewage and the chemical into the river, killing thousands of fish, and posing a health risk to river users as far south as Burton. 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. 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. The current state of knowledge and proposals for future research", "Cavendish Bridge Conservation Area Appraisal and Study", "Coal-Fired Power Plants in East England & the Midlands", "Strategic Priorities for Water Related Recreation in the Midlands", "Burton-upon-Trent: Social and cultural activities", "Tom Milner swims 139 miles in nine days", "Tom Milner completes River Trent Challenge", "National Water Sports Centre About Us", "Report on the investigation of Nottingham Princess striking Trent Bridge Nottingham", "Water Framework Directive Surface Water Classification Status and Objectives 2012 csv file", Photographs along the Trent in Nottingham from Nottingham21, Predictive Modelling of Multi-Period Geoarchaeological Resources at a River Confluence. Rugeley. The river continues north-east, passing the village of Walton-on-Trent until it reaches the large town of Burton upon Trent. [153], The effluent and industrial pollution of the early 20th century, led to a rapid decline in fish stocks, large stretches of the river became fishless and species such as salmon almost disappeared. [114], This was a particular problem in Stoke-on-Trent and the growing towns of the Potteries. [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. River Bann, Irish An Bhanna, river, the largest in Northern Ireland, falling into two distinct parts. Such was the case at Willington, Gunthorpe and Gainsborough. [17] Farther downstream at Hemington, archaeologists have found the remains of a medieval bridge across another abandoned channel. Wilmington, North Carolina, United States. 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