Downstream of Dunham the river passes Church Laneham and reaches Torksey, where it meets the Foss Dyke navigation which connects the Trent to Lincoln and the River Witham. [11], Downstream of Keadby the river progressively widens, passing Amcotts and Flixborough to reach Burton upon Stather and finally Trent Falls. The upper Bann rises in the Mourne Mountains and flows northwest to Lough (lake) Neagh. These cities lie on the river Trent: Stoke-on-Trent. The Trent Aegir tidal bore. These include recreational water activities, and once rehabilitated, as nature reserves and wetlands. 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. 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. The river is known for dramatic flooding after storms and spring snowmelt, which in the past often caused the river to change course. The lower river occupies a peaty depression in the . Some 20,000 acres (81km2; 31sqmi) were flooded for a period of over three weeks.[23][81][82]. 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. Below Cromwell lock, the Trent is tidal, and therefore only navigable by experienced, well-equipped boaters. 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. Flows measured at Nottingham were exceptionally low by the end of August, and were given a drought return period of greater than one hundred years. These levels extend across the Trent valley, and include the lower reaches of the Eau, Torne and Idle. The River Great Ouse meanders through some of the prettiest towns and villages in Cambridgeshire. The north part from the south, on my so either sides, [176], The tall chimneys and concave shaped cooling towers of the many power stations are a dominant and familiar presence within the open landscape of the Trent valley, which has been widely used for power generation since the 1940s. [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. 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. 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. He reported that they could be treacherous to the unwary, since there were few gauges to show if the river had become too deep to cross, and that they were rarely used except by locals. The residents of the town wanted to increase the use of the branch nearest to them, and so an Act of Parliament was obtained in 1772 to authorise the work. 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. In 1683 the same bridge was partially destroyed by a flood that also meant the loss of the bridge at Newark. 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. 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. River Trent, courtesy of Richard Croft Free guides for fun days out Looking for a perfect place to picnic, relax, think, run, walk your dog and more, all for free? [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. 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. It also incorporates the iconic Howden, Derwent and Ladybower Reservoirs. [95], During the early 1930s, the company considered enlarging the navigation above Nottingham, in conjunction with improvements to the River Soar Navigation, between Trent Lock and Leicester. [159] Returning adult salmon have been seen leaping over weirs on the river[159] and in 2011 a large salmon weighing over 10 pounds (4.5kg) was caught at an undisclosed location, and was 'thought to be the biggest caught on the Trent in the last thirty years'.[160]. 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. As they were a source of income, they were recorded in the Domesday Book at a number of locations including Weston on Trent and Fiskerton, both of which were still in operation in the middle of the 20th century. [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. . The last act of the directors was to pay a 7.5 per cent dividend on the shares in 1950. "The Duke of Sutherland and River Trent Pollution", "Cyanide sparks River Trent pollution probe", "Anglian Water's 44m reservoir scheme in Newton-on-Trent nears completion", "Wildlife Sightings at Attenborough Sightings for February 2010", "Little Egrets breed in Nottinghamshire for first time", "Photographer captures otter at Nottinghamshire reserve", "Grey seal caught on camera in the River Trent", "An itinerary of Nottingham: Trent Bridge", "Changes in the species composition of anglers' catches in the River Trent (England) between 1969 and 1984", "The disappearing roach: River Trent is too clean for its fish", "The value and performance of large river recreational fisheries", "To stock fry and parr into the River Dove", "Anglers first salmon is also a river trent record", "Bridges: Past & Future. [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. elephant jokes from the 60's . [178] At one time these sites provided a quarter of the electricity needs of the UK, giving rise to the epithet 'Megawatt Valley'. Today, exploring the lovely old riverside buildings provides a great family day out. Commercial carrying above Nottingham ceased during the 1950s, to be replaced by pleasure cruising. It flows through and drains most of the metropolitan central and northern Midlands south and east of its source north of Stoke-on-Trent. Historical archives often record details of the bridge repairs that followed floods, as the cost of these repairs or pontage had to be raised by borrowing money and charging a local toll. Plans for new larger locks at Beeston and Wilford were abandoned when the Trent Catchment Board opposed them. This may explain the presence of the Romano-British element rid (cf. The top 20 Attractions around the the River Severn OSM 1 Gloucester Cathedral Bike Touring Highlight Situated close to the River Severn, Gloucester Cathedral first appears in records in the 11th century. Agreement could not be reached, and so William Jessop was asked to re-assess the situation. [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. 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. The work was completed by October 1773, and the separate tolls remained in force until 1783, when they were replaced by a one-shilling (5p) toll whichever channel the boats used. Wading birds such as Eurasian oystercatcher and great bittern have also been observed at the reserve; as have kingfishers, reed warblers and water rails. The total length is 80 miles (129 km). Trento, Latin Tridentum, German Trient, English Trent, city, Trentino-Alto Adige/Sdtirol regione (region), northern Italy. The use of a maritime pilot on the Trent is not compulsory for commercial craft, but is suggested for those without any experience of the river. [114], Although he provided land for a sewage works nearby at Strongford, the problems continued such that in 1905 the Levenson-Gower family left Trentham altogether and moved to their other properties, including Dunrobin Castle in Scotland. Polluting substances such as ammonia showed a reduction, as did the biochemical oxygen demand, an indicator of the contamination present in the river. [157], Recreational fishing is still popular, although anglers no longer line the banks as they once did. [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. It is then joined by other small streams to form the Head of Trent, which flows south, to the only reservoir along its course at Knypersley. 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 most important in terms of the river are the extensive sandstone and limestone aquifers that underlie many of the tributary catchments. The Trent drains a large portion of south-central Ontario, including most of the Kawartha Lakes and their supplying watersheds. Much of the river's route, with the exception of the city of Derby, is rural. key towns of river bann. [67][68] 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. Having taken over responsibility for the waterway, the Transport Commission enlarged Newark Town lock in 1952, and the flood lock at Holme was removed to reduce the risk of flooding in Nottingham. 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. [40] Once worked out, the remaining gravel pits which are usually flooded by the relatively high water table have been reused for a wide variety of purposes. Newark was once an important inland port on the mighty River Trent. Crossing a wide flood plain, the bridge is almost one mile (1.6km) long, a laborious project to allow flood waters to pass under it. The River Tamar is situated in south west England and forms a natural border between the counties of Devon and Cornwall. 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. Due to the relatively small size of the Trent and its tributaries such as the Fowlea Brook, which drained these towns, the river and brooks were unable to dilute the inflow of domestic sewage and soon became overwhelmed and badly polluted. In places, however the mudstones do form river cliffs, most notably at Gunthorpe and Stoke Lock near Radcliffe on Trent, the village being named after the distinctive red coloured strata. [128] The improvements that have taken place mean that the Trent can be used for public water consumption. Wilmington, North Carolina, United States. 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