[177][179], The three largest remaining coal-fired stations at Ratcliffe, Cottam and West Burton still use domestic coal supplies, although this is now being replaced by imported coal brought by ship from abroad. [58], The river's flow is measured at several points along its course, at a number of gauging stations. [95], Increased running costs after the First World War could not be met by increasing the tolls, as the company had no statutory powers to do so, and so suggested that the Ministry of Transport should take over the navigation, which they did from 24 September 1920. Hayne's lease expired in 1762, and Lord Paget's son, the Earl of Uxbridge, gave the new lease to the Burton Boat Company. [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. The upper Bann rises in the Mourne Mountains and flows northwest to Lough (lake) Neagh. [203][204], Although Spenser endowed 'The beauteous Trent' with 'thirty different streams'[d] the river is joined by more than twice that number of different tributaries,[206] of which the largest in terms of flow is the Tame which drains most of the West Midlands, including Birmingham and the Black Country. [95], Although commercial use of the river has declined, the lower river between Cromwell and Nottingham can still take large motor barges up to around 150 feet (46m) in length[90] with a capacity of approx 300 tonnes. February27February 27, 2023. key towns of river bann. Cities and towns on or close to the river include: Stoke-on-Trent Stone Rugeley Lichfield Burton upon Trent Castle Donington Derby Long Eaton Beeston Nottingham Newark-on-Trent Rampton Dunham Bridge - A57 Swing Toll bridge Gainsborough Gunness Scunthorpe Read more about this topic: River Trent Famous quotes containing the word places: The documentary "Guardians of the Grasslands" has now evolved into an online game for students in Grade 7 to 10. The river now flows north-east below the Toot and Trent Hills before reaching Hazelford Ferry, Fiskerton and Farndon. It shall not wind with such a deep indent, The river is known for dramatic flooding after storms and spring snowmelt, which in the past often caused the river to change course. 109. . Throughout history, the river has been a main route for trade and travel. Mills were important locations for fish and eel traps, the eels being caught during quill time between mid-August and early September. [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. [49] Rainfall totals in the Tame are not as high as would be expected from the moderate relief, due to the rain shadow effect of the Welsh mountains to the west, reducing amounts to an average of 691mm (27.2in) for the tributary basin. [83] In Newark the water was deep enough to allow four grammar school boys to row across the countryside to Kelham. 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. Although not quite as large as 1795 this flood devastated many places along the river, at Burton upon Trent much of the town was inundated, with flooded streets and houses, and dead animals floating past in the flood. [114], This was a particular problem in Stoke-on-Trent and the growing towns of the Potteries. 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. [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. Rainfall is Annual Average 196190 for the catchment to the Gauging Station, Tributary names from Ordnance Survey maps added where list amalgamated river reaches, River Order 1 being closest to Trent Falls, Ripper, S. and Cooper L.P., 2009, The Hemington Bridges: "The Excavation of Three Medieval Bridges at Hemington Quarry, Near Castle Donington, Leicestershire", Leicester Archaeology Monograph, Holme Pierrepont National Watersports Centre, National Watersports Centre at Holme Pierrepont, "Historical channel-floodplain dynamics along the River Trent", "Midlands Catchment Flood Management Plans", "University of Wales Trinity Saint David", "The Trent Valley: palaeochannel mapping from aerial photographs", "Stanhope, Sir Thomas 1540-96 of Shelford", "River Trent Catchment Flood Management Plan Chapter 2", "Environment Agency What's in your Backyard", "River Trent Catchment Flood Management Plan Chapter 3", "Geological Evolution of Central England with reference to the Trent Basin and its Landscapes", "The BGS Lexicon of Named Rock Units Gunthorpe member", "The Lower and Middle Palaeolithic Occupation of the Middle and Lower Trent Catchment and Adjacent Areas, as Recorded in the River Gravels used as Aggregate Resources", "River Trent: Archaeology and Landscape of the Ice Age", "The BGS Lexicon of Named Rock Units - Trent Valley Formation", "River Trent Catchment Flood Management Plan Chapter 2 Part1", "River Trent Catchment Flood Management Plan Scoping Report, Part 5", "28095-Tame at Hopwas Bridge Spatial Data Rainfall", "Climate tables Climate region:England 1961-90", "Hi flows UK AMAX Data for: Trent at Colwick (28009)", "1947 U.K. River Floods:60-Year Retrospective", "Hi Flows UK AMAX Data for: Trent at Stoke (28040)", "Hi Flows UK AMAX Data for: Trent at Great Haywood (28006)", "Hi Flows UK AMAX Data for: Trent at Yoxall (28012)", "Hi Flows UK AMAX Data for: Trent at Drakelow (28019)", "Hi Flows UK AMAX Data for: Trent at Shardlow (28007)", "Hi Flows UK AMAX Data for: Trent at North Muskham (28022)", "Willington C Gas Pipeline Environmental Statement, Volume 1, Chapter 7, Hydrology, Hydrogeology and Flood Risk Assessment", "Alluvial Archaeology in the Vale of York", "Chesterfield Canal Trust History of the Restoration", "Nottingham Left Bank Flood Alleviation Scheme Flood Risk Assessment", "Reassessing flood frequency for the River Trent through the inclusion of historical flood information since AD1320", "County floods remembered by Nottinghamshire Archives and Picture the Past", "Hull and north Lincolnshire floods clean-up begins", "East Staffordshire Strategic Flood Risk Assessment Level 1 Report", "The Annual RPI and Average Earnings for Britain, 1209 to Present (New Series)", British Waterways, River Trent Water Freight Feasibility Study, p11, "Ports and wharves of North Lincolnshire", "Freighter-Celtic-Endeavor-aground-and-refloated". Below Cromwell lock, the Trent is tidal, and therefore only navigable by experienced, well-equipped boaters. The lowest flows for the river were recorded during the drought of 1976, following the dry winter of 1975/6. The suburbs of Long Eaton, West Bridgford and Beeston all suffered particularly badly. [11], At Shardlow, where the Trent and Mersey Canal begins, the river also meets the Derwent at Derwent Mouth. 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. These include recreational water activities, and once rehabilitated, as nature reserves and wetlands. The lower Bann flows northward through Lough Beg and carries the waters of Lough Neagh to the sea below Coleraine. 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. [47][148] More definitive finds from the medieval period were also found at this site and near Colwick. 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. There are also baseflow contributions from the major aquifers in the catchment. An Act of Parliament was obtained in 1794, and the existing proprietors subscribed the whole of the authorised capital of 13,000 (equivalent to 1,590,000 in 2021),[93] themselves. The River Great Ouse meanders through some of the prettiest towns and villages in Cambridgeshire. 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. 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. Downstream of the town the villages are often named in pairs, representing the fact that they were once linked by a river ferry between the two settlements. 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? Plans for new larger locks at Beeston and Wilford were abandoned when the Trent Catchment Board opposed them. The Trent Aegir tidal bore. The Dadfords, who were engineers on the Trent and Mersey Canal, estimated the cost at 20,000, but the proposal was opposed by landowners and merchants on the river, while the Navigator, published in 1788, estimated that around 500 men who were employed to bow-haul boats would have lost their jobs. Recorded at 1230hrs on 8 November 2000 highest discharge since 1 September 1958. [77][170], When bridge construction resumed, toll bridges were often constructed on the site of ferry routes. 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. Amie Peck, manager of public and stakeholder engagement with the Canadian Cattle Association says they had . 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. 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. Nottingham seems to have been the ancient head of navigation until the Restoration, due partly to the difficult navigation of the Trent Bridge. 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. Built as an abbey church, it has a Norman nucleus as well as touches Tip by Amy Bookmark Take Me There OSM 2 Shrewsbury Abbey [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. It flows through and drains most of the metropolitan central and northern Midlands south and east of its source north of Stoke-on-Trent. [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. At least one other medieval attempt was made to bridge the Trent near Wilden at Hemington, but this was gone long before the end of the Middle Ages. [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]. 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. River Bann, Irish An Bhanna, river, the largest in Northern Ireland, falling into two distinct parts. Brian/CC BY-SA 2.0. [91] Eventually in 1805, they reached an agreement with Henshall & Co., the leading canal carriers, for the closure of the river above Wilden Ferry. From Syresham in central England, the Great Ouse flows into East Anglia before entering the Wash, a bay of the North Sea. [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. Key information about Oxford, Royal Windsor, London and Southend and all the other towns 200+ miles along the River Thames. The second and third largest are the Derwent and the Dove respectively; together these two rivers drain the majority of Derbyshire and Staffordshire, including the upland areas of the Peak District. [67][68] The central arches of the medieval Swarkestone bridge were knocked out by the great flood of 1795 and rebuilt, but the bridge's more rural location allowed large portions of the medieval bridge to survive and remain in use today. [100][101] It also includes the green spaces and gardens of . 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. [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. The Trent historically marked the boundary between Northern England and Southern England. The river flows in a southerly direction for fifty miles before reaching it's estuary on the Hamoaze, situated on Plymouth Sound in the English Channel. In Nottingham the heights of significant historic floods from 1852 have been carved into a bridge abutment next to Trent Bridge, with flood marks being transferred from the medieval Hethbeth bridge that pre-dated the existing 19th-century crossing. 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. Menu. 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). [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. [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. 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 [92], The first improvement of the lower river was at Newark, where the channel splits into two. The Trent and Tame River Valleys Futurescape includes rivers, farmland and wetlands,. 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 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%. key towns of river bannmr patel neurosurgeon cardiff 27 februari, 2023 . [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. I received this morning a letter from the secretary of a Burton rowing club. Pictures & slide show. 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. 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. [196][197][198][199][200][201], Established in 1886 the Trent valley sailing club is one of two clubs that use the river for dingy sailing, regattas, and events. Using invertebrates as an indicator of pollution levels, it was appropriately named the Trent Biotic index. Duke of Sutherland, describing the river in his injunction of 1902. 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. 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. [98][99], Down river of Shardlow, the non-tidal river is navigable as far as the Cromwell Lock near Newark, except in Nottingham (Beeston Cut & Nottingham Canal) and just west of Nottingham, where there are two lengths of canal, Sawley and Cranfleet cuts. He also took out an injunction against the council to prevent the ongoing contamination causing a "most foul and offensive stench", the river not even being suitable to water grazing cattle on the estate. Livestock was badly affected, 72 sheep drowned in Wilford and ten cows were lost in Bridgford. [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. Unusually for an English river, the channel altered significantly during historic times, and has been described as being similar to the Mississippi in this respect, especially in its middle reaches, where there are numerous old meanders and cut-off loops. 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. The river in Burton is crossed by a number of bridges including the ornate 19th-century Ferry Bridge that links Stapenhill to the town. [77], Early bridges were vulnerable to floods, and in 1309 many bridges were washed away or damaged by severe winter floods, including Hethbeth Bridge. [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. 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 river continues north-east, passing the village of Walton-on-Trent until it reaches the large town of Burton upon Trent. The river crosses a band of Triassic Sherwood sandstone at Sandon, and it meets the same sandstone again as it flows beside Cannock Chase, between Great Haywood and Armitage, there is also another outcrop between Weston-on-Trent and King's Mill. It flows through the most frequented national Park in the country - The Peak District. Last Thursday, its senior eight were out rowing when Its source is in Staffordshire on the southern edge of Biddulph Moor. The mighty River Trent is one of England's major rivers. Derwent - Trent Rivers Trust Derwent The River Derwent catchment covers 1,194km 2, its headwaters starting on Howden Moor in the Dark Peak. In order to retain control of the whole river, they supported the inclusion of the Beeston Cut in the bill for the Nottingham Canal, which prevented the Erewash Canal company from getting permission to build it, and then had the proposal removed from the Nottingham Canal company's bill in return for their support of the main bill. 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. And cuts me from the best of all my land [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. It also incorporates the iconic Howden, Derwent and Ladybower Reservoirs. [117] Angling clubs in Burton used the Dove or local lakes for fishing, as the Trent through the town was absent of any fish. Over the study period the returns revealed that there was a variation in the species caught, with a shift from roach and dace based catches, to one of chub and bream, a change that was perceived by anglers to represent a serious detriment to the fishery. [69][70][71], In the lower tidal reaches the Trent has a high sediment load, this fine silt which is also known as warp', was used to improve the soil by a process known as warping, whereby river water was allowed to flood into adjacent fields through a series of warping drains, enabling the silt to settle out across the land. [155], Analysis of catch returns from 1969 to 1985, showed that the fish caught most often by anglers were barbel, bream, bleak, carp, chub, dace, eel, gudgeon, perch, and roach. The River Trent is the third longest river in England with a length of 298 km, and the second largest in terms of flow, with a basin estimating 10,435 km 2 . The cost of improvements was too great for the old company, and so an Act of Parliament was obtained in 1884 to restructure the company and raise additional capital. 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. [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. 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. 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