[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. [112] The collapse of the fishery was due to the rapid population increase of the towns that developed following the Industrial Revolution. [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. 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. [177], In downstream order, the power stations that continue to use, or have used the river as their source of cooling water are: Meaford, Rugeley, Drakelow, Willington, Castle Donington, Ratcliffe-on-Soar, Wilford, Staythorpe, High Marnham, Cottam, West Burton and Keadby. [23], On 1718 March 1947 the Trent overtopped its banks in Nottingham. Riverside lakes near Shardlow act as a reserve water source for Nottingham and Derby, and water is also abstracted at Torksey and Newton-on-Trent for supplies in Lincolnshire. [11], Downstream of Keadby the river progressively widens, passing Amcotts and Flixborough to reach Burton upon Stather and finally Trent Falls. 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. [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. The upper Bann rises in the Mourne Mountains and flows northwest to Lough (lake) Neagh. 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. The most important in terms of the river are the extensive sandstone and limestone aquifers that underlie many of the tributary catchments. [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. Navigation can be difficult, and there have been a number of incidents with ships running aground and in one case, striking Keadby Bridge. [168][169]) Cavendish Bridge was itself damaged beyond repair by a flood in March 1947, requiring a temporary Bailey bridge to be used until a new concrete span was constructed in 1957. [115][118], The pollution of the "Trent catchment was probably at its worst in the late 1950s",[115] this being the result of the ongoing industrialisation of the urban areas, combined with the interruption and under investment caused by two world wars, which lead to only piecemeal improvements of the sewerage treatment infrastructure taking place. [91] Eventually in 1805, they reached an agreement with Henshall & Co., the leading canal carriers, for the closure of the river above Wilden Ferry. [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. [57][84][85] Two days later, in the lower tidal reaches of the river, the peak of the flood combined with a high spring tide to flood villages and 2,000 properties in Gainsborough. River Trent through Nottingham. In Nottingham a cart overturned in the floodwaters near the Wilford Road and six people drowned, dwellings nearby were flooded to a depth of 6 feet (1.8m). [142], One of the more unusual ecological sites is Pasturefields nature reserve near Hixon, an inland saltmarsh, which is a rare habitat for the UK. Though the river is no doubt legally still navigable above Shardlow, it is probable that the agreement marks the end of the use of that stretch of the river as a commercial navigation. 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. At Besthorpe near Newark, breeding pairs of little egrets and grey herons have been observed. 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. [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. [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. [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. [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. 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. [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. The north part from the south, on my so either sides, [94], The arrival of the railways resulted in significant change for the company. These include the Sherwood sandstones that occur beneath much of eastern Nottinghamshire, the Permian Lower Magnesian limestone and the carboniferous limestone in Derbyshire. [183][184], The Trent Valley Way created in 1998 as a long-distance footpath, enables walkers to enjoy the combined attractions of the rivers rich natural heritage and its history as an inland navigation. Lord Paget seems to have funded the work privately, building locks at King's Mill and Burton Mills and several cuts and basins. [2] Throughout its course, the river mostly flows through the Peak District and its foothills. The most recent occurrence involved the Celtic Endeavour being aground near Gunness for ten days, finally being lifted off by a high tide.[102][103][104]. The canal connects the Trent to the Potteries and on to Runcorn and the Bridgewater Canal. [136][137], Other managed wetland sites along the river include Beckingham Marshes, Croxall Lakes, Drakelow, and Willington Gravel Pits. The river is known for dramatic flooding after storms and spring snowmelt, which in the past often caused the river to change course. [125] The river remains vulnerable to these pollution events, such as the one that occurred in October 2009 when an accidental release of cyanide from a factory into the sewer system in Stoke-on-Trent, affected the treatment works at Strongford. [116], Until the outbreak of the Second World War, the main source of pollution continued to be the Potteries, although there was contamination from the Tame and other lower tributaries it was not as prominent. the river flowed over major road routes. Failure to raise much of the capital resulted in another Act being obtained in 1887, with similar aims and similar results. 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. [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. Commercial carrying above Nottingham ceased during the 1950s, to be replaced by pleasure cruising. 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. [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. It flows through and drains the North Midlands. 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. 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. At this point the River Sow joins it from Stafford. 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. By early 1796, the Beeston cut was operational, with the Cranfleet cut following in 1797, and the Holme cut in 1800, with the whole works being finished by 1 September 1801. Water level management is important in these lowland areas, and the local watercourses are usually maintained by internal drainage boards and their successors, with improved drainage being assisted by the use of pumping stations to lift water into embanked carrier rivers, which subsequently discharge into the Trent. In. The total length is 80 miles (129 km). [94], The aim of the improvements was to increase the minimum depth from 2 feet (0.6m) to 3 feet (0.9m). Throughout history, the river has been a main route for trade and travel. key towns of river bann. 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. 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. [34] To bring clean water to the West Midlands, Birmingham Corporation created a large reservoir chain and aqueduct system to bring water from the Elan Valley. 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. [43] Another notable find in a related terrace system near Derby from a warmer interglacial period, was the Allenton hippopotamus. [128] The improvements that have taken place mean that the Trent can be used for public water consumption. It flows through the bustling city of Nottingham, the market town of Newark and the rural Trent Vale. [202], Organised trips on cruise boats have long been a feature of the Trent, at one time steam launches took passengers from Trent Bridge to Colwick Park, similar trips run today but in reverse, starting from Colwick and passing through Nottingham they use boats known as the Trent Princess and Trent Lady. The tipping point being the introduction of piped water and a basic sewer network, which meant that effluent, which was previously stored in cesspits, was carried away through drains into the nearest brook.[112][113]. [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. At Newark, the last bridge on the Trent until modern times, the bridge was rebuilt in 1775. 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 . And here the smug and silver Trent shall run As water quality improved from the 1960s onwards, fish numbers recovered, and recreational coarse fishing became more popular. It meanders almost 190 miles through this Futurescape, from the Tame in the heart of the Midlands to the Humber. 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) [162] One of the earliest known fords was the crossing at Littleborough, constructed by the Romans it was paved with flagstones, and supported by substantial timber pilings. [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. [29], Land use is predominantly rural, with some three-quarters of the Trent catchment given over to agriculture. 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. [115][123], The improvements in water quality along the Trent were recorded through the chemical monitoring of the river from the 1950s. More improvements followed between 1957 and 1960. . [130][131][132] These include wildfowl and wading birds that use the Trent Valley as a migration corridor, with the river also being used as a wildlife route by mammals such as otters and non-native American mink. Plans for new larger locks at Beeston and Wilford were abandoned when the Trent Catchment Board opposed them. Trento, Latin Tridentum, German Trient, English Trent, city, Trentino-Alto Adige/Sdtirol regione (region), northern Italy. 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. DETROIT (AP) Nissan is recalling more than 809,000 small SUVs in the U.S. and Canada because a key problem can cause the ignition to shut off while they're being driven. Tolls were reduced to retain the traffic, wages were increased to retain the workforce, and they sought amalgamation with a railway company. [117] Angling clubs in Burton used the Dove or local lakes for fishing, as the Trent through the town was absent of any fish. elephant jokes from the 60's . [132][133] It forms part of the Severn-Trent flyway, a route used by migratory birds to cross Great Britain. 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. [125][144][145][146] Seals have been reported up to near the head of the tidal section at Newark. 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. 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. Food was scarce, "in one day 10,000 loaves had to be sent into the town and distributed gratuitously to save people from famine". 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. At Yoxall, the flow increases to 12.8m3/s (450cuft/s) due to the input of larger tributaries including the Sow and Blithe. The cost exceeded the authorised capital by a large margin, with the extra being borrowed, but the company continued to pay a 7 per cent dividend on the original shares and on those created to finance the new work. The River Trent was a major working river until after the Second World War. 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. [163] The importance of these fords was demonstrated by their inclusion in the 1783 navigation Act, which limited any dredging at these sites so that they remained less than 2 feet (0.61m) deep. [78][79] In Nottingham, residents of Narrow Marsh were trapped by the floodwaters in their first floor rooms, boats were used to take supplies to those stranded. [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. 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. Despite a Chancery injunction against them, the two men continued with their action. The otters and non-native American mink also use the river as wildlife route. [115], At the downstream end of the Potteries was Trentham Hall, here pollution became so bad that the owner, the Duke of Sutherland, made a claim against the local Fenton council in 1902. 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. In 1823 and again in 1831, the Newark Navigation Commissioners proposed improvements to the river, so that larger vessels could be accommodated, but the Trent Navigation Company were making a good profit, and did not see the need for such work. February27February 27, 2023. key towns of river bann. The River Great Ouse meanders through some of the prettiest towns and villages in Cambridgeshire. The scale of the ambition of Trent Gateway is large and aims to deliver a functioning watercourse that reduces flood risk, creates habitats and supports the sustainable growth and the local economy across 75km of the river. John Jennings MP for Burton-upon-Trent, 1956. Not only do these provide baseflows to the major tributaries, the groundwater is an important source for public water supply. [154], By the 1970s the Trent was regarded as 'one of the most productive rivers in the British Isles'. For the Trent this proportion is lower, but with nearly half of low flows being made up of these effluent inflows, it is still significant. Together these contain the majority of the 6 million people who live in the catchment.[29]. The only toll bridge that remains across the Trent is at Dunham, although it is free to cross on Christmas and Boxing Day. 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. A huge half-moon, a monstrous cantle out. Agreement could not be reached, and so William Jessop was asked to re-assess the situation. Hayne's lease expired in 1762, and Lord Paget's son, the Earl of Uxbridge, gave the new lease to the Burton Boat Company. [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. The bridges at Wolseley, Wychnor and the main span at Swarkestone were all destroyed. oregon rainfall totals 2021 / tatum ranch golf membership cost / key towns of river bann. More specifically, the name may be a contraction of two Romano-British words, tros ("over") and hynt ("way"). Navigation was then extended to Wilden Ferry, near to the more recent Cavendish Bridge, as a result of the efforts of the Fosbrooke family of Shardlow. Write by: . [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. I'll have the current in this place damm'd up; This was caused by fumes rising from the river. [156] Competition from other fisheries such as well stocked ponds and lakes with better amenities and more consistent catches of fish also meant a reduction in the appeal of fishing the Trent. Today, Torksey is an ordinary Lincolnshire village that lies alongside the River Trent and astride the busy A156. [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. The flood defences around Nottingham and Burton constructed during the 1950s, following the 1947 event, stopped any major urban flooding, but problems did occur in undefended areas such as Willington and Gunthorpe, and again at Girton where 19 houses were flooded. In 1974, these works were transferred to the regional water authorities, with the Severn Trent Water Authority taking over the role for the Trent catchment. 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. It also incorporates the iconic Howden, Derwent and Ladybower Reservoirs. key towns of river bann. [17] Farther downstream at Hemington, archaeologists have found the remains of a medieval bridge across another abandoned channel. The wide Humber estuary has often been described as the boundary between the Midlands and the north of England. 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. 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. 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. [11], Downstream of Nottingham it passes Radcliffe on Trent, Stoke Bardolph and Burton Joyce before reaching Gunthorpe with its bridge, lock and weir. Traffic increased from 620,000 tonnes during 1951 to 1,017,356 tonnes during 1964, but all of this was below Nottingham. the polluted state of the Trent is a terror to Trentham. Such was the case at Willington, Gunthorpe and Gainsborough. [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. [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. Its source is in Staffordshire on the southern edge of Biddulph Moor. I received this morning a letter from the secretary of a Burton rowing club. Other changes, such as the replacement of town gas with natural gas, saw the end of the polluting and toxic coal tar emissions to rivers in 1963. The Trent Aegir tidal bore. A number of the smaller Trent tributaries are still named as warping drains, such as Morton warping drain, near Gainsborough. There are other big events each year like the Oxford and Cambridge University Boat Races . The majority of these urban areas are in the upper reaches of either the Trent itself, as is the case with Stoke, or its tributaries. [54][57], At the other extreme, extended periods of low rainfall can also cause problems. From Syresham in central England, the Great Ouse flows into East Anglia before entering the Wash, a bay of the North Sea. Another translation is given as "the trespasser", referring to the waters flooding over the land. See how this river comes me cranking in, Key information about Oxford, Royal Windsor, London and Southend and all the other towns 200+ miles along the River Thames. [95], Frank Rayner, who had been with the company since 1887, and had served as its engineer and later general manager since 1896, died in December 1945. 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. Trent catchment Board opposed them abandoned when the Trent until modern times the! 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