[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, The Trent now flows south-east past the town of Rugeley until it reaches Kings Bromley where it meets the Blithe. [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 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 . [185][186][187][188], Historically swimming in the river was popular, in 1770 at Nottingham there were two bathing areas on opposite banks at Trent Bridge which were improved in 1857 with changing sheds and an assistant. The River Trent is the third-longest river in the United Kingdom. [112] The collapse of the fishery was due to the rapid population increase of the towns that developed following the Industrial Revolution. [59], In terms of rainfall the Derwent receives the highest annual average rainfall, whereas the Devon, which has the lowest average rainfall is the driest catchment of those tabulated. However, a more likely explanation may be that it was considered to be a river that could be crossed principally by means of fords, i.e. [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. 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]. Flowing for 143 miles, the vast waterway is the fourth-longest in the UK and its history is . 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. [166] King Edward fortified the Nottingham bridge in 920, while a notable battle took place at Burton's bridge in 1322, and another in 1643. River Trent, river in the English Midlands. It lies along the Adige River, south of Bolzano. 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. 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. [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. Nottingham seems to have been the ancient head of navigation until the Restoration, due partly to the difficult navigation of the Trent Bridge. I received this morning a letter from the secretary of a Burton rowing club. 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. 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. An extra set of gates were added to Cromwell lock in 1935, effectively creating a second lock, while the Lenton to Trent Lock section was leased from the LNER in 1936, and ultimately purchased in 1946. The mighty River Trent is one of England's major rivers. Key information about Oxford, Royal Windsor, London and Southend and all the other towns 200+ miles along the River Thames. 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. Shortly afterwards, the river becomes the Derbyshire-Leicestershire border, passing the traditional crossing point of King's Mill, Castle Donington, Weston-on-Trent and Aston-on-Trent. [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. 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. 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. These consisted of V shaped alignments of stakes; wattle panels and a large wicker trap and demonstrate that passive fishing techniques were in use on the river. 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. [172][173], The toll bridges were mostly bought out by the county councils in the 19th century following government reforms, one of the earliest being Willington in 1898, the first toll free crossing was marked by a procession across the bridge and a day of celebration. [97], The river is legally navigable for some 117 miles (188km) below Burton upon Trent. Up to 0.3 metres (1ft) of deposition could occur in a single season, and depths of 1.5 metres (5ft) have been accumulated over time at some locations. The lowest flows for the river were recorded during the drought of 1976, following the dry winter of 1975/6. The last point of measurement is North Muskham here the average flow is 88.4m3/s (3,120cuft/s), a relatively small increase due to the input of the Devon, and other smaller Nottinghamshire tributaries. Further north at Littleborough is the site of the Roman town of Segelocum, where a Roman road once crossed the river. [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. It also incorporates the iconic Howden, Derwent and Ladybower Reservoirs. The total length is 80 miles (129 km). key towns of river banniridescent telecaster pickguard. Newark was once an important inland port on the mighty River Trent. Plans for new larger locks at Beeston and Wilford were abandoned when the Trent Catchment Board opposed them. [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. [18][19] Researchers using aerial photographs and historical maps have identified many of these palaeochannel features, a well-documented example being the meander cutoff at Sawley. [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. [17] Farther downstream at Hemington, archaeologists have found the remains of a medieval bridge across another abandoned channel. Downstream of Burton upon Trent, the river increasingly trends northwards, cutting off a portion of Nottinghamshire and nearly all of Lincolnshire from his share, north of the Trent. 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. Historically, these issues resulted in a considerable deterioration in the water quality of both the Trent and its tributaries, especially the Tame. [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. [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. It flows through the bustling city of Nottingham, the market town of Newark and the rural Trent Vale. [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. 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. It flows through the most frequented national Park in the country - The Peak District. [11], Downstream of Nottingham it passes Radcliffe on Trent, Stoke Bardolph and Burton Joyce before reaching Gunthorpe with its bridge, lock and weir. The suburbs of Long Eaton, West Bridgford and Beeston all suffered particularly badly. Lord Paget seems to have funded the work privately, building locks at King's Mill and Burton Mills and several cuts and basins. A huge half-moon, a monstrous cantle out. the river flowed over major road routes. 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. [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. 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. 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. [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. [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. [36][37], In the wider catchment the geology is more varied, ranging from the Precambrian rocks of the Charnwood Forest, through to the Jurassic limestone that forms the Lincolnshire Edge and the eastern watershed of the Trent. When this retreated, the Trent adopted its current course into the Humber. Livestock was badly affected, 72 sheep drowned in Wilford and ten cows were lost in Bridgford. The native and migrant species are still spotted in River Trent where they live on the nature reserves and wetland areas. [154], By the 1970s the Trent was regarded as 'one of the most productive rivers in the British Isles'. [11], At Shardlow, where the Trent and Mersey Canal begins, the river also meets the Derwent at Derwent Mouth. At Yoxall, the flow increases to 12.8m3/s (450cuft/s) due to the input of larger tributaries including the Sow and Blithe. 4 - River Great Ouse - (Estimated Length: 143 Miles) Wiki Info: The River Great Ouse is a river in the United Kingdom, the longest of several British rivers called "Ouse". The upper Bann rises in the Mourne Mountains and flows northwest to Lough (lake) Neagh. I'll have the current in this place damm'd up; oregon rainfall totals 2021 / tatum ranch golf membership cost / key towns of river bann. 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. Traffic increased from 620,000 tonnes during 1951 to 1,017,356 tonnes during 1964, but all of this was below Nottingham. 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