Nottingham Corporation invested some 450,000 on building the locks authorised by the 1906 Act, starting with Holme lock on 28 September 1921, and finishing with Hazelford lock, which was formally opened by Neville Chamberlain on 25 June 1926. [58], The river's flow is measured at several points along its course, at a number of gauging stations. Its source is in Staffordshire, on the southern edge of Biddulph Moor. It flows through the bustling city of Nottingham, the market town of Newark and the rural Trent Vale. [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. 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. konstantin guericke net worth; xaverian brothers high school nfl players; how is the correct gene added to the cells; hong kong supermarket flyer calgary; ben fogle: new lives in the wild do they get paid; 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. 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. It is situated mainly on the west bank of the River Trent and on the Grand Trunk (Trent and Mersey) Canal. A third Act of 1892 reverted the name to the Trent Navigation Company, and this time, some improvements were performed. [46]:3647 Four of these main tributaries, including the Dove and Derwent which drain the upland Peak District, all join within the middle reaches, giving rise to a comparatively energetic river system for the UK. [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. 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. 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. Mills were important locations for fish and eel traps, the eels being caught during quill time between mid-August and early September. Lord Paget leased the navigation and the wharf at Burton to George Hayne, while the wharf and warehouses at Wilden were leased by Leonard Fosbrooke, who held the ferry rights and was a business partner of Hayne. Livestock was badly affected, 72 sheep drowned in Wilford and ten cows were lost in Bridgford. During the 1950s, however, the same problem of effluent dilution that occurred in Stoke began to become significant in Birmingham and the Black Country. There were corresponding increases in dissolved oxygen, an indicator of a healthy river environment. The river originates from Staffordshire, west Midlands of England, on the southern edge of Biddulph Moor. [94], The aim of the improvements was to increase the minimum depth from 2 feet (0.6m) to 3 feet (0.9m). [5][6], The name "Trent" is possibly from a Romano-British word meaning "strongly flooding". Similar facilities were present in 1870 on the water meadows at Burton-on-Trent, which also had its own swimming club. As water quality improved from the 1960s onwards, fish numbers recovered, and recreational coarse fishing became more popular. [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. [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 Aegir occurs when a high spring tide meets the downstream flow of the river. Pictures & slide show. River levels dropped when the floodbank at Morton breached, resulting in the flooding of some 78sqmi (200km2; 50,000 acres) of farmland in the Trent valley. [72], Warp was also used as a commercial product, after being collected from the river banks at low tide, it was transported along the Chesterfield Canal to Walkeringham where it was dried out and refined to be eventually sold as a silver polish for cutlery manufacturers. [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. 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. For example, Birmingham lies at the upper end of the Tame, and Leicester is located towards the head of the Soar. Flowing for 143 miles, the vast waterway is the fourth-longest in the UK and its history is . Navigation can be difficult, and there have been a number of incidents with ships running aground and in one case, striking Keadby Bridge. February 27, 2023 endeavor air pilot contract No Comments . 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. [154], By the 1970s the Trent was regarded as 'one of the most productive rivers in the British Isles'. Lord Paget seems to have funded the work privately, building locks at King's Mill and Burton Mills and several cuts and basins. These villages include West Stockwith and East Stockwith, Owston Ferry and East Ferry, and West Butterwick and East Butterwick. [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. 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. [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. [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. elephant jokes from the 60's . These lower reaches are protected from tidal flooding by a series of floodbanks and defences. members of the crew were seized with pains in the chest. 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. [45], The topography, geology and land use of the Trent catchment all have a direct influence on the hydrology of the river. 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. [47][148] More definitive finds from the medieval period were also found at this site and near Colwick. This may explain the presence of the Romano-British element rid (cf. [80] The vulnerable flood bank at Spalford was breached again, floodwaters spreading out across the low-lying land, even reaching the River Witham and flooding Lincoln. [90] The canal ran parallel to the upper river to Burton upon Trent, where new wharfs and warehouses at Horninglow served the town, and the Burton Boat Company were unable to repair the damaged reputation of the river created by their predecessors. Nottingham seems to have been the ancient head of navigation until the Restoration, due partly to the difficult navigation of the Trent Bridge. [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. [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. 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. Underlying the upper reaches of the Trent, are formations of Millstone Grit and Carboniferous Coal Measures which include layers of sandstones, marls and coal seams. The only toll bridge that remains across the Trent is at Dunham, although it is free to cross on Christmas and Boxing Day. [109][110] This divide was also described in Michael Drayton's epic topographical poem, Poly-Olbion, The Sixe and Twentieth Song, 1622: And of the British floods, though but the third I be, [191][192], Rowing clubs have existed at Burton, Newark and Nottingham since the mid-1800s, with various regattas taking place between them, both on the river and on the rowing course at the national watersports centre. [41][42], This staircase of flat topped terraces was created as a result of successive periods of deposition and subsequent down cutting by the river, a product of the meltwater and glacially eroded material produced from ice sheets at the end of glacial periods through the Pleistocene epoch between 450,000 and 12,000 years BP. 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. 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