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what are the key towns of the river trent

[138][139][140][141], The Trent valley also links together other SSSI and local nature reserves, which have varying habitats not only for birds, but also mammals, insects and fish, a good example is the tributary River Mease where the entire watercourse has been designated both as a SSSI and a European special area of conservation. Efird Commercial Real Estate. Associated British Ports, the navigation authority for the river from Gainsborough to Trent Falls, insist that anyone in charge of a boat must be experienced at navigating in tidal waters. There were corresponding increases in dissolved oxygen, an indicator of a healthy river environment. Wading birds such as Eurasian oystercatcher and great bittern have also been observed at the reserve; as have kingfishers, reed warblers and water rails. Much of the river's route, with the exception of the city of Derby, is rural. 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 now flows north-east below the Toot and Trent Hills before reaching Hazelford Ferry, Fiskerton and Farndon. [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. 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 . 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. 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. Similar facilities were present in 1870 on the water meadows at Burton-on-Trent, which also had its own swimming club. When this retreated, the Trent adopted its current course into the Humber. 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. See answer (1) Copy. [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. Throughout history, the river has been a main route for trade and travel. This can be a result of a sudden rise in temperature after a prolonged cold period, or when combined with extensive rainfall. It also incorporates the iconic Howden, Derwent and Ladybower Reservoirs. [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. It also includes the green spaces and gardens of . [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 lower Bann flows northward through Lough Beg and carries the waters of Lough Neagh to the sea below Coleraine. 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. A vestige of the saline marshes created by the brine springs that seep from the groundwater of the Mercia mudstones, the reserve contains salt tolerant species normally found on the coast, such as sea plantain, arrowgrass and milkwort. 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. [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. 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. 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. 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. [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. [177], Once these early stations reached the end of their functional life, they were usually demolished, although in some cases the sites have been retained and redeveloped as gas fired power stations. [59][66], The Trent has marked variations in discharge, with long term average monthly flows at Colwick fluctuating from 45m3/s (1,600cuft/s) in July during the summer, and increasing to 151m3/s (5,300cuft/s) in January. [94], The aim of the improvements was to increase the minimum depth from 2 feet (0.6m) to 3 feet (0.9m). 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. [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, Hayne's lease expired in 1762, and Lord Paget's son, the Earl of Uxbridge, gave the new lease to the Burton Boat Company. The only toll bridge that remains across the Trent is at Dunham, although it is free to cross on Christmas and Boxing Day. [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. Historically, these issues resulted in a considerable deterioration in the water quality of both the Trent and its tributaries, especially the Tame. Duke of Sutherland, describing the river in his injunction of 1902. I'll have the current in this place damm'd up; 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". 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. Not only do these provide baseflows to the major tributaries, the groundwater is an important source for public water supply. Last Thursday, its senior eight were out rowing when [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. The recall covers certain Rogues from the 2014 through 2020 model years, as well as Rogue Sports from 2017 through 2022. The Aegir occurs when a high spring tide meets the downstream flow of the river. The changes were helped by the introduction of more stringent pollution control legislation, which required industrial waste to be discharged to sewers, and the formation of the Trent River Authority, which had new duties relating to managing water quality issues. 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; 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. 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. Key information about Oxford, Royal Windsor, London and Southend and all the other towns 200+ miles along the River Thames. 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. The ferry boats used along the Trent ranged in size from small rowing boats, to flat decked craft that could carry livestock, horses, and in some case their associated carts or wagons. 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. [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.

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