The upper Bann rises in the Mourne Mountains and flows northwest to Lough (lake) Neagh. 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. Hayne's lease expired in 1762, and Lord Paget's son, the Earl of Uxbridge, gave the new lease to the Burton Boat Company. Flows measured at Nottingham were exceptionally low by the end of August, and were given a drought return period of greater than one hundred years. The only time it was settled was in the winter of 872 to 873 and, as a result, we can be pretty sure that all these finds date from that winter. More specifically, the name may be a contraction of two Romano-British words, tros ("over") and hynt ("way"). Stone. [100][101] [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. 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. The parallel canal was thwarted in May 1793, when they negotiated the withdrawal of the canal bill by proposing a thorough survey of the river which would result in their own legislation being put before parliament. [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. [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. With a course of 143 miles . [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, 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. [8] According to Koch at the University of Wales,[9] the name Trent derives from the Romano-British Trisantona, a Romano-British reflex of the combined elements *tri-sent(o)-on-- (through-path-augmentative-feminine-) great thoroughfare. Newark Navigation Commissioners were created, with powers to borrow money to fund the construction of two locks, and to charge tolls for boats using them. [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. Raising finance was difficult, but some was subscribed by the chairman and vice-chairman, and construction of Cromwell Lock began in 1908. In quantity equals not one of yours: 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. '[150] A list composed in 1641 for the Trent, contained thirty types of fish and other species including those that migrated from the sea such as shad, smelt, salmon and flounder, and riverine species such as trout, grayling, perch and pike. On reaching West Bridgford it flows beneath Trent Bridge near the cricket ground of the same name, and beside The City Ground, home of Nottingham Forest, until it reaches Holme Sluices. key towns of river banniridescent telecaster pickguard. 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. 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. Wading birds such as Eurasian oystercatcher and great bittern have also been observed at the reserve; as have kingfishers, reed warblers and water rails. [43] Another notable find in a related terrace system near Derby from a warmer interglacial period, was the Allenton hippopotamus. [59], The River Soar which drains the majority of the county of Leicestershire, could also be considered as the second largest tributary, as it has a larger catchment area than the Dove or Derwent, but its discharge is significantly less than the Derwent, and lower than the Dove. 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 [24][25] The idea for this scene, may have been based on the disagreement regarding a mill weir near Shelford Manor, between local landowners Gilbert Talbot, Earl of Shrewsbury, and Sir Thomas Stanhope which culminated with a long diversion channel being dug to bypass the mill. Menu. Efird Companies began in 1965 as the original developer of the Town of River Bend in . 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. Some 20,000 acres (81km2; 31sqmi) were flooded for a period of over three weeks.[23][81][82]. Its drainage basin covers more than 4,000 square miles (10,000 square km). These cities lie on the river Trent: Stoke-on-Trent. [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. [152] The last known catch was in 1902 near Holme, the fish was .mw-parser-output .frac{white-space:nowrap}.mw-parser-output .frac .num,.mw-parser-output .frac .den{font-size:80%;line-height:0;vertical-align:super}.mw-parser-output .frac .den{vertical-align:sub}.mw-parser-output .sr-only{border:0;clip:rect(0,0,0,0);height:1px;margin:-1px;overflow:hidden;padding:0;position:absolute;width:1px}8+12 feet (2.6m) and weighed 250 pounds (110kg). Commercial carrying above Nottingham ceased during the 1950s, to be replaced by pleasure cruising. [193][194][195], Both whitewater and flat water canoeing is possible on the Trent, with published guides and touring routes being listed for the river. River Great Ouse. I'll have the current in this place damm'd up; 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. Historic flood levels have also been recorded at Girton and on the churchyard wall at Collingham. Jan 1993 - May 202128 years 5 months. [112] The collapse of the fishery was due to the rapid population increase of the towns that developed following the Industrial Revolution. [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. members of the crew were seized with pains in the chest. Men bound them on the north, or on the south of Trent[111], It is not clear when pollution first became an issue for the River Trent, but in the late 1880s, it had a thriving salmon fishery, with the river producing an annual catch of some 3,000 fish, a decade later, this had fallen to 100. The National Watersports Centre at Holme Pierrepont, near Nottingham combines facilities for many of these sports, including rowing, sailing and whitewater canoeing. River Trent through Nottingham. 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]. 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. [149], The Domesday catalogue showed that there were many successful mills and fisheries along the Trent. These include recreational water activities, and once rehabilitated, as nature reserves and wetlands. River Trent, river in the English Midlands. [94], The arrival of the railways resulted in significant change for the company. Mills were important locations for fish and eel traps, the eels being caught during quill time between mid-August and early September. William Jessop performed the survey, assisted by Robert Whitworth, and they published their report on 8 July 1793. [154] This led to comments that the river had become too clean for its fish, and its popularity, especially for match fishing, declined from the mid 1980s. 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. [29], Land use is predominantly rural, with some three-quarters of the Trent catchment given over to agriculture. 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. For that I am the mere of England, that divides The UK's third longest river, the Trent, touches the lives of more than six million people. 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. The river originates from Staffordshire, west Midlands of England, on the southern edge of Biddulph Moor. 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. [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. [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. The north part from the south, on my so either sides, The two locks at Cromwell became one, capable of holding eight Trent barges, dredging equipment was updated, and several of the locks were mechanised. Restrictions on size mean that the largest vessels that can be accommodated are 100m (330ft) long and 4,500 tonnes. [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. Together these contain the majority of the 6 million people who live in the catchment.[29]. Flowing for 143 miles, the vast waterway is the fourth-longest in the UK and its history is . The Aegir cannot travel much beyond Gainsborough as the shape of the river reduces the Aegir to little more than a ripple, and weirs north of Newark-on-Trent, Nottinghamshire, stop its path completely. The Aegir occurs when a high spring tide meets the downstream flow of the river. [114], This was a particular problem in Stoke-on-Trent and the growing towns of the Potteries. [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. [115], The economic recession in the 1970s meant that there was a considerable contraction of heavy industrial sectors, reducing pollution loadings from factories and foundries. 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. [11], Downstream of Nottingham it passes Radcliffe on Trent, Stoke Bardolph and Burton Joyce before reaching Gunthorpe with its bridge, lock and weir. 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. During lower flows the Trent and its tributaries are heavily influenced by effluent returns from sewage works, especially the Tame where summer flows can be made up of 90% effluent. (Until the late 18th century, a long period of stagnation for economic and technical reasons limited the number of bridges over the Trent; it has been noted that relatively few bridges were constructed in England on new sites anywhere between around 12501300 and 1750. 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. During the 1950s, however, the same problem of effluent dilution that occurred in Stoke began to become significant in Birmingham and the Black Country. [118], In the 17th century Izaak Walton described the River Trent as 'One of the finest rivers in the world and the most abounding with excellent salmon and all sorts of delicate fish. Brian/CC BY-SA 2.0. These include the Sherwood sandstones that occur beneath much of eastern Nottinghamshire, the Permian Lower Magnesian limestone and the carboniferous limestone in Derbyshire. 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. [117] Angling clubs in Burton used the Dove or local lakes for fishing, as the Trent through the town was absent of any fish. The Trent drains a large portion of south-central Ontario, including most of the Kawartha Lakes and their supplying watersheds. [118] Written records show that in the 12th century landlords were paid in salmon, in lieu of rent at Burton upon Trent. "[10], The Trent rises within the Staffordshire Moorlands district, near the village of Biddulph Moor, from a number of sources including the Trent Head Well. In. The mighty River Trent is one of England's major rivers. The average for the whole Trent catchment is 720mm (28in) which is significantly lower than the average for United Kingdom at 1,101mm (43.3in) and lower than that for England at 828mm (32.6in). 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 river in Burton is crossed by a number of bridges including the ornate 19th-century Ferry Bridge that links Stapenhill to the town. The native and migrant species are still spotted in River Trent where they live on the nature reserves and wetland areas. [11] To the north-east of Burton the river is joined by the River Dove at Newton Solney and enters Derbyshire, before passing between the villages of Willington and Repton where it turns directly east to reach Swarkestone Bridge. As no archive sources record that the Hemington bridge existed, there may have been other medieval bridge projects now forgotten. It was a Viking winter camp. [116][171], At Stapenhill near Burton, there were similar calls for a new bridge, a tally of usage showed that the foot ferry was being used 700 times per day. At certain times of the year, the lower tidal reaches of the Trent experience a moderately large tidal bore (up to 5 feet [1.5m] high), commonly known as the Trent Aegir (named after the Norse sea god). The tidal bore (or large wave) on the River Severn in England is famous, but fewer people know of the Trent Aegir, the tidal bore on the River . 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 Another translation is given as "the trespasser", referring to the waters flooding over the land. 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. [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. A description of the breach was given as follows: The bank is formed upon a plain of sandy nature, and when it was broken in 1795, the water forced an immense breach, the size of which may be judged from the fact that eighty loads of faggots and upwards of four hundred tons of earth were required to fill up the hole, an operation which took several weeks to complete. [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. 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). The Travellers' Dictionary of Quotations: Who Said What, About Where? [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. Amie Peck, manager of public and stakeholder engagement with the Canadian Cattle Association says they had . [48][50] 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. [157], Recreational fishing is still popular, although anglers no longer line the banks as they once did. Its source is in Staffordshire, on the southern edge of Biddulph Moor. [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. [23], On 1718 March 1947 the Trent overtopped its banks in Nottingham. 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. One effect of this pollution was that the upper and middle reaches were completely devoid of any fish life.[115]. For example, Birmingham lies at the upper end of the Tame, and Leicester is located towards the head of the Soar. [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. [54][57], At the other extreme, extended periods of low rainfall can also cause problems. [58], The river's flow is measured at several points along its course, at a number of gauging stations. The Grand Union refused to improve the Soar Navigation, because the Trent Navigation Company could not guarantee 135,000 tons of additional traffic. 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. 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. [180][181], There is one hydroelectric power station on the river, Beeston Hydro at Beeston Weir. 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. 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 documentary "Guardians of the Grasslands" has now evolved into an online game for students in Grade 7 to 10. The Trent Aegir tidal bore. 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. Facts about the River Trent 5: the native and migrant species. Most of the town belongs to the historic county of Staffordshire, but the neighbourhoods on the east bank of the Trent lie in the . Efird Commercial Real Estate. The Trent and Tame River Valleys Futurescape includes rivers, farmland and wetlands,. oregon rainfall totals 2021 / tatum ranch golf membership cost / key towns of river bann. It flows through the bustling city of Nottingham, the market town of Newark and the rural Trent Vale. Recorded at 1230hrs on 8 November 2000 highest discharge since 1 September 1958. It flows through and drains most of the metropolitan central and northern Midlands south and east of its source north of Stoke-on-Trent. [5][6], The name "Trent" is possibly from a Romano-British word meaning "strongly flooding". 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. [34] This may explain the presence of the Romano-British element rid (cf. [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 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%. [92], The first improvement of the lower river was at Newark, where the channel splits into two. 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. 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. Open water swimming still takes place at locations including Colwick Park Lake adjacent to the river, with its own voluntary lifeguards. [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. [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. 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. [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. There are also baseflow contributions from the major aquifers in the catchment. [7] This may indeed indicate a river that is prone to flooding. And cuts me from the best of all my land [23][77], The largest known flood was the Candlemas flood of February 1795, which followed an eight-week period of harsh winter weather, rivers froze which that meant mills were unable to grind corn, and then followed a rapid thaw. Today, exploring the lovely old riverside buildings provides a great family day out. 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