Traffic increased from 620,000 tonnes during 1951 to 1,017,356 tonnes during 1964, but all of this was below Nottingham. [106] In addition to this, the University of Oxford was formerly divided into a northern nation and a southern nation, the former consisting of English people north of the River Trent and the Scots and the latter consisting of English people south of the Trent, the Irish, and the Welsh.[107][108]. 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. 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. One effect of this pollution was that the upper and middle reaches were completely devoid of any fish life.[115]. 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. 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. The variation in these factors is also reflected in the contrasting runoff characteristics and subsequent inflows of the principal tributaries. [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. It also includes the green spaces and gardens of . The river is known for dramatic flooding after storms and spring snowmelt, which in past times often caused the river to . Whilst this is not unique for an English river, it does mean that there is an ongoing legacy of issues relating to urban runoff, pollution incidents, and effluent dilution from sewage treatment, industry and coal mining. [51][52][53], Like other large lowland British rivers, the Trent is vulnerable to long periods of rainfall caused by sluggish low pressure weather systems repeatedly crossing the basin from the Atlantic, especially during the autumn and winter when evaporation is at its lowest. [164], Ferries often replaced these earlier fording points, and were essential where the water was too deep, such as the tidal section of the lower river. [94], The arrival of the railways resulted in significant change for the company. More specifically, the name may be a contraction of two Romano-British words, tros ("over") and hynt ("way"). [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. Pictures & slide show. 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. This led to increased investment, the closure of older and smaller works, with sewage treatment being combined at larger modern works such as Strongford and Minworth. [87], The fifth largest flood recorded at Nottingham occurred in November 2000, with widespread flooding of low-lying land along the Trent valley, including many roads and railways. (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. In an attempt to improve the situation, the company toyed with the idea of cable-hauled steam tugs, but instead purchased a conventional steam dredger and some steam tugs. 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. Some traces of the former division remain: the Trent marks the boundary between the provinces of two English Kings of Arms, Norroy and Clarenceux. 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. The Act gave him absolute control over the building of any wharves and warehouses above Nottingham Bridge. 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. Rampton. [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. [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. Archaeologists have recently discovered phenomenal site in Torksey, on the north bank of the River Trent, that has yielded tens of thousands of metal finds over the years. key towns of river bann. 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. As no archive sources record that the Hemington bridge existed, there may have been other medieval bridge projects now forgotten. [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. [178] At one time these sites provided a quarter of the electricity needs of the UK, giving rise to the epithet 'Megawatt Valley'. [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. [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. [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. Such conditions occurred in February 1977, with widespread flooding in the lower reaches of the Trent when heavy rain produced a peak flow of nearly 1,000m3/s (35,000cuft/s) at 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. Navigation can be difficult, and there have been a number of incidents with ships running aground and in one case, striking Keadby Bridge. oregon rainfall totals 2021 / tatum ranch golf membership cost / key towns of river bann. [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). [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. [77], Early bridges were vulnerable to floods, and in 1309 many bridges were washed away or damaged by severe winter floods, including Hethbeth Bridge. 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. Flowing for 143 miles, the vast waterway is the fourth-longest in the UK and its history is . Historic flood levels have also been recorded at Girton and on the churchyard wall at Collingham. 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. 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. The lowest flows for the river were recorded during the drought of 1976, following the dry winter of 1975/6. [17] Farther downstream at Hemington, archaeologists have found the remains of a medieval bridge across another abandoned channel. [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. [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. [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. 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. The complex of three bridges provides evidence of attempts to keep a crossing open over slightly more than two hundred years from 1097, with three bridges constructed on the same site but felled by scouring, floods and course migration of the river to the south eroding the bridgehead. And here the smug and silver Trent shall run The flood defences in Nottingham that protect 16,000 homes and those in Burton where they prevent 7,000 properties from flooding were reassessed after this flood, and were subsequently improved between 2006 and 2012.[84][88]. The Trent now flows south-east past the town of Rugeley until it reaches Kings Bromley where it meets the Blithe. [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. 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. [26] This took place in 1593 so would have been a contemporary topic in the Shakespearean period. elephant jokes from the 60's . [54][57], At the other extreme, extended periods of low rainfall can also cause problems. There were corresponding increases in dissolved oxygen, an indicator of a healthy river environment. [67][68] [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. Burton upon Trent. Later improvements such as the series of purification lakes that were constructed on the Tame in the 1980s, which allowed contaminated sediment to settle out from the river, also reduced pollution levels, and lessened the impact of first flush runoff events in the lower Tame and the middle 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. [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. 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. Large parts of the city and surrounding areas were flooded with 9,000 properties and nearly a hundred industrial premises affected some to first floor height. [125][129], Artificial changes along the Trent, due to navigation, farming, mineral extraction and drainage works, mean that much of the riparian landscape has been altered, reducing the amount of natural habitat. [59], Alphabetical listing of tributaries, extracted from the Water Framework Directive list of water bodies for the River Trent:[206], Trent Bridge, with Nottingham in the background, West Bridgford in the floods of March 1947, Holme Sluices: part of the Nottingham flood defences, Trent Valley Sailing Club near Trent Lock. 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. '[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. https://en.wikipedia.org/w/index.php?title=River_Trent&oldid=1132366164, This page was last edited on 8 January 2023, at 14:59. It flows through the bustling city of Nottingham, the market town of Newark and the rural Trent Vale. [147], Evidence of fishing along the Trent can be traced back to the Neolithic period, with the possible remnants of a fish weir discovered in the abandoned river channels at Hemington. There were also negotiations with the London and North Eastern Railway, who were responsible for the Nottingham Canal between Trent Lock and Lenton. [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. This may explain the presence of the Romano-British element rid (cf. [28], The Trent basin covers a large part of the Midlands, and includes the majority of the counties of Staffordshire, Derbyshire, Leicestershire, Nottinghamshire and the West Midlands; but also includes parts of Lincolnshire, South Yorkshire, Warwickshire and Rutland. 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. [136][137], Other managed wetland sites along the river include Beckingham Marshes, Croxall Lakes, Drakelow, and Willington Gravel Pits. [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. [45], The topography, geology and land use of the Trent catchment all have a direct influence on the hydrology of the river. 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. 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. Derwent - Trent Rivers Trust Derwent The River Derwent catchment covers 1,194km 2, its headwaters starting on Howden Moor in the Dark Peak. [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. Write by: . [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. Today, exploring the lovely old riverside buildings provides a great family day out. Extended in 2012, the route now runs from Trent Lock in the south through to Alkborough where the river meets the Humber. 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. Last Thursday, its senior eight were out rowing when The north part from the south, on my so either sides, [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. Cities and towns on or close to the river include: Prior to the mid-18th century there were few permanent crossings of the river with only four bridges downstream of the Tame confluence: the old medieval bridges at Burton, Swarkestone, Nottingham (known as Hethbeth Bridge) and Newark, all first built by 1204. . [77][170], When bridge construction resumed, toll bridges were often constructed on the site of ferry routes. [89], In 1748, merchants from Nottingham attempted to end this monopoly by landing goods on the banks and into carts, but Fosbrooke used his ferry rope to block the river, and then created a bridge by mooring boats across the channel, and employing men to defend them. 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