what are the key towns of the river trent

The Trent River is a river in southeastern Ontario which flows from Rice Lake to empty into the Bay of Quinte on Lake Ontario.This river is part of the Trent-Severn Waterway which leads to Georgian Bay.The river is 90 kilometres (56 mi) long. Commercial carrying above Nottingham ceased during the 1950s, to be replaced by pleasure cruising. The Trent is the third-longest river in the United Kingdom.Its source is in Staffordshire, on the southern edge of Biddulph Moor.It flows through and drains the North Midlands.The river is known for dramatic flooding after storms and spring snowmelt, which in the past often caused the river to change course. These cities lie on the river Trent: Stoke-on-Trent. The lower river occupies a peaty depression in the . Domestic effluent and polluting discharges from the metal working industries in the upper reaches, combined to affect the whole length of the tributary River Tame. Key information about Oxford, Royal Windsor, London and Southend and all the other towns 200+ miles along the River Thames. In. [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. [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, [49] Rainfall totals in the Tame are not as high as would be expected from the moderate relief, due to the rain shadow effect of the Welsh mountains to the west, reducing amounts to an average of 691mm (27.2in) for the tributary basin. elephant jokes from the 60's . See answer (1) Copy. 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. [77], Early bridges were vulnerable to floods, and in 1309 many bridges were washed away or damaged by severe winter floods, including Hethbeth Bridge. [130][131][132] These include wildfowl and wading birds that use the Trent Valley as a migration corridor, with the river also being used as a wildlife route by mammals such as otters and non-native American mink. The company also considered a plan to reopen the river to Burton, which would have involved the rebuilding of Kings Mills lock, and the construction of four new locks. Lord Paget seems to have funded the work privately, building locks at King's Mill and Burton Mills and several cuts and basins. [29]:29[35], The less populous rural areas are offset by a number of large urbanised areas including the conurbations of Stoke-on-Trent, Birmingham and the surrounding Black Country in the West Midlands; and in the East Midlands the major university cities and historical county seats of Leicester, Derby and Nottingham. [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. [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. It is situated mainly on the west bank of the River Trent and on the Grand Trunk (Trent and Mersey) Canal. 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. 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. This proposal formed the basis for an Act of Parliament obtained in 1783, which also allowed a horse towing path to be built. 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. [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. It combines riverside and towpath sections, with other paths to villages and places of interest in the wider valley. [95], Increased running costs after the First World War could not be met by increasing the tolls, as the company had no statutory powers to do so, and so suggested that the Ministry of Transport should take over the navigation, which they did from 24 September 1920. It flows through the bustling city of Nottingham, the market town of Newark and the rural Trent Vale. 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. There were also negotiations with the London and North Eastern Railway, who were responsible for the Nottingham Canal between Trent Lock and Lenton. [11][12], It then reaches the town of Gainsborough with its own Trent Bridge. [116][161], Glover noted in 1829 that all three types of crossing were still in use on the Derbyshire section of the Trent, but that the fords were derelict and dangerous. The native and migrant species are still spotted in River Trent where they live on the nature reserves and wetland areas. 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. [122] The responsibility for sewage treatment works still belonged primarily to local authorities, which often meant an uncoordinated approach and a proliferation of small works. [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. Students in Alberta will be the first to experience the online grazing simulation game which focuses on the ecosystem services provided by raising cattle on grasslands. Last Thursday, its senior eight were out rowing when The flood bank was subsequently strengthened and repaired, following further floods during 1824 and 1852. Tolls were increased, and a committee recommended improvements to the river. 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. [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. Pictures & slide show. [157], Recreational fishing is still popular, although anglers no longer line the banks as they once did. Further north at Littleborough is the site of the Roman town of Segelocum, where a Roman road once crossed the river. [128] The improvements that have taken place mean that the Trent can be used for public water consumption. [114], This was a particular problem in Stoke-on-Trent and the growing towns of the Potteries. 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. 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. Some 20,000 acres (81km2; 31sqmi) were flooded for a period of over three weeks.[23][81][82]. It flows through the most frequented national Park in the country - The Peak District. [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. Today, exploring the lovely old riverside buildings provides a great family day out. The wide Humber estuary has often been described as the boundary between the Midlands and the north of England. The Trent drains a large portion of south-central Ontario, including most of the Kawartha Lakes and their supplying watersheds. 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. [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. The use of a maritime pilot on the Trent is not compulsory for commercial craft, but is suggested for those without any experience of the river. Yet Thames and Severne both in this come short of me, 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 suburbs of Long Eaton, West Bridgford and Beeston all suffered particularly badly. key towns of river banniridescent telecaster pickguard. Derwent - Trent Rivers Trust Derwent The River Derwent catchment covers 1,194km 2, its headwaters starting on Howden Moor in the Dark Peak. The medieval bridges of Burton and Nottingham survived relatively intact until the 1860s, when both were replaced and demolished. 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. These levels extend across the Trent valley, and include the lower reaches of the Eau, Torne and Idle. Sir Ernest Jardine, who as vice-chairman had partly funded the first lock at Cromwell in 1908, died in 1947, and the company ceased to exist in 1948 when the waterways were nationalised. Duke of Sutherland, describing the river in his injunction of 1902. Efird Companies began in 1965 as the original developer of the Town of River Bend in . At Yoxall, the flow increases to 12.8m3/s (450cuft/s) due to the input of larger tributaries including the Sow and Blithe. Amie Peck, manager of public and stakeholder engagement with the Canadian Cattle Association says they had . [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. The Nottingham and Gainsborough Railway offered 100 per share during 1845, but this was rejected. [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. [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. The only toll bridge that remains across the Trent is at Dunham, although it is free to cross on Christmas and Boxing Day. key towns of river bannmr patel neurosurgeon cardiff 27 februari, 2023 . 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 lower Bann flows northward through Lough Beg and carries the waters of Lough Neagh to the sea below Coleraine. 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. [159] Returning adult salmon have been seen leaping over weirs on the river[159] and in 2011 a large salmon weighing over 10 pounds (4.5kg) was caught at an undisclosed location, and was 'thought to be the biggest caught on the Trent in the last thirty years'.[160]. [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. These fording points only allowed passage across the river when water levels were low; when the river was in flood a long detour could be required. [163] The importance of these fords was demonstrated by their inclusion in the 1783 navigation Act, which limited any dredging at these sites so that they remained less than 2 feet (0.61m) deep. [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. Rugeley. One effect of this pollution was that the upper and middle reaches were completely devoid of any fish life.[115]. [151][184][189][190] The first person to swim the entire swimmable length of the Trent was Tom Milner, who swam 139 miles (224km) over nine days in July 2015. [34] [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. [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. [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. It also incorporates the iconic Howden, Derwent and Ladybower Reservoirs. In quantity equals not one of yours: 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. [112] The collapse of the fishery was due to the rapid population increase of the towns that developed following the Industrial Revolution. [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. From its source in the Plynlimon Mountains in west Wales, the River Severn flows through the West Midlands counties of Shropshire, Worcestershire and Gloucestershire Wales (Powys) Llanidloes(165m above sea level) Caersws Newtown(103m above sea level) Welshpool(70m above sea level) England Shropshire Shrewsbury(county town and historic city) Throughout history, the river has been a main route for trade and travel. [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. It flows through and drains the North Midlands. 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. (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. [37][39], The low range of hills, which have been formed into a steep set of cliffs overlooking the Trent between Scunthorpe and Alkborough are also made up of mudstones, but are of the younger Rhaetic Penarth Group. For example, the administration of royal forests was subject to a different justice in eyre north and south of the river, and the jurisdiction of the medieval Council of the North started at the Trent. When this retreated, the Trent adopted its current course into the Humber. . [91], At the beginning of the 1790s, the Navigation faced calls for a bypass of the river at Nottingham, where the passage past Trent Bridge was dangerous, and the threat of a canal running parallel to the river, which was proposed by the Erewash and the Trent and Mersey Canal companies. As it enters the city, it passes the suburbs of Beeston, Clifton and Wilford; where it is joined by the Leen. At Besthorpe near Newark, breeding pairs of little egrets and grey herons have been observed. The two locks at Cromwell became one, capable of holding eight Trent barges, dredging equipment was updated, and several of the locks were mechanised. [92], The first improvement of the lower river was at Newark, where the channel splits into two. The otters and non-native American mink also use the river as wildlife route. 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). [136][137], Other managed wetland sites along the river include Beckingham Marshes, Croxall Lakes, Drakelow, and Willington Gravel Pits. 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. The majority of these urban areas are in the upper reaches of either the Trent itself, as is the case with Stoke, or its tributaries. 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. 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). 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. [9] A traditional but almost certainly wrong opinion is that of Izaak Walton, who states in The Compleat Angler (1653) that the Trent is " so called from thirty kind of fishes that are found in it, or for that it receiveth thirty lesser rivers. [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. oregon rainfall totals 2021 / tatum ranch golf membership cost / key towns of river bann. From Syresham in central England, the Great Ouse flows into East Anglia before entering the Wash, a bay of the North Sea. [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. Nissan says the SUVs have jackknife folding keys that may not stay fully open. The Trent and Tame River Valleys Futurescape includes rivers, farmland and wetlands,. [132][135] One of the most important of these is Attenborough Nature Reserve, a 226-hectare (560-acre) Site of Special Scientific Interest (SSSI) which is visited by wildfowl such as Eurasian wigeon and common teal. [41], The lower sequences of these terraces have been widely quarried for sand and gravel, and the extraction of these minerals continues to be an important industry in the Trent Valley, with some three million tonnes of aggregates being produced each year. [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). 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. The new Ferry Bridge was opened in 1889, although it needed the financial support of the brewer and philanthropist Michael Bass to pay for the construction, and later in 1898 to purchase the existing ferry rights so that it became free of tolls. 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