The river passes through Stoke-on-Trent, Stone, Rugeley, Burton upon Trent and Nottingham before joining the River Ouse at Trent Falls to form the Humber Estuary, which empties into the North Sea between Hull in Yorkshire and Immingham in Lincolnshire. Due to the size of the flood and the ice entrained in the flow, nearly every bridge along the Trent was badly damaged or washed away. 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. The Trent historically marked the boundary between Northern England and Southern England. It also includes the green spaces and gardens of . [54][55][56], Another meteorological risk, although one that occurs less often, is that related to the rapid melting of snow lying in the catchment. After this confluence, the river turns north-east and is joined by the Soar before reaching the outskirts of Nottingham, where it is joined by the Erewash near the Attenborough nature reserve and enters Nottinghamshire. Not only do these provide baseflows to the major tributaries, the groundwater is an important source for public water supply. [11], At Shardlow, where the Trent and Mersey Canal begins, the river also meets the Derwent at Derwent Mouth. One effect of this pollution was that the upper and middle reaches were completely devoid of any fish life.[115]. [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 lower river occupies a peaty depression in the . [2] Throughout its course, the river mostly flows through the Peak District and its foothills. 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. 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. 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. Today, exploring the lovely old riverside buildings provides a great family day out. [34] To bring clean water to the West Midlands, Birmingham Corporation created a large reservoir chain and aqueduct system to bring water from the Elan Valley. Flowing for 143 miles, the vast waterway is the fourth-longest in the UK and its history is . At Newark, the last bridge on the Trent until modern times, the bridge was rebuilt in 1775. Throughout history, the river has been a main route for trade and travel. Restrictions on size mean that the largest vessels that can be accommodated are 100m (330ft) long and 4,500 tonnes. Pictures & slide show. "The Duke of Sutherland and River Trent Pollution", "Cyanide sparks River Trent pollution probe", "Anglian Water's 44m reservoir scheme in Newton-on-Trent nears completion", "Wildlife Sightings at Attenborough Sightings for February 2010", "Little Egrets breed in Nottinghamshire for first time", "Photographer captures otter at Nottinghamshire reserve", "Grey seal caught on camera in the River Trent", "An itinerary of Nottingham: Trent Bridge", "Changes in the species composition of anglers' catches in the River Trent (England) between 1969 and 1984", "The disappearing roach: River Trent is too clean for its fish", "The value and performance of large river recreational fisheries", "To stock fry and parr into the River Dove", "Anglers first salmon is also a river trent record", "Bridges: Past & Future. During a following glaciation (Devensian, 70,000BC) the ice held back vast areas of water called Glacial Lake Humber in the current lower Trent basin. [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. Failure to raise much of the capital resulted in another Act being obtained in 1887, with similar aims and similar results. key towns of river bann. [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, [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. [168][169]) Cavendish Bridge was itself damaged beyond repair by a flood in March 1947, requiring a temporary Bailey bridge to be used until a new concrete span was constructed in 1957. 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%. The river in Burton is crossed by a number of bridges including the ornate 19th-century Ferry Bridge that links Stapenhill to the town. At 188 by 30 feet (57.3 by 9.1m), Cromwell lock could hold a tug and three barges, and was opened on 22 May 1911. 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. 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. For the Trent this proportion is lower, but with nearly half of low flows being made up of these effluent inflows, it is still significant. [114], This was a particular problem in Stoke-on-Trent and the growing towns of the Potteries. elephant jokes from the 60's . [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. [136][137], Other managed wetland sites along the river include Beckingham Marshes, Croxall Lakes, Drakelow, and Willington Gravel Pits. [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. members of the crew were seized with pains in the chest. 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. For that I am the mere of England, that divides [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. The canal connects the Trent to the Potteries and on to Runcorn and the Bridgewater Canal. [149], The Domesday catalogue showed that there were many successful mills and fisheries along the Trent. [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. . Extended in 2012, the route now runs from Trent Lock in the south through to Alkborough where the river meets the Humber. Shortly afterwards, the river becomes the Derbyshire-Leicestershire border, passing the traditional crossing point of King's Mill, Castle Donington, Weston-on-Trent and Aston-on-Trent. 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 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. The Trent drains a large portion of south-central Ontario, including most of the Kawartha Lakes and their supplying watersheds. 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. The River Trent was a major working river until after the Second World War. [177], The primary reason for locating so many generating stations beside the Trent was the availability of sufficient amounts of cooling water from the river. [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. It shall not wind with such a deep indent, Today, Torksey is an ordinary Lincolnshire village that lies alongside the River Trent and astride the busy A156. The flood marks at Girton show that this flood was only 4 inches (100mm) lower than that of 1795, when the village was flooded to a depth of 3 feet (0.91m). [91] Eventually in 1805, they reached an agreement with Henshall & Co., the leading canal carriers, for the closure of the river above Wilden Ferry. Duke of Sutherland, describing the river in his injunction of 1902. key towns of river banniridescent telecaster pickguard. 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 River Tamar is situated in south west England and forms a natural border between the counties of Devon and Cornwall. [157], Recreational fishing is still popular, although anglers no longer line the banks as they once did. [92], The first improvement of the lower river was at Newark, where the channel splits into two. The river now flows north-east below the Toot and Trent Hills before reaching Hazelford Ferry, Fiskerton and Farndon. What is the River Trent used for? A third Act of 1892 reverted the name to the Trent Navigation Company, and this time, some improvements were performed. The mighty River Trent is one of England's major rivers. [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. [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. Welsh rhyd, "ford") in various place names along the Trent, such as Hill Ridware, as well as the Old Englishderived ford. 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. He reported that they could be treacherous to the unwary, since there were few gauges to show if the river had become too deep to cross, and that they were rarely used except by locals. [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. [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. [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. Yet Thames and Severne both in this come short of me, [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. [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. The river originates from Staffordshire, west Midlands of England, on the southern edge of Biddulph Moor. Plans for new larger locks at Beeston and Wilford were abandoned when the Trent Catchment Board opposed them. 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. At Colwick near Nottingham, the average flow rises to 83.8m3/s (2,960cuft/s), due to the combined inputs of the other major tributaries namely the Dove, Derwent and Soar. 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