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Sir Cornelius Vermuyden ( Dutch pronunciation: [kɔrˈneːlijəs fərˈmœydə(n)] ; 1595 – 11 October 1677) was a Dutch engineer who introduced Dutch land reclamation methods to England.

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62-600: (Redirected from River Torne ) Torne may refer to: River Torne (England) , a river in South Yorkshire and Lincolnshire, England Torne (Finnish and Swedish river) , a river in Finland and Sweden PlayTV#Torne , a Japanese PlayStation 3 accessory See also [ edit ] Thorne (disambiguation) Topics referred to by the same term [REDACTED] This disambiguation page lists articles associated with

124-518: A Dutch haberdasher to whom Vermuyden was related by marriage. This, or perhaps work at Windsor , brought him to the notice of Charles I , who commissioned him in 1626 to drain Hatfield Chase in the Isle of Axholme , Lincolnshire . The King was Lord of the four principal manors there: Hatfield , Epworth , Crowle and Misterton , as well as 13 of the adjacent manors, and he wanted to expand

186-495: A short distance it has dropped below the 49-foot (15 m) before it is crossed by the A60 Oldcotes to Tickhill road at the foot of Malpas Hill. It turns to the north to pass under the embankment of the dismantled railway which used to serve Firbeck Colliery at Langold , and the industrial railway which serves Harworth Colliery. The river is joined by a number of drainage dikes and ditches as it crosses Tickhill Low Common, to

248-620: A well between Loversall and Balby joins at the northern edge of the spoil heap. The channel is embanked at a number of locations from here onwards. To the north of Rossington it turns to the east to pass under the East Coast Main Line railway, and then the A638 Great North Road at Rossington Bridge, which it shares with the Mother Drain. This drains the area around Doncaster International Railport and

310-601: A year later, Smeaton produced a detailed report on the Torne, and work began, but some alterations were made as the scheme progressed. Scott suggested that the northern drain should be re-routed to Keadby, and then steered the bill through Parliament. The Act of Parliament was obtained in March 1783, before he retired in June. Samuel Foster replaced him, built the new drain and outfall at Keadby, and built separate outfalls at Althorpe for

372-599: Is a river in the north of England, which flows through the counties of South Yorkshire and North Lincolnshire . It rises at the Upper Lake at Sandbeck Hall, in Maltby in South Yorkshire, and empties into the River Trent at Keadby pumping station. Much of the channel is engineered, as it plays a significant role in the drainage of Hatfield Chase , which it crosses. The first major change occurred around 1628, when

434-638: Is also the namesake for the Vermuyden Group of South Yorks, a Long Distance Walkers Association based in South Yorkshire, and the Vermuyden Concert Band, the most senior Saturday afternoon band at William Appleby Music Centre in Doncaster. His motto Niet Zonder Arbyt ("Nothing Without Work") was adopted as the official motto of South Cambridgeshire District Council . The motto was adopted by No. 3 Group RAF and it appears in

496-530: Is some inconclusive evidence that one of his nephews may have acted as a colonel of horse in the parliamentary army, alongside Oliver Cromwell in the Eastern Association army. But with the beginning of the second phase of Bedford-led construction, Vermuyden was again appointed as the director of the works in January 1649/50. This second phase included continuing the work of both the first and

558-476: The Isle of Axholme , and then turned to the east for 3 miles (4.8 km), where it entered the Trent at a sluice near Althorpe. At the same time, a drain was constructed which ran northwards from Idle Stop in a straight line for 8 miles (13 km) to Dirtness. It passed under the new channel of the Torne at Tunnel Pits. At Dirtness it was joined by another new drain, some 3 miles (4.8 km) long, flowing in from

620-649: The M180 motorway . As it turns to the east again, the Folly Drain also runs parallel, but a little beyond the A161 bridge, the two drains continue to the east, while the river diverts to the north, to run parallel to the North Engine Drain. The Hatfield Waste Drain runs parallel to the North Engine Drain on its south bank, but after the approach on the Torne, there was nowhere for it to go, and so it passes under

682-629: The Potteric Carr Nature Reserve , and the flows combine after the bridge, near the site of some Roman pottery kilns and Wheatcroft fishing lakes. Next to cross are the Doncaster to Gainsborough railway line and the B1396 road at Auckley Bridge. The Aldam Drain drains Cantley Low Common, and beyond the junction, the river becomes a high level carrier, with permanent embanking of both banks, and catchwater drains running along

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744-493: The River Trent at Keadby was by gravity until 1940, when the pumping station was built to assist when water levels in the Trent are too high to allow for gravity discharge. Six 60-inch (150 cm) Gwynnes pumps were powered by 420 hp (310 kW) Crossley diesel engines, but one of them was replaced by an electric motor in 1994, when the engines were refurbished by the National Rivers Authority . It

806-652: The Royal Society in 1663. He had a total of nine children with Katherine, including Charles, Deborah, Elizabeth, and John. His second wife was Dionysia Stonhouse. Vermuyden lived in Maiden Lane, Covent Garden in 1647 and had a home in Kelfield , North Lincolnshire . Vermuyden died on 11 October 1677 in London . Despite the initial success of the reclamation, the engineers did not understand enough about

868-668: The Somerset Levels and Malvern Chase in Worcestershire ; he also entered into a partnership in the lead mines in Wirksworth , which he drained by means of a sough . Contrary to popular belief, Vermuyden was not involved with the draining of the "Great Fen " in Cambridgeshire and Norfolk in the 1630s. He did not participate until the second phase of construction in the 1650s. This area of marshland

930-512: The Wissey , Little Ouse and Lark , away from Denver. As a result, the area suffered continued flooding, which was not controlled until a project of the early 1960s. Due to the high cost of labour, and the continuing unpopularity of the project among the local inhabitants, the government provided Vermuyden with Scottish and Dutch prisoners of war (after the Battle of Dunbar in 1650) and the start of

992-715: The Zeeland province of the Dutch Republic . He trained in the Netherlands as an engineer, learning Dutch techniques for controlling water and draining marshland. By the period of 1621 to 1623, Vermuyden was working in England, where his first projects were on the River Thames , repairing a sea wall at Dagenham and working to reclaim Canvey Island , Essex . The latter project was financed by Joas Croppenburg,

1054-467: The 1760s for the fourth Earl, and the interior was remodelled for the ninth Earl by William Burn in 1857. The grounds were landscaped by Capability Brown , and he created the Upper Lake and the Lower Lake, from which the river flows. The Upper Lake is close to the 130-foot (40 m) contour, but the outlet to the river is at the 98-foot (30 m) contour. The river flows to the east, and within

1116-590: The 1970s, to handle water from the Middle Drain, which crosses an area affected by mining subsidence. It was managed on behalf of the Coal Board by Tickhill Internal Drainage Board (IDB), now part of Doncaster East IDB. There are Environment Agency pumping stations at Candy Farm and Tunnel Pits. Before 1628, much of the area through which the River Torne now passes was waterlogged, and the river system

1178-456: The Folly Drain. The River Torne used to continue eastwards to a sluice at Althorpe, but the sluice is no more and the channel drains in the reverse direction. The South Engine Drain, which was built as part of improvements made in 1795, used to pass under the Torne and the road through another grade II listed syphon, which dates from 1813. The syphon is now redundant, since the channels have been connected together. Three parallel channels, known as

1240-712: The King's (1.5 phase). In addition, he dredged the New Bedford River (with a large area of wash between it and the Bedford River) and the Forty Foot Drain . He established Denver Sluice to stop tides and flood water from depositing silt into the Great Ouse to the east of Ely . The work did not include his projected "cutoff channel," which was designed to take flood water from the southern rivers,

1302-425: The King's takeover of their project and to gain restoration of all of the 95,000 acres (380 km ) first awarded in January 1630/31. By 29 May 1649, a few months after the King's execution, they had succeeded; an Act of Parliament (later known as "The Pretended Act") restored them to the undertaking and gave their claim to the enclosures the force of law. Before this time, Vermuyden's activities are not clear; there

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1364-731: The Nene through the salt marshes to the sea. Vermuyden was still working in the Great Level as of May 1642, but was by then responding to the House of Lords , rather than the beleaguered King. Having received perhaps less than £5000, the engineer was continually in arrears for the wages of his workmen. During the Civil War , the drainage project was halted by the chaos of war. The original financiers – now headed by Bedford's heir William – began to seek an Act of Parliament to overturn

1426-589: The North Engine Drain to its north bank through a grade II listed syphon, which was probably built by Samual Foster in 1795 or by Thackray in 1813 as part of a series of improvements recommended by the engineer John Rennie . The three parallel channels, with the A18 running to the south of the Hatfield Waste Drain, arrive at Pilfrey Bridge, where they are joined by the South Engine Drain and

1488-499: The Three Rivers, flow to the north east, passing under the Doncaster to Scunthorpe railway, to arrive at Keadby pumping station. The Environment Agency assesses the water quality of the river systems in England. Each is given an overall ecological status, which may be one of five levels: high, good, moderate, poor and bad. There are several components that are used to determine this, including biological status, which looks at

1550-404: The Torne and the southern drain. The reconstruction was completed by 1789. In 1813, the South Engine Drain was routed under the Torne through a syphon, and became the third of the Three Rivers. The 1887 Ordnance Survey map shows only the Torne flowing eastwards from Pilfrey Bridge. As it approaches Althorpe, it splits into two, and uses both of the sluices into the Trent. The Folly Drain turns to

1612-546: The Torne from where it crosses the A60 road to a little below the junction with the Middle Drain, has been managed by the Tickhill Internal Drainage Board since 1931. They are responsible for an area of 10 square miles (26 km ), which includes 9 miles (14.5 km) of watercourses. Most of these flow into the Torne by gravity, but the Middle Drain has suffered from subsidence, and a pumping station

1674-458: The Trent in the 1780s, but the Torne was not re-routed to it until much later. The sluice at Keadby became a pumping station in 1940, and the option to pump water into the Trent at all states of the tide led to the abandonment of the Althorpe outfall, and the routing of the Torne to Keadby. There are a number of pumping stations along the course of the river. Tickhill pumping station was built in

1736-473: The area, together with two branch drains. These were completed by 1768. Doncaster Corporation then divided up the Carr and enclosed it, and when this was completed in 1771, Trustees took over the management of the scheme. Further work was done between 1772 and 1777, again with Tofield directing, and Mathias Scott acting as resident engineer and surveyor. By the time the scheme was completed, 4.6 miles (7.4 km) of

1798-631: The case of the Ruddle to St Catherine's Well section, leaching of cadmium and zinc compounds from abandoned mine workings. Like most rivers in the UK, the chemical status changed from good to fail in 2019, due to the presence of polybrominated diphenyl ethers (PBDE), perfluorooctane sulphonate (PFOS) and mercury compounds, none of which had previously been included in the assessment. Download coordinates as: [REDACTED] Media related to River Torne at Wikimedia Commons Cornelius Vermuyden Vermuyden

1860-522: The common fen in his right of "improvement" as the Lord of the Manor , leaving one-third for those local residents who had common rights of pasturage in the fens. The local people were upset by the project, particularly those of the Manor of Epworth , whose lord had already enclosed part of the commons in the 14th century. He had later signed a legal document giving up all subsequent rights of enclosure within

1922-412: The cultivable area. Vermuyden was to receive one third of the drained land, most of which had previously been commons , as recompense for his investment. To finance the drainage project, he sold shares in this land to other investors, including some fellow Dutchmen. Some French and Walloon Protestant refugees also settled in the area as landowners or tenants. The King intended to enclose one third of

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1984-404: The drainage engineer Cornelius Vermuyden cut a new channel for the river across the Isle of Axholme , and built a sluice at Althorpe where it entered the River Trent . Nearly 90 years of civil unrest followed, before the issues of flooding were finally resolved. Drainage of the land bordering the river was carried out in the 1760s and 1770s. A new sluice was built at Keadby, lower downstream on

2046-422: The ecology of the fens. The drying of the land caused the peat to shrink greatly, lowering the remaining land below the height of the drainage channels and rivers. This caused the reclaimed farmland to become vulnerable again to flooding. By the end of the 17th century, much of the reclaimed land was regularly flooded. This continued until the development of steam-powered pumps in the early 19th century. The drop in

2108-549: The extra depth at Potteric Carr, since the flow increases depending on the ratio of the cross-sectional area to the wetted perimeter, when the gradient of the channel is less than 4 inches per mile (6 cm per km). The sluice which connected the Mother Drain to the Torne was designed by Scott in 1772. Scott resigned his post in April 1774, to move to Thorne and to work for the Trustees of Hatfield Chase. One of his first suggestions

2170-463: The extra water that cannot drain to the sea – and a catchdrain around the eastern edge of the fen. The washes were constructed as part of the second phase of drainage in the 1650s, but the catchdrain was not developed until the early 1960s. This catchdrain follows the contours of the western edge of the hilly brecklands where they rise above the fen, commencing in the south at Mildenhall through Hockwold cum Wilton northwards to Denver Sluice . At

2232-570: The foot of both banks. At Candy Farm there are two pumping stations, the southern one pumping the Black Bank Drain into the river, and the northern one pumping the East Ring Drain. At Tunnel Pits, there are two more pumping stations, and Tunnel Pits Bridge carries the road which follows Vermuyden's North Idle Drain over the channel. Soon, the South Engine Drain is running parallel to the river, as it crosses under Sandtoft Road and

2294-423: The land level can be seen at the pumps near Ramsey Forty Foot , where animal-powered pumps, steam pumps and now fossil-fuel pumps are all co-located, at different heights. They demonstrate both the development of technology and the resulting decline in land levels. Prickwillow Museum has a large pumping engine in working order, but not actively used. Vermuyden has several locations named after him, including: He

2356-455: The land subject to winter flooding. The Merchant Adventurers had been offered 95,000 acres (380 km ) by the Crown as the reward for their work. This settlement was disrupted: first by the riots, which erupted against the enclosures (and that occurred periodically into the 1650s), and second, by the King. He reversed the granting of Bedford's contract and declared himself as the principal in

2418-520: The latter village the River Little Ouse flows westwards off the brecks from Brandon enclosed within high embankments, over an aqueduct many feet higher than the catchment drain and surrounding farmland. Thus illustrating many of the anachronistic but brilliant features (in engineering terms), the work of Vermuyden commenced. Charles I appointed Vermuyden as his agent for the draining on 19 September 1639, but his government did not approve

2480-535: The length of the River Great Ouse by many miles. It was eventually named the Bedford River (subsequently Old Bedford River ) after Francis Russell, 4th Earl of Bedford , who was the chief Adventurer and financier. The project created or improved eight other channels. The operation was judged as substantially complete in 1637. It was criticized for its limited goal to provide "summer lands", leaving

2542-536: The manor. As with other fen drainage schemes at the time, the locals did not oppose drainage per se, but were outraged about the large enclosures of their common pasture and turbary fens. This threatened their commons rights and livelihoods, as they depended on the fens for pasturage and for peat for burning as fuel. From 1627, the richer members of the community challenged the project in court by lawsuits, even as large groups of commoners (not necessarily poor people, but including some substantial farmers) rioted against

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2604-568: The maximum volume of water which the river could deliver, and the agricultural land was subject to flooding. There was dissatisfaction among the inhabitants of the Hatfield Chase area with the effects of the drainage scheme, which resulted in riots and damage to the work. A series of lawsuits followed, and the situation was not finally resolved until 1719. In the 1760s, there were plans to drain Potteric Carr , an area of wetland to

2666-468: The plan until 5 August. In a precarious position with all three of its kingdoms, the Crown lacked both sufficient funds and attention to pay for the works in the Great Level, but it authorized Vermuyden to start. He widened the River Nene below Horseshoe Sluice, banking the north side of Morton's Leam. Beginning on the south, he set a new sluice, known as Shire Drain, and cut a new channel at the mouth of

2728-573: The project, taking 52,000 acres (210 km ) and leaving the other parties with only 40,000 acres (160 km ). At this time, Vermuyden was recruited to participate in the Great Level, as in 1637 he wrote a Discourse Touching the Draining of the Great Fennes for the King (it was not published until 1642). In it, he proposed two innovations to the drainage scheme: washes – areas of land allowed to flood in periods of bad weather to absorb

2790-445: The quantity and varieties of invertebrates , angiosperms and fish. Chemical status, which compares the concentrations of various chemicals against known safe concentrations, is rated good or fail. The water quality of the Torne was as follows in 2019. Reasons for the ecological quality being less than good include discharge from sewage treatment works, disharge from the transport infrastructure, runoff from agricultural land, and in

2852-404: The river channel had been rerouted, the Mother Drain had been extended to 4.5 miles (7.2 km), and 3 miles (4.8 km) of catchwater drains had been built. The fall on the Mother Drain was very low, but Smeaton had designed it with a channel, the bottom of which was below the level of the outfall. In a separate dispute over the design of drains for Deeping Fen , he explained how he had used

2914-537: The river just before it crosses the 16-foot (4.9 m) contour, and the western bank is embanked as it passes Reedy Holmes Plantation. Already the meandering course of the river has been replaced by straight sections with tight bends. The Little Mother Drain, which drains Stancil Carr and Wellingley Low Grounds, joins before the river passes around the western edge of the huge spoil heap of Rossington Main Colliery, and St Catherine's Well Stream, which flows eastwards from

2976-561: The rivers. The Don was routed northwards from Stainforth, to join the River Aire near Turn Bridge near East Cowick (grid reference SE668215), while the Idle was dammed at Idle Stop, and routed eastwards to join the Trent at West Stockwith . This left the Torne with no outfall, and a completely new channel was constructed for it, which was embanked on both sides. It ran in a north-easterly direction from Wroot for 6 miles (9.7 km), crossing

3038-443: The south and joins the Trent at Derrythorpe. By 1946/51, maps show a connection between the Torne and the middle of the Three Rivers, with a connection between the middle channel and the east channel downstream of Pilfrey Bridge. By 1966, the channels are inter-connected much as they are today, with a sluice between the Folly Drain and the South Engine Drain, and the sluices at Althorpe and Derrythorpe no longer used. The outlet into

3100-685: The south of Tickhill . The common and the river are crossed by the Doncaster Bypass section of the A1(M) motorway , which is built on an embankment here and was one of the earliest motorways built in Britain, opening in July 1961. Next it passes under the A631 Tickhill to Bawtry road at Goole Bridge. The river carries the alternative name of Goole Dike at this point. The Middle Drain joins

3162-402: The south of Doncaster covering 4,250 acres (1,720 ha). The engineers John Smeaton and James Brindley were responsible for the plans, but Thomas Tofield, a botanist and civil engineer who lived nearby at Balby , directed the project when work began in 1765 or 1766. The first stages involved a new channel for the Torne, and the construction of the Mother Drain, the main drainage channel for

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3224-467: The title Torne . If an internal link led you here, you may wish to change the link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Torne&oldid=1180552532 " Category : Disambiguation pages Hidden categories: Short description is different from Wikidata All article disambiguation pages All disambiguation pages River Torne (England) The River Torne

3286-730: The war with the Dutch respectively) as labourers in this phase of construction. Vermuyden's relationship with the other adventurers was never easy and, by 1655, they had parted company altogether. Several other of his initiatives failed, including a proposal for a treaty between England and the States-General of the Netherlands which he made to Cromwell. In addition, Vermuyden was unable to gain support to drain his areas of Sedgemoor and Malvern Chase . Vermuyden married Katherine Lapps on 16 November, 1623, at St Mary's, Rotherhythe. One son, Cornelius Vermuyden Jr., became an Original Fellow of

3348-481: The west, and the combined flow was carried to the east for a further 5 miles (8 km), to enter the Trent at another sluice at Althorpe. The Torne sluice was 11 feet (3.4 m) wide, and the sluice on the drain was 14 feet (4.3 m) wide. The new route of the Torne was not entirely successful. It crossed fertile parture land to the north-west of the Isle of Axholme, but the banks were not sufficiently large to hold

3410-575: The works and the enclosures. Because the legal position of the commoners of Epworth was unique, the legal debate over the drainage and enclosures lasted into the eighteenth century. Vermuyden was knighted in 1629 for his work, and became a British citizen in 1633. In 1631 he built the Horseshoe Sluice on the tidal river at Wisbech , Isle of Ely , Cambridgeshire at a cost of £8,000, by a "little Army of Artificers Venting, contriving and acting outlandish devises" The work on Hatfield Chase

3472-527: Was commissioned by the Crown to drain Hatfield Chase in the Isle of Axholme , Lincolnshire . In the 1650s, he directed major projects to drain The Fens of East Anglia , introducing the innovation of constructing washes , to allow periodic flooding of the area by excess waters. Cornelius was the son of Gillis Vermuyden and Sarah Werkendet. He was born in 1595 in Haestinge on the Isle of Tholen in

3534-576: Was installed in the 1970s to overcome this. The IDB operates the station on behalf of the National Coal Board , who own it. In April 2012, Tickhill IDB became part of the much larger Doncaster East Internal Drainage Board. The River Torne rises in the grounds of Sandbeck Hall , the home of the Earl of Scarborough . The house is a grade I listed structure, and was originally built in 1626 for Sir Nicholas Saunderson. James Paine extended it in

3596-635: Was naturally drained by a labyrinth of rivers. It had been inadequately maintained since before the Dissolution of the Monasteries in 1537 during the English Reformation , as the monasteries had been chiefly responsible in the region for keeping the channels clear. The initial plan for the drainage was based on a proposal by John Hunt in 1604-1605, to construct a new river 21 miles (34 km) long from Earith to Denver , shortening

3658-450: Was only partially successful: the straightening of the river Don and outlet into the Aire caused flooding in Fishlake , Sykehouse and Snaith . As a result of a lawsuit in 1633, Vermuyden dug the Dutch River , which provided a direct route from the Don to the River Ouse at Goole . It required him to deplete most of the land that he had acquired in the Chase. The same year he bought 4,000 acres (1,619 ha) of land in Sedgemoor on

3720-413: Was quite different. The River Don flowed across Hatfield Chase from Stainforth to Adlingfleet . The River Idle flowed northwards from the point later called Idle Stop, and joined the Don near to Sandtoft , while the Torne formed two channels to the west of Wroot , both of which joined the Idle. In 1626, Cornelius Vermuyden was given the task of draining Hatfield Chase, and he radically altered

3782-424: Was the availability of power, which enabled water to be discharged to the Trent at all states of the tide that led to the routing of the Torne and the Folly Drain to Keadby, and the abandonment of the Althorpe and Derrythorpe outfalls. Following the passing of the Land Drainage Act 1930 , internal drainage boards were set up to manage low-lying areas prone to flooding. The area to the east of Tickhill, surrounding

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3844-427: Was to divert the Torne out of the Chase altogether, by making a new cut for it to the River Don at Thorne. Thomas Yeoman proposed an alternative scheme, which involved routing the drains away from Althorpe to a new outfall some 4 miles (6.4 km) downstream on the Trent. Scott produced a report on both schemes in October 1775, but the cost of acquiring the land outside of the Chase was a major disadvantage. Exactly

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