Swinefleet Warping Drain | |
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History | |
Principal engineer | R Creyke |
Date of act | 1821 |
Swinefleet Warping Drain is an artificial waterway in the English county of the East Riding of Yorkshire, which was built to allow silt to be deposited on the peat moors, but now functions as a land drainage channel. It was constructed by Ralph Creyke, and the first section was completed in 1821.
Ralph Creyke was a proponent of warping, a process where silt-laden water was allowed to flow over barren land, and to deposit the silt on its surface. He lived at Rawcliffe House in Goole, [1] and was probably the first person in Yorkshire to carry out warping as a contract. His first contract was in 1812 for Francis Blackburne, where he agreed to warp 55 acres (22 ha) in Goole for a price of £1,165. His next known project was the warping of 225 acres (91 ha) in Sandhill for his client Josias Cockshutt Twisleton, while in April 1816 he obtained permission to warp 900 acres (360 ha) in Rawcliffe from the Court of Sewers. All three of these schemes used silt-laden water from the final section of the River Don, known as the Dutch River. His next major project was for "warping and otherwise improving certain moors, commons and wastes and other low grounds in the parishes of Whitgift and Snaith" and for this he obtained an Act of Parliament in 1820. [2] In order to achieve this, he constructed the Swinefleet Warping Drain southwards from the River Ouse to improve land on the edge of Thorne Moors for agriculture. The first section was completed in 1821, [3] and allowed him to warp 430 acres (174 ha) of the moors. In recognition of his achievements, he was awarded a gold medal by the Society for Encouragement of the Arts in 1825. [1]
Creyke, using his previous experience, constructed a sluice at Swinefleet Clough which was 30 feet (9.1 m) wide at the bottom and 90 feet (27 m) wide at the surface level of the land. It included two openings in the stonework, each 16 feet (4.9 m) wide, and four large pointing doors, which normally prevented the tide from entering, but could be held open by iron rods, to allow the tidal water to enter. Banks were constructed on either side of the main channel, and the drain initially ran for around 3 miles (4.8 km), with the project including land purchase and the building of the sluice costing £18,000. [4] By 1825, 1,528 acres (618 ha) were being warped, on behalf of 30 landowners, who paid £15 per acre for Creyke's services. In a letter to the Society of Arts, Creyke explained that he worked on a bigger scale and at less cost than others who had preceded him. Hence the drain was 90 feet (27 m) wide, compared to the 12 feet (3.7 m) he had previously used, the sluice was over three times wider, and he was thus able to warp 500 acres (200 ha) at a time, rather than 14 acres (5.7 ha). He also warped the land throughout the year, rather than just in the summer months. [2]
Creyke died in 1828, but his son, also known as Ralph Creyke, inherited the drain and continued the family warping business. By 1845, some 2,000 acres (810 ha) of land towards Fockerby Common were being warped, [5] facilitated by an extension of the Swinefleet Warping Drain by 4.7 miles (7.6 km) to the east. [6] The younger Creyke was subsequently involved in a large scheme to warp 1,000 acres (400 ha) of Thorne Moors, working with T H S Sotheron, for which they obtained an Act of Parliament in 1848, but the project was beset by legal delays, and work never commenced. [1] [7] Creyke continued to work with Sotheron's descendents until 1878, when he sold the warping business to Makin Durham, who was another great exponent of warping. He had built Durham's Warping Drain eastwards from the River Don in 1856, extended it further eastwards prior to 1881, and then built a southern extension to the site that later became Thorne Colliery. [8]
Around 1875, Durham formed the Yorkshire Land and Warping Company, which had its registered office at Thorne from then until 1947, when the company was wound up. Swinefleet Warping Drain was part of the assets of that company, either from 1878, [9] or maybe from 1904. [10] Makin died at the beginning of 1882 at the age of 77 yrs. [11] Gradually, the value of the moors as a source of peat for commercial exploitation became more important than their potential for agriculture, and attempts to create agricultural land dwindled. [7] Around 1900, Swinefleet Warping Drain was extended southwards, giving it a total length of around 5.6 miles (9 km) [12] The drain was used for warping land near Medge Hall, Crowle just before the start of the First World War, [1] and was last used for this purpose in 1934. [10]
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Swinefleet has long been prone to flooding, due to the low-lying nature of the land, and in 1793, an Act of Parliament was obtained to allow land within the parishes of Swinefleet and Reedness to be enclosed, and some drainage work to be carried out. [13] Another Act, obtained in 1884, created the Reedness and Swinefleet Drainage Commissioners, who managed land drainage in the area until the board was reconstituted in 1990, under the provisions of the Land Drainage Act 1976. [14] The Reedness and Swinefleet Internal Drainage Board manage 41 miles (66 km) of drainage ditches and have one pumping station. Most of the watercourses within their jurisdiction are man-made, [15] and this includes that part of Swinefleet Warping Drain which is north of the county border at Blackwater Dyke. [16] In 2019, they were considering building one or two ramps, to allow a weed-cutting boat to be used on the drain; modifications to their pumping station so that it would comply with regulations on the passage of eels along waterways; and the possibility of constructing a pumping station at the outlet of the drain, at an estimated cost of £2.5 million. [17]
Immediately to the west of Swinefleet Warping Drain, Goole Fields District Drainage Board (DDB) manage the drainage of 2,641 acres (1,069 ha) of land, where they maintain 9.48 miles (15.26 km) of drains and have one pumping station. Some of the excess water from their area enters the River Ouse through a sluice at the end of Shipcote Drain, just to the west of the Warping Drain outlet, but water is also pumped from Goole Fields Cross Drain into the Warping Drain by a pumping station. [18] The pumping station outputs between 13 Ml per day and an agreed maximum of 22 Ml per day. Since the cessation of peat extraction on the moors, large areas form the Thorne, Crowle and Goole Moors Site of Special Scientific Interest (SSSI). In order to aid the recovery of the peat moors, water levels are held significantly higher than they had been when peat extraction was taking place, and English Nature also use pumping in an attempt to maintain constant water levels. [19]
Construction of their current pumping station on Blackwater Dike commenced in late 2016, and included the installation and commissioning of a permanent Archimedes' screw pump to ensure that water levels in the peat bog are kept at an optimum level for peat regeneration. The work was commissioned by the Doncaster East Internal Drainage Board, and the principal contractor for the works was North Midland Construction PLC. The installation includes a tilting weir, which controls water levels for much of the time, but when the pump is required, it is powered by an off-grid generator, controlled by a telemetry system which uses wind and solar power. The installation was the first in the United Kingdom to use a new design of screw pump, enclosed in a vinyl ester pipe, which greatly improves its efficiency, and allows fish to travel through it without harm. [20]
The new pump is powered by electricity, derived from a battery pack which is charged by a wind generator and solar cells, with an auxiliary diesel generator which can be used if necessary. [21] The amount of water that English Nature can pump into the Warping Drain is restricted by the need to maintain the gravity outfall from Black Dyke and Reedness village, while in 2019 the new pump was out of action for several months, resulting in the old one having to be used. Goole Fields DDB consider that water flowing out of the SSSI as a result of the new regime threatens properties in the parish of Goole Fields. [19]
Swinefleet Warping Drain begins at Swinefleet Clough, an indentation in the right bank of the River Ouse, on the border between the parishes of Swinefleet and Goole Fields. Creyke's historic sluice with pointing doors has been replaced by a modern concrete construction with a flapped outlet. The sluice is situated on the north side of the A161 road, which is named Goole Road to the east and Swinefleet Road to the west. The drain is actually in Goole Fields, since the parish boundary runs along Quay Road, which runs parallel to the drain on its east bank. [22] The safety of the A161 bridge was raised in Parliament in 1939, when Mr Adam Hills MP for Pontefract stated that both it and the bridge over Earnshaw's Warping Drain to the west were unsafe, and that Goole Urban District Council had been in conversation with the West Riding of Yorkshire County Council for ten years, but had failed to reach an agreement. Captain Hudson, speaking for the government, replied that the road was scheduled to be widened, and that plans for new bridges would be available within six months. [23]
Most of the drain is in open countryside, with the only habitation nearby consisting of farm houses. The first is Field House Farm, on the left bank, where the farmhouse dates from the late 18th century, with 19th century additions at the rear. The grade II listed building is made of brown brick with a Welsh slate roof, and has two storeys with an attic. [24] Continuing to the south, Quay Road leaves the side of the drain, but the parish boundary remains on the right bank. The drain turns to a south-south-easterly direction, to be joined on its left bank by Goosefields Cross Drain. This was the location at which the Axholme Joint Railway crossed the drain, to reach Reedness Junction railway station on the right bank. Here the line to Fockerby turned off from the line to Haxey Junction. The railway was carried over the drain by a steel girder bridge, 120 feet (37 m) in length, which was the subject of an unusual request by Colonel Thompson in 1906. He asked the railway to allow a group of about 16 female potato pickers to walk through the goods yard and over the bridge, as it was the only crossing of the drain in the vicinity, and would save the ladies from having to walk a considerable distance to reach the fields. A heated Board meeting followed, but permission was given, although the Colonel had to indemnify the railway should an accident occur in which the ladies were involved. [25] Passenger services on the railway ceased in 1933, but it remained open for goods traffic until 1965. However, the rails and bridge over the drain were retained until 1972, as the section of line between Ealand and Belton was used occasionally by the Central Electricity Generating Board to move stators from Keadby Power Station across the Stainforth and Keadby Canal, until the road bridge over the canal was replaced with something more substantial. [26]
The next farm building by the drain is at Swinefleet Moor Farm, where in 1890 the drain turned to the east towards Swinefleet Peat Works and Fockerby Common. [27] By 1906, the drain continued southwards, but the section towards the peat works was still labelled Swinefleet Warping Drain. By that time a 3 ft (914 mm)-gauge railway ran parallel to the drain from the peat works, which crossed the main drain and turned southwards to run alongside the newly constructed drain. The tramway bridge is still in situ, with its rails embedded in the surface. At Blackwater Dike, which runs at right angles to the Drain on both banks, it leaves East Yorkshire and enters North Lincolnshire, as the boundary follows the Dike. In 1906, the final section of the drain was still under construction, as far as Thousand Acre Drain. [28] Beyond that point, there is a network of drains, all of which are considerably narrower than Swinefleet Warping Drain, so it is probable that it officially ends in this location. In 1966, the one that carries straight onwards was called Swinefleet Line Drain, and those that ran to Medge Hall were simply labelled "Drain". [29]
The reach of the River Ouse near the outflow of the Swinefleet Warping Drain heads in a south-westerly direction travelling upstream, and then makes a right-angle turn to the north-west. On this next reach is the outflow of Earnshaw's Warping Drain. This was cut in the 1800s by a local farmer called George Rawden Earnshaw, who lived at Manor Cottage in Old Goole. His daughter Ann married William Eden Cass in 1834, the new town of Goole's first medical practitioner. [30] A bridge carries the A161 road over the drain, with a sluice next to the road. Both are grade II listed, although only the south-western face of the bridge is visible, the rest being obscured by later earth infill, from when the road was widened. The sluice was constructed of tooled ashlar, with a wooden gate and an iron mechanism to raise or lower the gate. It was one of only two sluices in the area which retained their original hoist mechanism, the other being on the Folly Drain at Keadby, and was the most complete example when it was listed in 1987, but by 2003 the hoist mechanism had been removed. [31]
Nearby on the right bank is Goole Hall, a grade II* listed house built in 1820 for Jarvis Empson, and largely unaltered until 1985–86. [32] The drain heads in a south-south-westerly direction, passing Goole Grange, where it makes two right angle turns towards the west, and continues in the same general direction. On the edge of Goole Moors, it connects with a number of other drains that carry water from the moors. [22]
The Environment Agency measure 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 the quantity and varieties of invertebrates, angiosperms and fish. Chemical status compares the concentrations of various chemicals against known safe concentrations and is rated good or fail. [33]
The water quality for the Earnshaw's Warping Drain was as follows in 2019. Prior to 2019, the data was labelled as if it was for Swinefleet Warping Drain, but querying it with the Environment Agency led them to correct the location.
Section | Ecological Status | Chemical Status | Length | Catchment | Channel |
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Earnshaw's Warping Drain [34] | Moderate | Fail | 2.9 miles (4.7 km) | 7.99 square miles (20.7 km2) | artificial |
The main reasons for the water quality being less than good are physical modification of the channel and the leaching of nutrients into the water from agricultural land. Like many rivers in the UK, the chemical status changed from good to fail in 2019, due to the presence of polybrominated diphenyl ethers (PBDE) and mercury compounds, neither of which had previously been included in the assessment.
Crowle is a market town in the civil parish of Crowle and Ealand, on the Isle of Axholme in the North Lincolnshire unitary authority of Lincolnshire, England. The civil parish had a population at the 2011 census of 4,828. The town lies on the Stainforth and Keadby Canal.
Sir Cornelius Vermuyden was a Dutch engineer who introduced Dutch land reclamation methods to England.
The Axholme Joint Railway was a committee created as a joint enterprise between the Lancashire and Yorkshire Railway (L&Y) and the North Eastern Railway (NER) and was established by the North Eastern Railway Act of 31 July 1902. It took over the Goole and Marshland Railway, running from Marshland Junction near Goole to Reedness Junction and Fockerby, and the Isle of Axholme Light Railway, running from Reedness Junction to Haxey Junction. Construction of the Goole and Marshland Railway had begun in 1898, and by the time of the takeover in early 1903, was virtually complete. The Isle of Axholme Light Railway was started in 1899, but only the section from Reedness Junction to Crowle was complete at the takeover. The northern section opened on 10 August 1903, and the line from Crowle to Haxey Junction opened for passengers on 2 January 1905.
Adlingfleet is a drained, fertile, former marshland village and former civil parish, now in the parish of Twin Rivers, in the East Riding of Yorkshire, England. It is 6.5 miles (10.5 km) east-southeast of Goole town centre. Its sea wall along the far north-east is set back from the Ouse estuary leaving the largest single reedbed in England. In 1961 the parish had a population of 137.
The Market Weighton Canal ran 9.5 miles (15.3 km) from the Humber Estuary to its terminus near Market Weighton. It gained its act of Parliament in 1772 and opened in 1782. The 3.5 miles (5.6 km) closest to Market Weighton was abandoned in 1900 and the right of navigation through Weighton lock was lost in 1971. However, as of 2002 the lock was passable and the canal usable up to the junction with the River Foulness where silt has made it impassable. Also there is no right of navigation under the M62 motorway bridge to the north of Newport.
Hatfield Chase is a low-lying area in South Yorkshire and North Lincolnshire, England, which was often flooded. It was a royal hunting ground until Charles I appointed the Dutch engineer Cornelius Vermuyden to drain it in 1626. The work involved the re-routing of the Rivers Don, Idle, and Torne, and the construction of drainage channels. It was not wholly successful, but changed the whole nature of a wide swathe of land including the Isle of Axholme, and caused legal disputes for the rest of the century. The civil engineer John Smeaton looked at the problem of wintertime flooding in the 1760s, and some remedial work was carried out.
The Stainforth and Keadby Canal is a navigable canal in South Yorkshire and Lincolnshire, England. It connects the River Don Navigation at Bramwith to the River Trent at Keadby, by way of Stainforth, Thorne and Ealand, near Crowle. It opened in 1802, passed into the control of the River Don Navigation in 1849, and within a year was controlled by the first of several railway companies. It became part of the Sheffield and South Yorkshire Navigation, an attempt to remove several canals from railway control, in 1895. There were plans to upgrade it to take larger barges and to improve the port facilities at Keadby, but the completion of the New Junction Canal in 1905 made this unnecessary, as Goole could easily be reached and was already a thriving port.
King's Sedgemoor Drain is an artificial drainage channel which diverts the River Cary in Somerset, England, along the southern flank of the Polden Hills, to discharge into the River Parrett at Dunball near Bridgwater. As the name suggests, the channel is used to help drain the peat moors of King's Sedgemoor. There was opposition to drainage schemes from the local inhabitants, who feared that they would lose their common grazing rights. However, the main channel was constructed between 1791 and 1795, and despite some defects, brought some relief from flooding to the area.
Swinefleet is a village and civil parish in the East Riding of Yorkshire, England. It is situated approximately 2 miles (3.2 km) south-east of the town of Goole on the A161 road from Goole to Crowle. It lies on the south bank of the River Ouse. According to the 2011 UK census, Swinefleet parish had a population of 787, an increase on the 2001 UK census figure of 748. The main centre of population is at the extreme north of the parish, close to the River Ouse. The southern part of the parish is part of Swinefleet and Reedness Moors, and is characterised by drainage ditches and a few farm buildings.
Reedness is a village and civil parish in the East Riding of Yorkshire, England. It is situated approximately 3 miles (4.8 km) east of the town of Goole and lies on the south bank of the River Ouse.
The River Went is a river in Yorkshire, England. It rises close to Featherstone and flows eastward, joining the River Don just to the north of Pincheon Green.
Goole Fields is a civil parish in the East Riding of Yorkshire, England. It is situated approximately 3 miles (4.8 km) south-west of Goole town centre and lies at both sides but mainly south of the A161 road, covering an area of 1,980.59 hectares. It is bordered to the east by the Swinefleet Warping Drain, to the south by the Blackwater Dike, and to the west by the railway line from Goole to Doncaster.
Reedness Junction railway station was a railway junction near Reedness, East Riding of Yorkshire, England on the Axholme Joint Railway. Immediately to the west of the station, the Fockerby Branch, which continued eastwards, turned off from the main line to Epworth, which curved to the south.
The River Foulness is a river in the East Riding of Yorkshire, England. Its name is derived from Old English fūle[n] ēa, meaning “dirty water”. Maintenance responsibilities for the river transferred from the Environment Agency to the Market Weighton Drainage Board on 1 October 2011. Market Weighton Drainage Board subsequently amalgamated with the Lower Ouse Internal Drainage Board on 1 April 2012 to create the Ouse and Humber Drainage Board. The river discharges into the Humber Estuary via Market Weighton Canal. Water levels within the river, its tributaries and the canal are managed and controlled by the Environment Agency. The river lies in an area known as the Humberhead Levels.
The River Torne 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.
Thorne and Hatfield Moors form the largest area of lowland raised peat bog in the United Kingdom. They are situated in South Yorkshire, to the north-east and east of Doncaster near the town of Thorne, and are part of Hatfield Chase. They had been used for small-scale extraction of peat for fuel from medieval times, and probably much earlier, but commercial extraction of the peat for animal bedding began in the 1880s. The peat was cut on the moors and, once it had dried, transported to several works on 3 ft narrow gauge tramways, always called trams locally. The wagons were pulled by horses to works at Creyke's Siding, Moorends, Medge Hall, Swinefleet and Hatfield. There was also a network of canals supplying the Moorends Works.
Thorne and Hatfield Moors Peat Canals were a series of canals in South Yorkshire and Lincolnshire, England, which were used to carry cut peat from Thorne and Hatfield Moors to points where it could be processed or exported. There were two phases to the canals, the first of which lasted from the 1630s until the 1830s when coal imported on the Stainforth and Keadby Canal reduced the demand for peat as a fuel. The second started in the 1890s when peat found a new use as bedding for working horses and lasted until 1922 when Moorends Mill which processed the peat was destroyed by fire.
Warping was the former practice of letting turbid river water flood onto agricultural land, so that its suspended sediment could form a layer, before letting the water drain away. In this way poor soils were covered with fertile fine silt, and their rentable value was increased.
The Hull and Doncaster Branch is a secondary main railway line in England, connecting Kingston upon Hull to South Yorkshire and beyond via a branch from the Selby Line near Gilberdyke to a connection to the Doncaster–Barnetby line at a junction near Thorne 8 miles north-east of Doncaster.
Crowle Peatland Railway is a railway museum based on the peat moors at Crowle in North Lincolnshire, England.
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