The New River is a drainage system in the South Holland district of Lincolnshire, England. Rising just east of Sisson's Farm near Crowland it flows very roughly eastwards, following the general line of the River Welland but a little to the south. It skirts the settlements of Crowland and Cowbit before flowing into the Welland at Cradge Bank near Little London.
Crowland Inclosure Act 1801 | |
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Act of Parliament | |
Long title | An Act for draining, dividing, and inclosing a Common, called Crowland Common, otherwise Goggushland, and certain open Half-year's Meadow, Commonable, and Waste Grounds, called The Washes and Fodder Lots, in, adjoining, or near the Township of Crowland, in the County of Lincoln. |
Citation | 41 Geo. 3. (U.K.) c. cxvi |
Dates | |
Royal assent | 23 June 1801 |
Text of statute as originally enacted |
The land enclosed between the Welland and the New River is referred to as Washland, Crowland Wash and Cowbit Wash being the principal areas. Washland was designed to be sacrificially flooded as a relief of high river levels. The current land usage, and the rights of the drainage authorities to flood it can be traced back at least to an act of parliament of George III, [1] and amended in 1847. [2] The arrangement is not theoretical. Cowbit Wash was flooded annually to protect Spalding until the creation of the Coronation Channel allowed excess water to bypass the town. Even now the option to overspill onto the Wash is available. [3]
Although it is customary to say the washes lie between the Welland and the New River, it is more accurate to say that there is an extra bank to the Welland to the south of the New River. It is this bank that restrains the spreading floodwaters: the New River lies in the bottom of this basin to remove the waters. This earthen bank can be seen on the left of the Cloot House photograph above. The availability of a suitable geological feature on which to build this bank determined the shape of the washes, and its location can be traced back through antiquity. To quote Wheeler: [4]
The right bank of the Welland between Crowland and Spalding is placed at a distance from the channel of the river varying from a quarter to half a mile leaving an area of about 2500 acres which is covered with water whenever the Welland is in flood. The depth of water in this land in high floods is as much as 5 feet. Originally, no doubt, the land by the side of the Wellland was little better than a Morass, and the banks were placed on the nearest firm ground.
Crowland or Croyland is a town in the South Holland district of Lincolnshire, England. It is situated between Peterborough and Spalding. Crowland contains two sites of historical interest, Crowland Abbey and Trinity Bridge.
The Wash is a rectangular bay and multiple estuary at the north-west corner of East Anglia on the East coast of England, where Norfolk meets Lincolnshire and both border the North Sea. One of Britain's broadest estuaries, it is fed by the rivers Witham, Welland, Nene and Great Ouse. It is a 620 km² biological Site of Special Scientific Interest. It is also a Nature Conservation Review site, Grade I, a National Nature Reserve, a Ramsar site, a Special Area of Conservation and a Special Protection Area. It is in the Norfolk Coast Area of Outstanding Natural Beauty and part of it is the Snettisham Royal Society for the Protection of Birds nature reserve.
The River Welland is a lowland river in the east of England, some 65 miles (105 km) long. It drains part of the Midlands eastwards to The Wash. The river rises in the Hothorpe Hills, at Sibbertoft in Northamptonshire, then flows generally northeast to Market Harborough, Stamford and Spalding, to reach The Wash near Fosdyke. It is a major waterway across the part of the Fens called South Holland, and is one of the Fenland rivers which were laid out with washlands. There are two channels between widely spaced embankments with the intention that flood waters would have space in which to spread while the tide in the estuary prevented free egress. However, after the floods of 1947, new works such as the Coronation Channel were constructed to control flooding in Spalding and the washes are no longer used solely as pasture, but may be used for arable farming.
The Fens, also known as the Fenlands, in eastern England are a naturally marshy region supporting a rich ecology and numerous species. Most of the fens were drained centuries ago, resulting in a flat, dry, low-lying agricultural region supported by a system of drainage channels and man-made rivers and automated pumping stations. There have been unintended consequences to this reclamation, as the land level has continued to sink and the dykes have been built higher to protect it from flooding.
The Old Bedford River is an artificial, partial diversion of the waters of the River Great Ouse in the Fens of Cambridgeshire, England. It was named after the fourth Earl of Bedford who contracted with the local Commission of Sewers to drain the Great Level of the Fens beginning in 1630. It provided a steeper and shorter path for the waters of the Great Ouse, and was embanked to prevent them flooding the low ground of the South Fens. Throughout the project, the Earl and his Adventurers faced disruption from those who were opposed to drainage schemes. The project was deemed to have succeeded in draining the fens in 1637, but that decision was reversed in 1638. After a lull during the English Civil War, when much of the work was damaged, the Dutch engineer Cornelius Vermuyden worked with William Russell, the fifth Earl of Bedford to complete the drainage. Disruption and unrest continued while the work was carried out, resulting in the Adventurers employing armed guards. A second river, the New Bedford River, was cut parallel to the first channel, which then became the Old Bedford River. At some point, the Old Bedford River was split into two parts, when the upper section was diverted into the River Delph at Welches Dam, and the lower section was joined to the Counter Drain. Both parts retain the name, but are not connected to each other. The area between the two Bedford rivers acts as a large washland, which holds floodwater when the river channels cannot cope with the volume of water in them.
The New Bedford River, also known as the Hundred Foot Drain because of the distance between the tops of the two embankments on either side of the river, is a navigable man-made cut-off or by-pass channel of the River Great Ouse in the Fens of Cambridgeshire, England. It provides an almost straight channel between Earith and Denver Sluices. It is tidal, with reverse tidal flow being clearly visible at Welney, some 19 miles (31 km) from the sea.
Ouse Washes is a linear 2,513.6-hectare (6,211-acre) biological Site of Special Scientific Interest stretching from near St Ives in Cambridgeshire to Downham Market in Norfolk. It is also a Ramsar internationally important wetland site, a Special Protection Area for birds, a Special Area of Conservation and a Nature Conservation Review site, Grade I. An area of 186 hectares between March and Ely is managed by the Wildlife Trust for Bedfordshire, Cambridgeshire and Northamptonshire and another area near Chatteris is managed by the Royal Society for the Protection of Birds. The Wildfowl & Wetlands Trust manages another area near Welney.
The River Glen is a river in Lincolnshire, England with a short stretch passing through Rutland near Essendine.
Spalding is a market town on the River Welland in the South Holland district of Lincolnshire, England. The town had a population of 31,588 at the 2011 census. The town is the administrative centre of the South Holland District. The town is located between the cities of Peterborough and Lincoln, as well as the towns of Bourne, March, Boston, Wisbech, Holbeach and Sleaford.
South Holland is a local government district of Lincolnshire. The district council is based in Spalding. Other notable towns include Crowland, Holbeach and Long Sutton. The district is named after the historical division of Lincolnshire known as the Parts of Holland.
The South Forty-Foot Drain, also known as the Black Sluice Navigation, is the main channel for the land-drainage of the Black Sluice Level in the Lincolnshire Fens. It lies in eastern England between Guthram Gowt and the Black Sluice pumping station on The Haven, at Boston. The Drain has its origins in the 1630s, when the first scheme to make the Fen land available for agriculture was carried out by the Earl of Lindsey, and has been steadily improved since then. Water drained from the land entered The Haven by gravity at certain states of the tide until 1946, when the Black Sluice pumping station was commissioned.
Bourne Eau is a short river which rises from an artesian spring in the town of Bourne in Lincolnshire, England, and flows in an easterly direction to join the River Glen at Tongue End. Within the town, it once powered three water mills, one of which is now a heritage centre. At Eastgate, it becomes much wider as it was navigable in the 18th and 19th centuries, and this was the location of the terminal basin. Below the town it is an embanked river, as its normal level is higher than that of the surrounding Fens. Navigation ceased in the 1860s and the river now forms an important part of the drainage system that enables the surrounding fen land to be used for agriculture.
The Deepings are a series of settlements close to the River Welland near the borders of southern Lincolnshire and north western Cambridgeshire in eastern England. Peterborough is about 8 miles to the south, Spalding about 10 miles to the north east and Stamford about 8 miles to the west.
The Fens Waterways Link is a project to improve recreational boating opportunities in the counties of Cambridgeshire and Lincolnshire, England. By a combination of improvements to existing waterways and the construction of new links a circular route between Lincoln, Peterborough, Ely and Boston is planned. The project is being organised by the Environment Agency and financed from the Regional Development Agency and the European Union.
Cowbit is a village and civil parish in the South Holland district of Lincolnshire, England. The population of the civil parish at the 2011 census was 1,220. It is situated 3 miles (5 km) south from Spalding and 5 miles (8 km) north from Crowland.
The A1175 road is a road in south-west Lincolnshire, England. It runs between Stamford and Spalding, along the old A16 route.
Pode Hole is a village in South Holland, Lincolnshire, England. It is 2 miles (3.2 km) from Spalding and a similar distance from Bourne. The village lies at the confluence of several drainage channels, where two pumping stations discharge water into Vernatt's Drain from land in Deeping Fen to the South and West. Water from Pinchbeck South Fen to the North is also lifted into Vernatt's Drain. The village arose to service the pumping stations.
Deeping Fen is a low-lying area in the South Holland district of Lincolnshire, England, which covers approximately 47 square miles (120 km2). It is bounded by the River Welland and the River Glen, and is extensively drained, but the efficient drainage of the land exercised the minds of several of the great civil engineers of the 17th and 18th centuries.
South Holland IDB is an English internal drainage board set up under the terms of the Land Drainage Act 1930. It has responsibility for the land drainage of 148.43 square miles (384.4 km2) of low-lying land in South Lincolnshire. It is unusual as its catchment area is the same as the area of the drainage district, and so it does not have to deal with water flowing into the area from surrounding higher ground. No major rivers flow through the area, although the district is bounded by the River Welland to the west and the River Nene to the east.
The Cut-off Channel is a man-made waterway which runs along the eastern edge of the Fens in Norfolk and Suffolk, England. It was constructed in the 1950s and 1960s as part of flood defence measures, and carries the headwaters of the River Wissey, River Lark and River Little Ouse in times of flood, delivering them to Denver Sluice on the River Great Ouse. In the summer months, it is also used as part of a water supply scheme for drinking water in Essex.
Historically, Cowbit and Crowland Washes were flooded each winter to protect Spalding. Since the construction of the Coronation Channel this is no longer required. However, the area remains a safety valve at times of flood risk.