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Adventurers were groups of English engineers and wealthy landowners, who funded large-scale land drainage projects in the seventeenth century, in return for rights to some of the land reclaimed.
Land drainage works were expensive, and were usually undertaken in sparsely populated areas. In the seventeenth century a number of such schemes were carried out by Adventurers, who acted under parliamentary sanction, but who financed the works carried out themselves. In return, they gained rights to the land reclaimed as a result of the civil engineering works.
One such scheme was the draining of the Bedford Levels. The Bedford Level Corporation was in charge of the works, which when conceived in 1630, would create large tracts of "summer lands", which would be suitable for grazing during the summer months, but would still be liable to flooding in the winter. Funds for the work were provided by the Earl of Bedford and thirteen other Adventurers. Of the land reclaimed, the fourteen men were to receive 43,000 acres (170 km2), to be shared between them, while 12,000 acres (49 km2) were to be given to the king, and another 40,000 acres (160 km2) were designated to provide income to maintain the works once they were completed. The Dutch engineer Cornelius Vermuyden was employed to carry out the work, and on 12 October 1637, it was judged to be complete, when the Court of Sewers met at St Ives. However, there was dissatisfaction with the decision, and the Royal Commission of Sewers overturned it in 1639, when they met at Huntingdon. An Act of Parliament passed in 1649 authorised the fifth Earl of Bedford to carry out further work, so that the land could be used throughout the year for agriculture. Another Act followed in 1660, but after initial improvements, the schemes gradually deteriorated, and the Bedford Level Corporation found it increasingly difficult to find anyone prepared to invest their money, when the outcome was so full of risk. [1]
As well as the engineering challenges faced by the Adventurers, there was also opposition from those who judged that their livelihood was affected by the works. In 1631, a group of Adventurers led by Sir Anthony Thomas [2] were authorised to drain the East Fen, the West Fen and the Wildmore Fen, to the north and west of Boston, Lincolnshire. They spent some £30,000 on the work, and received 16,300 acres (66 km2) of the drained land. They subsequently spent £20,000 on improvements and buildings, and the land generated some £8,000 per year in rent. [3] The land had previously been extra-parochial, on which people from adjacent villages had grazing rights. [4] After seven years, the Commoners rioted in 1642, breaking down the sluices, destroying crops, and demolishing houses. The Adventurers took their case to the House of Lords, who passed a bill for the "relief and security of the drainers", but the House of Commons were less supportive, refusing to take sides. They ordered that the Sheriff and the local Justices of the Peace should act to prevent and suppress riots. The Commoners then took their grievances to court, and won. [5] The outcome was that when the monarchy was restored in 1661, management of the Fens returned to the Court of Sewers, and remained in a poor state until the mid eighteenth century. [6]
To the south of Boston, the Earl of Lindsay and another group of Adventurers faced similar problems. Having reached an agreement with the Court of Sewers, they worked on draining the Lindsay Levels, the main feature of which was the South Forty-Foot Drain, running for 24 miles (39 km) from Bourne to Boston. The land reclaimed was suitable for agriculture, and in 1636 they took possession of it, building houses and growing crops. Again, Commoners and Fenmen felt that they had been dispossessed, and attempted to get Parliament to rule in their favour. After three years, they gave up their attempts at a legal solution, and took direct action, destroying the drains, buildings and crops. In the political turmoil of the time, just prior to the start of the Civil War, the Adventurers received no compensation for their loss. [7]
The River Witham is a river almost entirely in the county of Lincolnshire in the east of England. It rises south of Grantham close to South Witham at SK8818, passes through the centre of Grantham, passes Lincoln at SK9771 and at Boston, TF3244, flows into The Haven, a tidal arm of The Wash, near RSPB Frampton Marsh. The name "Witham" seems to be extremely old and of unknown origin. Archaeological and documentary evidence shows the importance of the Witham as a navigable river from the Iron Age onwards. From Roman times it was navigable to Lincoln, from where the Fossdyke was constructed to link it to the River Trent. The mouth of the river moved in 1014 following severe flooding, and Boston became important as a port.
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 or 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.
Sir Cornelius Vermuyden was a Dutch engineer who introduced Dutch land reclamation methods to England.
Holbeach is a market town and civil parish in the South Holland District in Lincolnshire, England. The town lies 8 miles (13 km) from Spalding; 17 miles (27 km) from Boston; 20 miles (32 km) from King's Lynn; 23 miles (37 km) from Peterborough; and 43 miles (69 km) by road from Lincoln. It is on the junction of the A151 and A17.
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 Forty Foot or Forty Foot Drain is a name given to several of the principal channels in the drainage schemes of the Fens of Eastern England, the name being qualified when there is a need to distinguish between them. They are Vermuyden's Drain, South Forty Foot and North Forty Foot.
The Middle Level Commissioners are a land drainage authority in eastern England. The body was formed in 1862, undertaking the main water level management function within the Middle Level following the breakup of the former Bedford Level Corporation.
The Witham Navigable Drains are located in Lincolnshire, England, and are part of a much larger drainage system managed by the Witham Fourth District Internal Drainage Board. The Witham Fourth District comprises the East Fen and West Fen, to the north of Boston, which together cover an area of 97 square miles (250 km2). In total there are over 438 miles (705 km) of drainage ditches, of which under 60 miles (97 km) are navigable. Navigation is normally only possible in the summer months, as the drains are maintained at a lower level in winter, and are subject to sudden changes in level as a result of their primary drainage function, which can leave boats stranded. Access to the drains is from the River Witham at Anton's Gowt Lock.
Guthram Gowt is a small settlement in the South Holland district of Lincolnshire, England. It is situated 5 miles (8 km) both east from Bourne and west from Spalding, and at a bend in the River Glen.
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.
John Grundy, Sr. was a teacher of mathematics, a land surveyor, and later a civil engineer. Grundy lived in Congerstone, Leicestershire, England for the first forty years of his life; he later moved to Spalding in Lincolnshire. He was one of the first engineers to apply mathematical principles to the problems of land drainage. His son, John Grundy Jr., was also a civil engineer.
Witham First District IDB is an English internal drainage board which was set up under the terms of the Land Drainage Act 1930. The Board inherited the responsibilities of the Witham General Drainage Commissioners, who were first constituted by an Act of Parliament of 1762. They manage the land drainage of an area to the west of the River Witham, between Lincoln and Dogdyke, which includes the valley of the River Slea to above Sleaford.
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.
Witham Third District IDB is an English internal drainage board set up under the terms of the Land Drainage Act 1930. The Board inherited the responsibilities of the Witham General Drainage Commissioners, who were first constituted by an Act of Parliament of 1762. They manage the land drainage of an area to the north and east of the River Witham, between Lincoln and Dogdyke, which includes the valley of the River Bain to above Hemingby, and the valleys of Barlings Eau and most of its tributaries, to the north east of Lincoln.
The Bedford Level Corporation was founded in England in 1663 to manage the draining of the Fens of East Central England. It formalised the legal status of the Company of Adventurers previously formed by the Duke of Bedford to reclaim 95,000 acres of the Bedford Level.
The Upper Witham IDB is an English Internal Drainage Board responsible for land drainage and the management of flood risk for an area to the west of the Lincolnshire city of Lincoln, broadly following the valleys of the upper River Witham, the River Till and the course of the Fossdyke Navigation.