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 artesian spring is fed by a limestone aquifer, which has been extensively used to supply drinking water to the locality and to Spalding. After a period of low rainfall in the late 1980s, the spring and hence the upper river dried up completely. A remediation project was implemented in 1992/93 to repair wild boreholes, where artesian water was uncontrollably running to waste. 30 boreholes were plugged or repaired, and water returned to the spring and river.
The river divides North Fen from South Fen. Both were enclosed in the 1770s, and surplus water from the North Fen was fed to the South Forty-Foot Drain. Steam pumping was introduced in 1845, and the drainage is the responsibility of the Black Sluice Internal Drainage Board (IDB). To drain the South Fen Gilbert Heathcote's tunnel was constructed to take water under the River Glen to the Counter Drain. Various engines were used to pump water through the tunnel, but after the failure of a gas engine in 1942, a new pumping station was built, to pump water into the River Glen. Drainage in the South Fen is now the responsibility of the Welland and Deepings IDB.
Course
Bourne Eau outside the Abbey Church at Bourne. The iron bridge is dated 1832.
The town of Bourne is surrounded by the River Glen. To the west, the East Glen and West Glen flow from north to south, and become one river to the south of the town. They then flow in a north-easterly direction to the east of the town.[1] Bourne sits over a layer of Middle Jurassic limestone, some 100 feet (30m) thick, which dips to the east, and is covered by Upper Estuarine mudrocks, which confine groundwater within the limestone layer.[2]
Bourne Eau rises in The Wellhead, otherwise known as St Peter's Pool, in Bourne.[3] The Wellhead is a natural artesian spring, rising from the limestone some 165 feet (50m) below the land surface.[4] It once formed the source of the water defences for Bourne Castle as well as the power for the town's three mills.[3] From the Wellhead, a branch flows to the east, along the southern edge of the castle site, while another flows north, then east and south, enclosing the castle site and Wellhead Gardens to rejoin the first branch near Baldock's Mill. A culvert carries the water under South Street, and it flows along the edge of Church Lane,[5] where it is crossed by a small cast-iron bridge with gates, providing rear access to Bourne Eau House.[6] It carries the date 1832. On the other side of Church Lane is the parish church of St Peter and St Paul, a grade I listed structure that was originally the chapel for an Arrouaisian order of Canons founded in 1138.[7]
At the north end of Church Lane, another culvert takes it under the gardens of the vicarage. This culvert and the South Street culvert are quite old, since they appear on the 1888 Ordnance Survey map.[8] When the river resurfaces, if turns to the south, running behind the church building and then to the east along the back of gardens belonging to houses on Coggles Causeway. A lengthy culvert carries it under the Abbey Lawn complex and Victoria Place.[5] This culvert is more recent, as it was built in the 1960s when the recreation ground became the Abbey Lawn sports complex. Before the culvert was built, the railway line to Sleaford crossed the river near to where the culvert starts.[9] It passes under Queen's Bridge, and then runs parallel to Eastgate. Half way along Eastgate, the channel becomes much wider, where it formed the terminal basin for the Bourne Eau when it was navigable. The RomanCar Dyke, now reused as a drainage channel, originally ran though the town, passing along the west side of Queen's Bridge,[8] but a modern channel joins the southern section to the basin,[5] on the north bank of which is the Anchor Inn, a small grade II listed public house dating from the 18th century.[10] The A151 Cherry Holt Road crosses the waterway at May's Sluice, and then it enters South Fen,[5] where it is joined by another channel linking to the Car Dyke on its north bank. Below the junction its flow is supplemented by the treated outfall from Bourne sewage treatment works. The river is embanked on both sides, and there are low level catchwater drains running parallel to the banks. A bridge carried the railway to Spalding over the river.[1]
The present course enters the River Glen at Tongue End, a name which derives from the low tongue of land within the enclosing banks of the rivers.[11]
Apart from the spring, most of the water of the river is collected by the Car Dyke, which, near Bourne, is arranged to act as a catchwater drain, gathering the surface water of the upland and feeding it via the Bourne Eau and River Glen to the sea, without its entering The Fens.
History
The pumping station at Tongue End, which replaced the former sluice between Bourne Eau and the River Glen.
The course of the river through South Fen is clearly manmade, as the river is above the level of the surrounding land, but there is no known documentary evidence as to when this was first carried out. In the 13th century it was called Bourne Ald Ea or Brunne Ea, and the Commission of Sewers issued an order that it should be raised and scoured by the people of Bourne. Work on the north bank was to extend as far as Goderam's Cote, and on the south bank to Merehirne. Another order was made in 1376, that the Brunne Ald Ea was to be repaired, raised and cleansed, but this time the responsibility for the work was shared between the town and the Abbot of Brunne. Later an order required that the banks be made 12 feet (3.7m) thick and raised by an extra 2 feet (0.6m).[12]
Documentary evidence for the use of the Bourne Eau is quite scant, but in the 16th century Bourne was a market town, and it is probable that the river enabled the corn trade to flourish. In 1765, there was serious flooding in the area, following the failure of the banks of both the Bourne Eau and the River Glen.[13] As a result, the north bank of the river became the responsibility of the Black Sluice Commissioners, a body which was created by an Act of Parliament, to construct the Black Sluice where the South Forty-Foot Drain entered The Haven at Boston, and to supervise the drainage of the Fens feeding that system. The north bank was a serious problem, as it was built on a peat subsoil, and defied attempts to raise it, with the result that the Bourne Fens often flooded.[14]
Improvements to the 3.5 miles (5.6km) of river from the River Glen junction to the town of Bourne were authorised by an act of Parliament obtained on 29 March 1781, which suggested that the river had previously been navigable, but had become choked with mud. The act created a body of 12 trustees, who were empowered to maintain a channel which was 30 feet (9.1m) wide by 5 feet (1.5m) deep.[15] They could charge tolls on all boats using the navigation, on which the main merchandise was coal and wool, which were shipped to Boston for onward transmission to the north east. Return trips brought coal and groceries to the town, and a coal wharf was erected on Eastgate during the early years of the 19th century.[16] There was also some trade with Spalding, including a regular service to take people and goods to Spalding market every Tuesday, but Thomas Hawkes noted in 1792 that the service was a little intermittent, as there was often too little or too much water in the river. Investigation showed that the river levels rose by 9 or 10 inches (230 or 250mm) for every quarter of an inch (6mm) of rainfall in the River Glen catchment.[17] The navigation included two locks, one near the junction with the Glen, and the other near Bourne.[3]
In order to ease the problems caused by the north bank, the Black Sluice Commissioners negotiated with the Trustees to allow them to build a set of self-acting flood gates at Tongue End, where the river joined the Glen, and an overfall weir, which allowed surplus water to flow over the bank and into the Weir Dyke in Bourne Fen.[14] The self-acting doors prevented high water levels in the Glen from flooding back up the Bourne Eau, and it improved navigation for a time, but competition from the railway saw traffic decline. A railway from Boston to Spalding opened in 1848, with a branch from Spalding to Bourne completed in 1866. A link from Bourne to Sleaford followed in 1872. By 1857, boats using the navigation only do so occasionally,[17] and the self-acting doors were replaced by a sluice in the 1860s, which effectively brought navigation to an end.[3] The Bourne Eau Act was repealed in 1962, removing the right of navigation,[17] and the sluice was replaced by a pumping station in 1966, which removed the need for the overfall weir.[14]
Milling
The river has been used to power mills since at least 1086, when the Domesday Book recorded three mills in the village. There were three mills in the late 1800s, all of which were marked as corn mills on the 1888 map. Cliffe's or West Street Mill was on the stream that ran around the northern edge of the castle site, was at times used for grinding bark for use in the tanning industry. It was demolished in 1910. Baldock's Mill was located where the streams left the castle site, on the western side of South Street, while Notley's Mill was a flour mill, and was located on the west side of Victoria Place, close to Eastgate. It survived until 1973.[5][3][18]
Baldocks Mill still exists, and has been repurposed as a heritage centre. The present building was constructed in 1800, and the mill was operated for two three-hour periods each day. This was subsequently increased, by digging a new channel, and was later supplemented by a gas engine. The mill had two water wheels, one make of timber which was 15 feet (4.6m) in diameter by 3 feet (0.91m) wide, and a second metal wheel which was 5 feet (1.5m) by 12 inches (30cm). The mill produced animal feed from corn and maize, and was used commercially in 1920, when the miller was Mr Baldock. The building was grade II listed in 1973, and initial restoration work was carried out by pupils from Bourne Secondary School, the Robert Manning Technology College (now known as Bourne Academy). It is owned by Bourne United Charities, but has been leased to the Civic Society since 1983, who have gradually turned it into a heritage centre, celebrating the town and the lives of some of its residents. In 2002, the Civic Society decided to restore the wheels. The large wheel could not be rebuilt to its full size, due to modifications made to the building to make it suitable for public use, but the small wheel is operational, and drives a generator, which powers the heating system for the centre.[19]
Water abstraction
A major component of the flow in the Bourne Eau is from the spring at St Peters Pool. Historically this produced some 4.5million imperial gallons (20Ml) per day, and was of sufficient purity that it was bottled and sold as mineral water in the late Victorian period. The flow has since reduced, resulting in the river being smaller than it was.[20] Anglian Water have two boreholes near the junction of Abbey Road and Manning Road, which are authorised to abstract up to 25Mld (megalitres per day), although they normally abstract around 16Mld. The water is oxygenated, chlorinated to disinfect it, and checked for clarity. It is then pumped into the public supply network, most of it passing along an 18-inch (46cm) pipeline to Spalding Tower.[21] Water for Spalding has been obtained from the aquifer below Bourne since 1894, when the first borehole was drilled to a depth of 134 feet (41m). Boreholes proliferated, and there were about 130 around the town by 1969. Most of these have since been sealed up, and only Anglian Water operates boreholes within the town.[22]
In the late 1960s, engineers began to appreciate that water was being removed from the aquifer at rates which were not sustainable, and several important studies took place to assess the situation. These coincided with a period of low rainfall, which reduced the speed at which the aquifer would recharge.[23] Housing development at Peterborough was expected to require an extra 100 Mld to maintain the public water supply, and it was thought that this could be obtained from the aquifer. However, since the passing of the Water Resources Act 1963, all abstraction had to be licensed, and investigation showed that the aquifer was already being over-abstracted. It was thought that it could supply around 68 Mld, but licences at the time allowed 139 Mld to be abstracted, although only 77 Mld actually were. This imbalance meant that an alternative water supply for Peterborough had to be found, and resulted in the construction of Rutland Water.[24]
These conditions led to a steady lowering of water levels within the aquifer, which were particularly bad in the mid-1970s, when river flows were significantly reduced. Abstraction from the aquifer was reduced, and river flows increased, but the lack of water in the River Glen led to most of the fish dying, and fish populations had still not recovered ten years later.[24] Bourne Eau dried up in 1972, and the curate of the Abbey Church inspired a group of 30 young people to remove all of the rubbish from the muddy river bed.[22] At that time, the existence of a number of wild artesian boreholes was recorded, but attempts to repair one of them proved difficult, and no further action was taken. A wild borehole is one where the discharge of water is no longer under control, and it continually runs to waste. There had been four years of below average rainfall in the late 1980s, resulting in the Bourne Eau drying up again,[25] and the National Rivers Authority undertook a project to seal or repair 30 wild boreholes located to the east of Bourne, between August 1991 and October 1992.[26] Most had been drilled in the later 19th century to supply the isolated farms that were established when the fens were drained. Initially they had been drilled by hand, but later, steam engines were used, with most of them being constructed by J E Noble of Thurlby.[27] The repairs were estimated to retain 7.5 Mld within the aquifer during dry periods, and as much as 18 Mld when conditions were more normal.[28] One obvious benefit of the work was that water again began to flow into St Peters Pool, and Bourne Eau flowed for the first time in several years, although this may have been aided by a very wet winter in 1992.[29]
An Act for allotting, dividing, enclosing, and draining, several Open and Common Fields, Meadows, Waste and Fen Grounds, within the Manor and Parish of Bourn, in the County of Lincoln.
Once Bourne Eau leaves the town of Bourne, it passes through fenland. Until 1772, land on both sides of the river was treated as one unit, but an act of Parliament[which?] obtained in 1772 split the North Fen, to the north of the river, and the South Fen, to the south of the river, into two separate drainage districts. Prior to that, rents had been payable to the Black Sluice Commissioners to fund the work they did on the drainage network. An enclosure act, the Bourn (Lincolnshire) Inclosure Act 1766 (6 Geo. 3. c. 52) was obtained in 1776, covering the North Fen and fenland in the hamlets of Dyke and Cawthorpe. After dealing will the allocation of land for use as cow parture, it included a clause that ensured that the Well Head would be protected, and its water would continue to feed into Bourne Eau. Maintenance of the south bank of the river was proving difficult, because there was a lack of soil within 120 feet (37m) of the bank, and this distance had previously been specified as the limits for obtaining material for repairs. The enclosure act extended this to 180 feet (55m).[30]
An Act for altering, amending and enlarging the Powers and Provisions of an Act passed in Her present Majesty's reign, for the better Drainage of Lands in Bourn North Eau and Dyke Fen, in the Manor and Parish of Bourn, in the County of Lincoln, and for other Purposes concerning the Drainage of the same Lands.
The North Fen drained by gravity into the South Forty-Foot Drain, but the owners wanted to improve the drainage. They intended to use steam engines to pump the water out of the fen and into the South Forty-Foot Drain, but the Black Sluice Commissioners objected to the proposal, on the basis that it would prevent other fens from draining properly. The disagreement took a long time to resolve, but the Proprietors eventually obtained the Bourne Drainage Act 1841 (4 & 5 Vict. c. cxiii), which transferred the responsibility for the North Fen from the Black Sluice Commissioners to trustees representing the owners of land within the North Fen. Significantly, the act allowed the trustees to build steam pumping engines. The introduction to the act stated that a number of wind-powered engines had been built following the 1776 enclosure act, but all had been removed after their condition deteriorated.[31] In order to prevent the South Forty-Foot Drain from being overwhelmed by the volume of water pumped into it, a gauge was erected, and pumping had to stop when water levels exceeded an agreed height.[32] A second act, the Lincolnshire Fens Drainage Act 1843 (6 & 7 Vict. c. xxxvii), transferred the maintenance of the drainage infrastructure within the North Fen from the Black Sluice Commissioners to the Bourne Fen Trust.[33]
The pumping station for the South Fen. The buildings carry the dates 1946 (left) and 1976 (right).
The pumping engine was built at Guthram Gowt. In 1872, some 2,000 acres (810ha) of the North Fen were flooded, when the level in the River Glen rose to 2 feet (0.6m) above any previously known level, and the north bank of Bourne Eau between the lower lock and Tongue End was breached. The Bourne Fen Trust attempted to sue the Black Sluice Commissioners, but the jury found that they had maintained the bank adequately, and therefore dismissed the claim. It was flooded again in 1877 when someone cut through the bank of the River Glen, but despite a reward of £100 being offered, the offender was not discovered.[34] The Guthram Gowt engine was obtained from the Butterley Company and erected in 1845. It was a 30hp (22kW) beam engine, driving a scoop wheel which was 15 feet (4.6m) in diameter. The scoop wheel was replaced by a 20-inch (51cm) pump manufactured by Easton and Anderson in 1895, and the engine was replaced by a Tangye gas engine in 1918. It drove the Easton and Anderson pump by a belt drive. A Ruston diesel engine driving a 36-inch (91cm)Gwynnes pump was installed to assist the gas engine in 1933, and both engines were replaced by a 24-inch (61cm) electric pump in 1968.[35]
Drainage of the South Fen was complicated by the fact that it was hemmed in by Bourne Eau and the River Glen, both of which were embanked. The solution adopted by Thomas Lovell, working on behalf of the Adventurers of Deeping Fen in the early 17th century, was to construct a culvert beneath the River Glen. It was to be maintained by John Heathcote, who owned the land.[36] The culvert, subsequently known as Gilbert Heathcote's tunnel, allowed water to drain into the Slacker Dyke, now called the Counter Drain, from where it flowed to Pode Hole. The South Fen was enclosed in 1772,[37] and ceased to pay taxes to the Adventurers by an act of Parliament[which?] obtained in 1738. A subsequent act[which?] ensured that if the Deeping Fen Trust ever lowered the bed of the Glen, they would first have to lower the culvert.[36] A number of scoop wheels, powered by horses, were used to assist in the drainage of the fen. Under the powers of the Land Drainage Act 1861 (24 & 25 Vict. c. 133),[38] the South Fen Drainage District was created in 1871. They hired a portable engine to drive a scoop wheel, and bought their own engine in 1872. The scoop wheel was supplemented by a centrifugal pump in 1887.[37]
In 1893, the engine was replaced by a new 10hp (7.5kW) portable engine, and a new scoop wheel was manufactured in 1904. The drainage district became the Bourne South and Thurlby Fen Drainage Board in 1910, increasing its area by 856 acres (346ha). In order to manage this larger area, a gas suction engine driving a scoop wheel was built nearer to the tunnel, to replace the previous engine. This worked until 1942, when it broke down. The fen became part of the Deeping Fen Drainage District in 1943, and until a new pumping station was built in 1949, portable pumps were used to maintain the water levels. The new station had two vertical spindle pumps driven by electric motors, and the station was altered in 1973, to lower the pumps.[39] In 1973, the Baston, Langtoft and the Deepings Internal Drainage Board (IDB) as it was by then known, was abolished, together with three other nearby IDBs, and replaced by the Welland and Deepings IDB.[40]
Etymology
Wheeler (1896) gives the name Bourne Old Ea to what is now the Bourne Eau and Bourne Ea or Brunne Ea to that part of the Glen downstream of Kate's Bridge. He then quotes Dugdale, and an act of Queen Elizabeth I:
Brunne, River of, Brunne Hee,Burne Alde Ee. In Dugdale the Brunne Ee is describhed in the margin as 'now the Glene'...'Which had its course through the midst of the town of Pincbec.' The 'Ware' Dyke is described as extending along 'the river of Burne Ee to Godramscote' in a commission of Sewers held at Hempringingham in Queen Elisabeth's time. [41]
The French-seeming spelling Eau is not unique in English river names. It appears to have arisen in the eighteenth century.[42] The older spelling was Ea, from Old Englishǣ (ultimately from the Proto-Indo-European*hakʷā- "(moving) water"), see also Aach (toponymy) for more detail. Bourne "stream" is from Old English burne, burna ("spring, fountain").
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 that 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 washlands 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.
The River Glen is a river in Lincolnshire, England with a short stretch passing through Rutland near Essendine.
The River Idle is a river in Nottinghamshire, England whose source is the confluence of the River Maun and River Meden near Markham Moor. The Idle flows north from its source through Retford and Bawtry before entering the River Trent at West Stockwith. Its main tributaries are the River Poulter and the River Ryton. The river is navigable to Bawtry, and there is a statutory right of navigation to Retford. Most of the land surrounding the river is a broad flood plain and the river is important for conservation, with Sites of Special Scientific Interest being designated along its course.
The River Lymn is a river in Lincolnshire, England. It rises in the Wolds on the eastern slope of Castcliffe Hill in Fulletby parish. It flows south-eastwards to the Lincolnshire Marsh, where it becomes known as the Steeping River on the boundary of Great Steeping parish. The main channel is supplemented by the Wainfleet Relief Channel as it passes Wainfleet All Saints, and the relief channel is joined by the old course of the Lymn. Once the two channels rejoin, there are three flood defence structures to protect the region from flooding by the North Sea.
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.
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 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 Navigations are a network of waterways in England, primarily used for land drainage, which lie in The Fens between the Rivers Nene and Great Ouse, and between the cities of Peterborough and Cambridge. Most of the area through which they run is at or below sea level, and attempts to protect it from inundation have been carried out since 1480. The Middle Level was given its name by the Dutch Engineer Cornelius Vermuyden in 1642, who subsequently constructed several drainage channels to make the area suitable for agriculture. Water levels were always managed to allow navigation, and Commissioners were established in 1754 to maintain the waterways and collect tolls from commercial traffic.
Barlings Eau is a small river near Barlings, Lincolnshire, England. It is a tributary of the River Witham, joining it near Short Ferry. It acts as the central spine for a number of other small rivers, which drain the low-lying land to either side. Most of its course is within the area managed by the Witham Third District IDB, an Internal Drainage Board responsible for land drainage. One of their pumping stations is on the banks of the river.
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.
Pode Hole is a village in South Holland, Lincolnshire, England. It is 2 miles (3.2 km) from Spalding and 10 miles 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.
Gilbert Heathcote's tunnel was an engineering project dating from the 1630s as one of the earliest modern attempts to drain The Fens in Lincolnshire. Rendered obsolete by the mechanical drainage improvements after World War II, it was finally removed in 1991.
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.
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