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River Witham
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River Witham
The Grand Sluice at Boston, where the River Witham empties into The Haven, which is tidal below this point
Path of the River Witham [1]
Location
CountryUnited Kingdom
Country within the UKEngland
Counties Lincolnshire
Nottinghamshire
Leicestershire
CitiesLincoln
TownsGrantham, Boston
Physical characteristics
Source 
 • locationSouth Witham, Lincolnshire
 • coordinates52°45′20″N 0°41′27″W / 52.755622°N 0.690858°W / 52.755622; -0.690858
 • elevation130 m (430 ft)
Mouth 
 • location
The Haven, Boston, Lincolnshire
 • coordinates
52°57′52″N 0°00′36″W / 52.964541°N 0.010042°W / 52.964541; -0.010042
 • elevation
0 m (0 ft)
Length132 km (82 mi)
Basin size3,817 km2 (1,474 sq mi)[1]
Discharge 
 • locationClaypole Mill
 • average1.86 m3/s (66 cu ft/s)[2]
 • maximum21.79 m3/s (770 cu ft/s)[3]
Discharge 
 • locationColsterworth
 • average0.23 m3/s (8.1 cu ft/s)
Basin features
Tributaries 
 • leftFoston Beck, Ease Drain, Shire Dyke, Fossdyke Navigation, Barlings Eau, Tupholme Beck, Bucknall Beck, Catchwater Drain, The Sewer, Engine Drain, Cut Dike, Newham Drain, Cowbridge Drain, Maud Foster, Hobhole Drain
 • rightHonington Beck, River Brant, Branston Delph, Middle Drain, Cathole Drain, Nocton Drain, Nocton Bankside Drain, Dunston Bankside Drain, Water Dike, Duns Dike, Metheringham Delph, Dales Drain, Blankney Town Drain, Black Horse Drain, Timberland Delph, Town Dike
Progression : River Witham – The HavenNorth Sea
River Witham is located in Lincolnshire
Source
Source
Lincoln
Lincoln
Boston
Boston
Grantham
Grantham
Claypole
Claypole
Dogdyke
Dogdyke
Kirkstead
Kirkstead
Bardney
Bardney
Map showing the course of the Witham and locations along its length

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 (where it may be closely followed using the Riverside Walk through Wyndham Park and Queen Elizabeth Park), 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.[4] 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.

From 1142 onwards, sluices were constructed to prevent flooding by the sea, and this culminated in the Great Sluice, which was constructed in 1766. It maintained river levels above Boston, and helped to scour the channel below it. The land through which the lower river runs has been the subject of much land drainage, and many drains are connected to the Witham by flood doors, which block them off if river levels rise rapidly. The river is navigable from Brayford Pool in Lincoln to Boston. Its locks are at Lincoln, Bardney and the Grand/Great Sluice. Passage through the latter is restricted typically to 4-hour intervals during daylight when the tidal levels are suitable. The river provides access for boaters to the Witham Navigable Drains, to the north of Boston, and to the South Forty-Foot Drain to the south, which was reopened as part of the Fens Waterways Link, a project to link the river to the Nene flowing through the city of Peterborough. From Brayford Pool the Fossdyke Navigation links to the Trent.

Route

[edit]
River Witham at Saltersford Bridge 1 mile south of Grantham. This part of the Witham is home to one of the last viable white clawed crayfish populations in the UK.[5]
(Credit: Mark A. O'Neill)
River Witham at New Somerby, Grantham

The Witham's course, which flows to the north and then to the south-east may be the result of glaciation (and possibly isostatic rebound) redirecting older rivers.[citation needed] The source of the river is on high ground near South Witham, Lincolnshire,[6] at around 340 feet (100 m) above ordnance datum (AOD). After briefly flowing to the east to reach South Witham, it flows generally north, passing through Colsterworth where it is crossed by the A1 road, which largely follows the line of the river to Newark on Trent. At Great Ponton, it is joined by the Cringle Brook on its left bank, and continues through Grantham, where it has already descended to 170 feet (52 m) AOD. After Barkston it turns to the west to pass through Marston. Foston Beck joins on the left bank, and at Long Bennington it resumes its northerly course. Beyond Claypole and near Barnby in the Willows it forms the border between Lincolnshire and Nottinghamshire for about 3 miles (4.8 km), before passing through an Army training area near Beckingham. The River Brant joins on the right bank, before it passes through North Hykeham to reach Lincoln, where it is only 16 feet (4.9 m) AOD.[7][6]

The upper waters are important for agricultural water extraction, and for coarse fish such as roach, common bream and pike; small mammals like water voles, and native crayfish.[5] A gap in the limestone scarp (see Lincolnshire Wolds) near Ancaster may represent an earlier course of the River Trent towards Boston, but is now occupied by the River Slea.[8]

In Lincoln, the river flows into Brayford Pool and exits along a narrow channel that passes under the medieval High Bridge.[9] The bridge not only restricts navigation due to its small size, but the volume of water that can pass through the gap is limited in times of flood. This is alleviated by the Sincil Dyke, which leaves the main channel at Bargate Weir and runs for 1.5 miles (2.4 km) through the industrial areas to the south of the main city centre. It used to rejoin the main channel at Stamp End, but was re-routed into the South Delph, a drainage ditch constructed by John Rennie in the early 19th century that joins the main channel below Bardney lock. The origins of the Sincil Dyke are unknown, but it is known to have been used as a drainage channel in the mid-13th century and is thought to be pre-medieval or even Roman. Parts of it were culverted in 1847 to allow the construction of Lincoln Central railway station.[10]

From Lincoln, the river again turns first east, then south, making a cut through a belt of upland known as the Lincoln Gap. This section has also been suggested as a lower course of the Trent during and before periods of glaciation.[8]

From Dogdyke near Coningsby to Boston, the north bank of the river was used by a section of the Great Northern Railway from Lincoln to Boston. A long-distance footpath, the Water Rail Way, follows the course of the river from Lincoln to Boston. The path uses sections of the river towpath and abandoned railway tracks, and has been opened in stages, with the final 2 miles (3.2 km) being completed in September 2008. The path is now part of Route 1 of the National Cycle Network and features a number of sculptures along its length, each commissioned from local artists.[11] They include Lincoln longwool sheep at Stixwould, Lincoln Red cows at Washingborough, and Lincoln curly pigs, which became extinct in 1972, at Southrey.[12]

History

[edit]
The Witham Shield, normally kept at the British Museum photographed during its visit to The Collection in 2013

The name "Witham" seems to be extremely old, apparently predating Anglo-Saxon, Roman, and even Celtic influence.[4] The meaning is uncertain,[13] although one possibility is Wye-om, meaning river plain, and the river has been known as the Witham since Saxon times. However, it was known as the Grant Avon in Ancient British times, meaning divine stream, and the fact that the main town on the upper river was Grant-ham may support this. John Leland writing in the 16th century noted that it was also called the Lindis, and others referred to it by that name.[14] The present course may be a combination of two rivers, with the upper river originally emptying into Brayford Mere, to the west of Lincoln, and draining along the course of the Fossdyke, while the Langworth River emptied into another mere to the east of Lincoln, located between Washingborough and Chapel Hill. From there, the water flowed along a tidal creek to reach the sea. There was a ridge of high ground between the two meres, and the Romans cut a channel through it as part of some drainage works.[15]

Archaeological evidence points to river navigation as far back as the Iron Age. Artefacts such as the Iron Age Witham Shield, found in the river near Washingborough in 1826,[16] and the Fiskerton Boat, a log boat found near Fiskerton during flood defence work in 2001[17] have been recovered[18] and are on display at the British Museum in London or The Collection in Lincoln.[19]

The Witham was an important navigation in Roman times. Lincoln (Lindum)—the meeting point of Ermine Street, joining London to York, and Fosse Way, leading to Leicester and Bath—was an important Roman fort that became one of only four colonia in Britain. Most important Roman cities were situated near navigable water, which enabled goods to be transported in bulk, but Lincoln did not possess this advantage, and so the Romans constructed the Fossdyke from Lincoln to Torksey on the River Trent, improved the River Witham from Lincoln to The Wash, and built the Car Dyke from Lincoln to the River Cam near Cambridge.[20] The Witham thus gave Lincoln access to the east coast, while the Fossdyke gave access to the Trent and further on to the Humber.

There have been claims that the Witham was originally tidal up to Lincoln, but that seems unlikely. Prior to the construction of the Grand Sluice, the lower river was affected by tides, but the highest they normally reached was Dogdyke or Chapel Hill, and Lincoln is considerably higher than these locations, by some 5 to 7 feet (1.5 to 2.1 m). Wheeler argues that it "would not have been possible for the tide to flow up to Lincoln," given the present geological conditions.[21]

Trading continued throughout the medieval period evidenced by the importance of Torksey, which was then a flourishing town, now only a small village. However, the Fossdyke needed much maintenance to keep it clear of silt. Henry I had overseen the scouring of its channel, and there were inquiries in 1335, 1365 and 1518 to consider the state of the Fossdyke and to compel the inhabitants of the region to maintain it. Lincoln was a centre for the collection of business taxes, but this came at the cost of maintaining the waterways, and having finally decided it was too large a cost, James I presented the Fossdyke to the City of Lincoln.[22]

The Witham originally flowed into The Wash at Bicker Haven, where the port of Drayton was established in the Welland estuary, and it was only as a result of massive flooding in 1014 that it diverted itself to flow into The Haven at Boston.[23] This gave rise to the growth of Boston as a port in the 12th and 13th centuries, exporting wool and salt to the Hanseatic League, though Boston only received its charter in 1545.[24]

Kirkstead Bridge (B1191 road)

The river was affected by silting which restricted trade despite the construction of various sluices and barriers from 1142 onwards, when the first sluice was built below Boston.[25] Other sluices were erected at Boston in 1500 and at Langrick in 1543, but navigation was again difficult on both the river and the Fossdyke by 1660.[26] In 1671 an Act of Parliament was obtained for the improvement of the Navigation.[27] In 1743, John Grundy, Sr. and his son John Grundy, Jr. were commissioned to produce a detailed survey of the river. They produced an engraved map in 1743 and a printed report, running to 48 pages, in the following year. The main recommendation was a 7-mile (11 km) new cut to eliminate the "prodigious meandering course" of the channel above Boston. Although the estimated cost of £16,200 dissuaded the landowners from taking action at the time, the report formed the basis for improvements in the 1760s.[28]

Canalisation

[edit]

Following meetings of Landowners held in 1752 and 1753, they asked John Grundy Jr, as his father had died in 1748, to re-evaluate his plans from 1744 and consider a plan for a "Grand Sluice" that had been produced by Daniel Coppin in 1745. Grundy suggested that the 1744 cut should be extended by a further 2 miles (3.2 km) into Boston, and that the sluice could then be built on the extension. The landowners moved the location of the sluice nearer to Boston, but otherwise approved his report, although no action was taken. John Grundy was again consulted in 1757, and Langley Edwards of King's Lynn was asked to review the positioning of the sluice in 1760. The landowners then asked John Smeaton to liaise with Grundy and Edwards, and the three engineers produced a joint report in 1761, with estimates of £38,000 for drainage works and £7,400 for improvements to navigation. The report was approved, although a meeting held in January 1762 decided that the new cut should revert to the alignment suggested by Grundy in 1753. The location of the Grand Sluice would be as suggested by Edwards in 1760. Grundy produced another engraved map, and parliamentary approval for the works was obtained in June 1762.[29]

Once the Act of Parliament was obtained, Edwards became the engineer for the project, and drew up the detailed plans, which Grundy and Smeaton checked and altered slightly, after which they had no further involvement with the scheme. Construction was started in April 1763, and the drainage element of the project, which included the sluice, was finished in 1768, having cost £42,000. Work on three locks and other work connected with navigation cost £6,000 and continued until 1771.[29] The locks were located at Stamp End, Kirkstead and Barlings.[30] The Grand Sluice was a major construction which maintained the height of water above Boston to near normal high tide level and had massive flood gates to cope with any tides above this. It was completed in 1766[31] and was effective in scouring the Haven below it and increasing silting of the river above it.

The 1762 act created the Witham Navigation Commissioners and the Witham Drainage General Commissioners,[32] who continued to promote drainage schemes actively,[33] creating a drainage network known as the Witham Navigable Drains that transformed much of northern Lincolnshire from fen to farming land. Today many of these channels are managed by the Witham First, Third and Fourth District Internal Drainage Boards and Upper Witham Internal Drainage Board. These four internal drainage boards reduce the flood risk to the surrounding properties, land and environment.

In 1791, as part of the campaign to promote the construction of the Horncastle Canal, the Commissioners of the River Witham asked the engineer William Jessop to assess the state of the Fossdyke Navigation and the Witham, with particular reference to the problems of navigating through Lincoln, where the channel was restricted by a medieval bridge. He proposed two solutions; the first avoided the route through the city entirely, by utilising the course of the Sincil Dyke to the south, while the second involved lowering the bottom of the channel through the Glory Hole bridge, which was only 18 inches (46 cm) deep at normal water levels. The Commissioners had imposed a toll on all traffic passing under the bridge, but decided that a channel bypassing the city would have grave financial consequences. They opted for improving the existing channel[34] and the work to remove the wooden floor, to lower the river bed under the bridge and to underpin its foundations was completed in 1795.[35] The Commissioners dropped the collection of tolls at the bridge, but the amount they received from traffic passing through the locks increased as the volume of traffic grew in response to the easier passage through the bridge.[34]

The Grand Sluice

[edit]

When completed in 1766, Edwards' Grand Sluice consisted of three channels each 17 feet (5.2 m) wide, fitted with pointed gates on both sides, and a lock adjacent to the north bank, which could be used as an additional flood relief channel if required.[31] The lock was originally very small, but was lengthened to its current 41 by 12 feet (12.5 by 3.7 m)[36] in 1881. The pointed doors on the non-tidal side of the sluice were replaced by steel guillotine gates between 1979 and 1982.[31]

Improvements

[edit]
Navigable River Witham
Fossdyke Navigation
Brayford Pool
River Witham
 B199  Wigford Way bridge
Lincoln High Bridge or Glory Hole
Sincil Dyke
 A1434  Lindum Road bridge
Stamp End Lock and sluice
Railway bridge (Stamp End Bridge)
South Delph
 A15  Lincoln Eastern Bypass Viaduct
Barlings Eau
Short Ferry Bridge
Old River Witham
Branston Delph
Bardney Lock
Old River Witham
Bardney Bridge
Nocton Delph and flood doors
Catchwater Drain and flood doors
Kirkstead Bridge
Timberland Delph and flood doors
Gibsons Cut, Horncastle Canal
Billinghay Skirth and flood doors
 A153  Tattershall Bridge
Horncastle Canal (abandoned)
and Dogdyke Marina
Kyme Eau and flood doors
Langrick Bridge
Anton's Gowt lock
Witham Navigable Drains
Railway bridge
Grand Sluice and sea lock
 A1137  bridge
(tidal below here)
 A16  bridge
Railway swing bridge
Black Sluice pumping station
South Forty-Foot Drain lock
Boston Barrage
Boston Docks
Maud Foster Drain
The Haven

The state of the Witham had deteriorated by 1802, and the Commissioners asked John Rennie for advice. He stated that the Kirkstead lock was badly placed, and the associated staunch was in danger of collapse. He recommended that it be demolished and rebuilt elsewhere, and also suggested that access to Boston should be through the Witham Navigable Drains, rather than the Grand Sluice, or that a new cut should be built to the south of the sluice, to rejoin the river at Boston Harbour.[37] In 1803, he suggested that High Bridge at Lincoln should be demolished and rebuilt. Four years later, he suggested that the locks at Kirkstead and Barlings should be removed, and replaced by one near Washingborough church. The Commissioners petitioned parliament in 1808, and a new Act of Parliament authorised the work, to be carried out by a company of proprietors. They could borrow £30,000 for the drainage element of the scheme and £70,000 for the navigation element. Two new locks were built, one at Stamp End and the other at Bardney, which replaced the original locks. A new channel was cut near Fiskerton, upstream of Bardney, and the plan for a lock at Washingborough was dropped.[38] While Stamp End lock was being rebuilt, an alternative route was provided, utilising the Sincil Dyke and the South Delph.[39] Rennie recorded that Branston Delph, Carlton Dike, Nocton Delph and Timberland Dike were navigable at the time. The proprietors obtained three more Acts of Parliament, in 1812, 1826 and 1829, all with the main aim of allowing more capital to be raised.[40]

Poster for the Favorite Paddle Steamer between Lincoln and Boston, July 1829

Tolls on the Witham had gradually risen as improvements had been made. £263 was raised in 1763–4, and had reached £898 by 1790.[30] In 1819, income exceeded £4,100 for the six months from March to September, and a five per cent dividend was paid in the following year. By 1826, over £180,000 had been spent on improvements, and another £40,000 was needed. However, the proprietors were still optimistic, and commissioned Sir John Rennie to investigate an extension to link the Witham to the River Ancholme, but although he made two proposals, neither was implemented.[41] Most traffic was carried by sailing vessels or in barges hauled by horses, but in March 1816, the first steam packet boat arrived on the river. It was named Witham and had been built by Shuttleworth and Robinson, whose yard was on Sincil Dyke. Despite a boiler explosion in March 1817, fortunately without causing injury to any of the crew or the 30 passengers, a second steam packet was operating by July 1817, and they soon displaced the sailing packet boats. During a flood in 1828, one of them lost power when a floating hedge became jammed in the paddle wheels. In the following year, a Lincoln man, William Pool invented a new type of paddlewheel, which resulted in the boats travelling faster, and in 1836, wooden vessels were superseded by iron packet boats.[42]

Railways reached Lincoln in August 1848, 15 years after the first proposal. The Wakefield, Lincoln and Boston Railway hoped to build railways in the area, and negotiated with the proprietors and those of the Fosdyke. Under the arrangement, they would take over both navigations, and guarantee a fixed income for the proprietors. They would then merge with the London and York Railway. Both proposals had been absorbed into the Great Northern Railway (GNR) by the time an Act of Parliament was obtained, but the original agreement was retained, and the GNR leased the Witham for 999 years for a payment of £10,545 per year to the proprietors. This figure represented the average profits for the previous three years, plus five per cent. The railway company also agreed to pay the interest on mortgages amounting to £24,692 which the proprietors held, but had redeemed them by 1857. The railway from Lincoln to Boston ran along the eastern bank of the river, and opened on 17 October 1848.[43]

Most of the stations were located near to the landing stages which the steam packets used, and the railway did all it could to draw passengers away from the river. This included the provision of fourth-class carriages, with fares set at a halfpenny per mile, in 1850, and by 1863, the steam packet boats had ceased operation. Freight traffic also declined, with coal passing through the Grand Sluice dropping from 19,535 tons in 1847 to 3,780 tons in 1857. Nevertheless, the railway company had to maintain the river, and in 1871, spent £5,000 on making Bardney lock deeper by 5 feet (1.5 m) at the request of the drainage commissioners. The GNR leased the navigation to the Great Northern and Great Eastern Joint Committee in 1882, and in 1897, by which time the Manchester, Sheffield and Lincolnshire Railway had become the Great Central Railway, they built a large warehouse beside Brayford Pool, with a transhipment dock next to it. Total traffic on the river had fallen to 18,548 tons in 1905, and averaged 5,870 tons during the years of the First World War, mainly general merchandise and agricultural produce. With the nationalisation of the waterways following the Second World War, the navigation eventually became the responsibility of British Waterways[44] as a result of the Transport Act 1962, and since 2 July 2012 has been managed by the Canal & River Trust.

Current navigation

[edit]

Today, commercial traffic, apart from tour boats, has ceased above the port of Boston (The Haven) and only pleasure craft carry on through the lock at the Grand Sluice into the Witham. Although the lock is only 41 feet (12 m) long, it is possible for longer boats to pass through it at certain states of the tide. Unlike many such sea locks, the reverse-facing gates close on every tide, as the normal high tide water level is higher than the level of the river, while at low tides there is insufficient water in the Haven to allow exit from the lock. Passage is therefore restricted to a brief period approximately two hours before or after high water.[36] It is still possible to navigate many of the drains in small vessels, and a new lock, completed in December 2008, provides entry to the South Forty-Foot Drain from below the Grand Sluice so that vessels will be able to reach the Fens without venturing out to the Wash, as part of the Fens Waterways Link.[45]

The Witham is navigable from Brayford Wharf in Lincoln to Boston. There are two locks between Boston and Lincoln – one at Bardney and the other in Lincoln itself, the Stamp End Lock which is unusually a guillotine lock.[9] The main obstruction to navigation is the High Bridge or Glory Hole in Lincoln, a medieval structure which is only about 15 feet (4.6 m) wide and 8.5 feet (2.6 m) high at normal river levels. In times of flood it is unnavigable. The bridge spans the river for 87 feet (27 m), and consists of an arch built in c1160, with extensions added in 1235, 1540 to 1550 and 1762/3. It is the only British bridge which still has secular medieval buildings standing on it, and is believed to be the second oldest masonry arch bridge in the country. It is currently a Scheduled Ancient Monument and a Grade I Listed Building.[35]

There are traffic lights on the short section between Brayford Pool and Stamp End Lock, which are used to indicate the state of the river in times of flood. Green indicates that flows are low or normal, and boats can proceed along this stretch. Red indicates that flows are high and that great care is required. Flashing red indicates that flows are very high and boats must not use the section.[46]

Connecting waterways

[edit]

There are a number of drains that connect to the River Witham and that are protected by flood doors. These consist of a single pair of mitre gates that are designed to close if the level in the river rises above the level in the drain. Several of these are navigable to the more adventurous boater.[47] The river is also joined by the Kyme Eau, which connects to the Sleaford Navigation on which navigation will eventually be restored to Sleaford. At Antons Gowt, a lock drops down into the Witham Navigable Drains, a system of drainage ditches which are used to prevent flooding of the fens to the north of Boston. Since November 2008 there has been an active campaign by the Billinghay Skirth Regeneration Society to restore navigation on the River Skirth, and the project has won the support of Billinghay and other parish councils, the Inland Waterways Association, the Environment Agency, Lincolnshire County Council and the Lincolnshire Waterways Partnership.[48]

Water quality

[edit]

The Environment Agency measure 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 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.[49]

The water quality of the River Witham system was as follows in 2019.

Section Ecological Status Chemical Status Length Catchment Channel
Witham – headwaters to conf Cringle Bk[50] Poor Fail 13.3 miles (21.4 km) 24.38 square miles (63.1 km2)
Witham – conf Cringle Bk to conf Brant[51] Moderate Fail 35.4 miles (57.0 km) 60.50 square miles (156.7 km2) heavily modified
Witham – conf Brant to conf Catchwater Drain[52] Moderate Fail 4.1 miles (6.6 km) 6.90 square miles (17.9 km2) heavily modified
Conf Catchwater Drain to conf Bain[53] Moderate Fail 33.3 miles (53.6 km) 76.83 square miles (199.0 km2) heavily modified
Lower Witham[54] Moderate Fail 10.8 miles (17.4 km) 0.66 square miles (1.7 km2) heavily modified
Witham[55] Bad Fail heavily modified

The reasons for the quality being less than good include sewage discharge affecting most of the river, physical modification of the channel for land drainage, and run-off from agricultural and rural land. 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.[56]

In March 2018, the river suffered the worst incidence of pollution ever recorded in Lincolnshire, when Omex Agriculture released ammonia into the water. It resulted in over 100,000 fish dying between Bardney and the Wash, for which the company was given a remediation notice as defined by the Environmental Damage (Prevention and Remediation) Regulations 2015. They must carry out a range of improvements to the river to ensure that its habitat is restored. Once the ammonia had been flushed out, 1.5 million fish larvae and 70,000 roach and bream were released into the river. The remediation notice was only the second to be issued since the legislation was introduced.[57]

Points of interest

[edit]

Tributaries

[edit]

The following flow into The Haven:

See also

[edit]

References

[edit]
[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
The River Witham is a 132-kilometre-long (82-mile) river in eastern , originating from springs in the Lincolnshire Limestone near South Witham, just south of in . It flows generally northward through rural countryside, passing and entering the city of Lincoln, where it is joined by the Fossdyke Canal, before turning eastward across the low-lying Fens to discharge into —a major bay on the —via The Haven estuary at . The river drains a predominantly rural catchment of approximately 3,000 square kilometres (1,200 square miles) across central and southern , encompassing about 90% arable farmland, permanent grasslands, and small urban areas. Its major tributaries include the Rivers Brant, , Bain, and Slea, along with Barlings Eau and the man-made Forty-Foot Drain, which together form an extensive network supporting agricultural irrigation and water transfer schemes like the Trent-Witham-Ancholme transfer. The upper reaches feature faster-flowing waters fed by limestone springs, transitioning to a slower, heavily modified channel in , where embankments and sluices manage tidal influences and prevent inundation of the fertile peatlands. Ecologically, the Witham supports diverse habitats valued for wildlife, including populations of native white-clawed crayfish () and (Salmo trutta), while its estuarine mouth at sustains shellfish fisheries and birdlife in a nationally protected conservation area. Economically and historically significant, the river has facilitated since Roman times through connections like the Fossdyke (dating to around 120 AD) and later 18th-century improvements by engineers such as William Jessop, enabling transport of goods amid the region's agricultural heartland. It also plays a vital role in flood risk management, protecting over 3,500 residents and 1,500 properties from river flooding and additional tidal threats, with ongoing adaptations to climate change impacts.

Physical Characteristics

Course

The River Witham originates from springs in boggy ground near the villages of and South Witham on the Leicestershire- border, at an elevation of approximately 100 m above . The river has a total length of 132 km (82 miles) and flows generally northward through before turning eastward to reach its mouth at The Haven in , where it enters . The upper Witham begins near its source and flows northward through rural countryside, passing villages such as Colsterworth, Great Ponton, and Long Bennington before reaching the town of . Continuing north from , the non-navigable upper section traverses the Vale of Belvoir, forming part of the Lincolnshire-Nottinghamshire border for a short distance, and arrives at Lincoln, where it widens into Brayford Pool, a natural lake in the city center. From Lincoln, the middle Witham flows eastward through the flat fenlands for about 15 km to Bardney, where the landscape remains low-lying and influenced by glacial formations. The lower Witham continues southeast for roughly 25 km to , becoming tidal in its final stretches and canalised alongside the upper sections to facilitate drainage and navigation across the level topography.

Hydrology and Tributaries

The of the River Witham encompasses approximately 3,261 km², predominantly within but extending into parts of and . This catchment supports extensive and includes a mix of rural landscapes, with the river serving as the primary conduit for runoff from these areas. The basin's is characterized by variable flow regimes, transitioning from spring-fed headwaters in the limestone uplands to slower, meandering flows through the low-lying fenlands downstream. Average discharge rates along the river vary significantly due to inputs from tributaries and fenland drainage. Further downstream, the river's flow is augmented by managed drainage systems. These dynamics are shaped by the permeable limestone geology upstream and the impermeable clay soils of the fens, which promote rapid surface runoff during rainfall. The River Witham receives contributions from several major tributaries, enhancing its overall hydrological regime. On the left bank, Foston Beck joins near Foston village south of Grantham, draining local farmland, while Barlings Eau, approximately 14 km in length, enters north of Lincoln near Barlings, channeling water from surrounding lowlands. The River Bain joins below Lincoln, and the River Slea enters via the Kyme Eau in the fens. On the right bank, the River Brant, about 23 km long, converges with the Witham south of Lincoln near Waddington, providing flow from the Vale of Belvoir. The River Till joins via the canalized Fossdyke Navigation at Lincoln, integrating waters from upstream Trent catchment extensions. The man-made South Forty-Foot Drain, a major drainage channel, joins near Boston. Hydrological features of the Witham include pronounced seasonal flooding risks in the fenlands, where much of the land lies below 4 m above , exacerbating inundation from river overflows, heavy rainfall, and tidal backwater effects near . The river plays a central role in regional drainage, particularly through integration with systems like the Witham Navigable Drains, an extensive network of channels managed by internal drainage boards to control fen water levels and prevent widespread flooding. These engineered features maintain summer while mitigating winter flood peaks across the low-lying catchment.

Historical Development

Pre-Industrial History

The River Witham played a significant role in settlement and activity in , with archaeological evidence pointing to its navigability for local trade and transport. Excavations have revealed enclosures and farmsteads along the river's floodplain margins, such as double-ditched curvilinear structures at Tattershall Thorpe and Stainfield Fen, suggesting organized agricultural communities that likely utilized the waterway for moving goods and livestock. Artifacts dredged from the river, including simple swords with raised midribs and plain tangs, indicate its use as a conduit for local exchange, as such items were commonly transported via waterways during this period. Additionally, the discovery of an timber causeway at Fiskerton, extending from the south bank to the north side of the Witham, points to the river serving as a key crossing point for drives and activities, with associated votive metalwork deposits underscoring its cultural and practical importance. During the Roman era, the Witham became integral to and commerce through enhancements to its course and the construction of the Fossdyke canal. The Romans improved the river's navigability from upstream to Lincoln, establishing as a key . Around AD 120, they built the 18 km Fossdyke to link the Witham at Brayford Pool in Lincoln directly to the River Trent at Torksey, enabling efficient transport of troops, supplies, and trade goods across eastern . This connection facilitated the movement of military materiel to support the colony's defenses and allowed commercial traffic in commodities like , metals, and agricultural products, integrating Lincoln into broader Roman waterway networks. The canal's design, with locks to manage water levels, reflected advanced engineering that sustained the Witham's role as a vital until the empire's decline. In the medieval period, a major natural event reshaped the Witham's lower course and economic landscape. A severe in 1014 diverted the river's mouth from its previous outlet at Witham Haven (near Bicker Haven) to flow into The Haven at , transforming the latter into a primary tidal . This shift, documented in historical accounts of widespread inundation in the , alleviated silting issues at the old mouth and enhanced navigability, propelling 's rise as a prominent port for and exports by the . The event marked a pivotal transition, aligning the river's path with emerging medieval trade routes while highlighting the fens' vulnerability to . Early medieval monasteries along the Witham fostered settlements, leveraging the river for sustenance and land management. Institutions like Bardney Abbey, founded in the late by King near the river's east bank, supported local communities and included fishponds that integrated with the surrounding landscape. Such settlements, often positioned on raised ground beside the Witham, integrated the river into daily life for , , and spiritual practices, contributing to the region's gradual humanization before widespread industrialization.

Engineering and Canalisation

Efforts to engineer the for drainage began in the , when monks in the surrounding undertook initial attempts to reclaim land by constructing basic embankments and dykes to protect against incursions and river flooding. These medieval initiatives laid rudimentary foundations for later systematic works, focusing on the low-lying fenlands east of the river to enable agricultural use. A significant advancement occurred in 1766 with the construction of the Grand Sluice at , designed by engineers John Grundy, Langley Edwards, and to regulate tidal flows and mitigate upstream flooding. The project involved excavating a new, straightened channel through , bypassing the river's meandering lower course and draining approximately 111,000 acres across , Wildmore, East, West, and Lincoln Fens. This structure featured three 17-foot-wide channels with mitre gates, enhancing both flood control and from to Lincoln. In the , William Jessop oversaw further canalisation efforts, including the deepening of key sections and straightening of the waterway from Lincoln to to improve and reduce flood risks amid growing industrial demands. Jessop's surveys, conducted around 1791 as part of broader assessments for the Witham Commissioners, informed modifications such as the 1795 deepening of the channel under Lincoln's High Bridge, which facilitated reliable passage for commercial traffic. These works built upon the pre-industrial natural course of the river, which had been prone to silting and seasonal overflows, to create a more controlled and efficient system. Post-World War II, extensive fen drainage schemes integrated the Witham Navigable Drains into a modern agricultural framework, with the construction of numerous to safeguard reclaimed lands from flooding. Key initiatives included the 1948 Wainfleet and Wrangle reclamation, the 1957 commissioning of Hobhole , and the 1976 activation of Leverton and Benington stations, all financed partly by local landowners to expand arable farming across thousands of acres. These 20th-century enhancements prioritized by linking the drains directly to the , transforming former wetlands into prime cropland while maintaining essential flood defenses.

Infrastructure and Locks

The navigation on the River Witham is supported by a series of locks and sluices that manage water levels and enable vessel passage along its 42 km course from Brayford Pool to . The maintains the channel and structures upstream, ensuring safe passage for boats with a maximum beam of 5.4 m and draught of 1.52 m. These limits apply throughout the navigable section, with headroom varying between 2.74 m near Lincoln and 3.5 m towards . The navigable section features three locks: Lincoln Lock (Stamp End), Bardney Lock, and Boston Lock (at Grand Sluice), all boater-operated and designed to accommodate narrowbeam and broadbeam vessels within the waterway dimensions. Lincoln Lock, located just south of the city at Stamp End, features a guillotine gate and serves as the primary descent from the upper Witham, controlling outflow from Brayford Pool into the canalized channel. Bardney Lock, positioned midway near the village of Bardney, uses curved mitre gates to regulate flow and prevent flooding while allowing passage for leisure craft and small commercial boats. Lock, at the downstream end near Grand Sluice, provides level control for tidal navigation, supporting the steady gradient maintained for efficient passage. At the downstream end, the Grand Sluice near consists of three channels, each approximately 5.2 m wide and fitted with gates on both landward and seaward sides to manage tidal surges and drainage. Constructed in 1766 to replace an earlier medieval structure, it includes an adjacent lock for vessel transit, with operations coordinated via radio or phone due to tidal constraints—passages are typically scheduled every four hours during daylight to align with safe water levels. The sluice and lock were upgraded in the late to enlarge capacity, and a major £15 million refurbishment began in 2025—which is ongoing as of November 2025—to reinforce flood defenses and navigation reliability. Maintenance responsibilities fall to the for the upstream infrastructure, including annual programs to combat silt accumulation from agricultural runoff and natural deposition, with schedules planned on a three-year rolling basis to preserve the required 1.52 m depth. Lock mechanisms are inspected regularly, and operations emphasize safety amid variable flows, particularly where tidal influences from affect the lower reaches below —high tides can raise levels by up to 6 m, necessitating coordinated gate management at the Grand Sluice. The oversees the Grand Sluice specifically for flood risk mitigation, integrating it with broader catchment controls.

Connected Waterways

The River Witham forms a key component of Lincolnshire's inland system, integrating with adjacent canals and drains to facilitate navigation from the Humber Estuary through the Trent and into , historically supporting trade in agricultural goods and to broader markets. This network extends the Witham's utility beyond its primary course, connecting inland regions to coastal ports like and enabling freight and leisure boating across a interconnected grid of channels. At its northern end in Lincoln, the Witham connects via Brayford Pool to the Fossdyke Navigation, an 11.3-mile (18.1 km) canal linking to the River Trent at Torksey Lock. Constructed by the Romans around 120 AD, the Fossdyke provided early access from Lincoln (ancient ) westward to the Trent and onward to the , serving as a vital for over two millennia and now accommodating modern leisure craft in a lock-free passage. Toward , the Witham integrates with the Witham Navigable Drains, a network of man-made channels branching north and south from Anton's Gowt Lock on the main river. The southern branch, via Frith Bank Drain to Lock, and the northern branch, including the 14-mile Hobhole Drain, connect to Boston Haven, historically transporting fen produce by freight and currently supporting seasonal leisure navigation from May to September under the management of the Witham Fourth District Internal Drainage Board. Parallel to the Witham's lower reaches, the South Forty-Foot Drain—also known as the Black Sluice Navigation—runs 19 miles (31 km) from Bourne to , discharging into the tidal Witham at the Haven via Grand Sluice (now featuring a lock restored in 2008). Originally developed for land drainage since the , it was reopened for navigation in 2009 as part of the Waterways Link, balancing flood control with boating access up to Donnington Bridge and enhancing connectivity within the broader system.

Environmental Status

Water Quality

The water quality of the River Witham is assessed under the (WFD) by the , with classifications reflecting chemical and ecological parameters across multiple water bodies in the catchment. In 2022, the overall ecological status for bodies in the Witham Management Catchment was predominantly moderate, with 58 out of 79 bodies at this level, 14 poor, 3 bad, and only 4 good; upper sections, such as the headwaters to the with Cringle Brook (water body ID GB105030051570) near , achieved a poor ecological status due to elevated levels from diffuse agricultural sources like poor and , as well as point sources including trade/industry and discharges. Chemical status across all 79 surface water bodies in the catchment failed in 2022, primarily due to exceedances of environmental quality standards for (PBDEs) and mercury compounds, with measures implemented but recovery pending; met good status in the upper headwaters section, though broader catchment issues persist from historical industrial legacies. A major pollution incident occurred in March 2018 when approximately 3 million litres of liquid urea ammonium nitrate (UAN) fertiliser, containing high ammonia levels, leaked from a faulty pipe at Omex Agriculture Ltd's facility near Bardney, contaminating a 46 km stretch of the River Witham to The Wash and killing over 135,000 fish in one of the largest recorded environmental incidents in the region. In response, the Environment Agency secured a remediation order in 2020 requiring Omex to maintain and enhance river habitats for 10 years, followed by a £510,190 fine and costs in 2023 after the company pleaded guilty to causing the pollution. Ongoing monitoring by the tracks key parameters such as (BOD), , and nutrients like and , which are elevated due to agricultural runoff carrying fertilisers and manures from the catchment's . Post-2018 trends indicate slight improvements in and BOD levels in affected lower reaches following the spill remediation, but persistent challenges remain from fen drainage in the lower catchment, where oxidation of soils releases stored nutrients, exacerbating . In 2024, the River Witham recorded 304 sewage spills totaling 3,802 hours, contributing to ongoing nutrient pressures. Influencing factors include agricultural runoff as the primary source of nutrients (accounting for much of the phosphate loading), urban sewage discharges contributing ammonia and pathogens in mid-catchment areas like Lincoln, and tidal mixing in the estuarine lower reaches, which can dilute pollutants but also redistribute sediments and contaminants during high flows. The 2018 spill severely impacted local fish populations, with dead fish observed across multiple species, underscoring broader risks to aquatic wildlife from acute pollution events.

Ecology and Conservation

The fenland wetlands associated with the River Witham provide critical habitats for wetland-dependent species, including otters (Lutra lutra) and water voles ( amphibius), which thrive in the river's riparian zones and adjacent marshes. These areas feature reedbeds and slow-flowing channels that support diverse communities and aquatic plants, contributing to the overall biodiversity of the . In the upper reaches near , meadow habitats along the floodplains host native flora such as wildflowers and grasses, enhancing pollinator populations and providing foraging grounds for birds and small mammals. Biodiversity in the Witham catchment faces challenges from and modification, though protected designations help mitigate losses; for instance, Sites of Special Scientific Interest (SSSIs) including floodplain grazing marsh sites along the river support resilient wetland ecosystems. Water quality stressors, such as nutrient enrichment, further impact these habitats by altering plant communities and reducing suitability for sensitive species like water voles. Recent incidents, such as weed overgrowth and dead geese reported in November 2025, highlight ongoing effects. Recent conservation efforts include the RESTORE initiative around , launched post-2020, which involves re-meandering channels through creation and reconnecting the river to its to boost diversity and natural flow dynamics; the project remains ongoing as of 2025. Complementing this, the Witham and Humber Drainage Boards' Nature Strategy (2021-2026) outlines enhancement measures, such as maintaining buffer strips for water vole and populations and promoting wetland restoration across the catchment. The Upper Witham Restoration project, recognized as a 2024 River Prize finalist, has advanced improvements in the upper catchment. The Royal Society for the Protection of Birds (RSPB) and the collaborate on floodplain restoration projects along the lower Witham, including at sites like Frampton Marsh, to enhance against flooding and , with targets for improved habitat connectivity by 2025.

Notable Sites

Landmarks

The High Bridge in Lincoln spans the River Witham and is the only surviving medieval bridge in with buildings upon it. Constructed in the with 13th-century additions, it features an semicircular arch supported by chamfered transverse and diagonal ribs, while the overlying timber-framed shops and houses date to the , including jettied structures with leaded casements, oriels, and dormers. A chapel dedicated to was erected on the east side around 1235, though it was demolished in 1763. The bridge, restored in 1902 by architect William Watkins, holds Grade I listed status and is a scheduled ancient monument due to its architectural and historic significance. Brayford Pool, located at the junction of the River Witham and the in Lincoln, served as an historic since Roman times, when the canal linked it to the River Trent around 120 AD. The pool's name derives from the 10th-century Viking occupation of Lincoln, translating from "Breit-ford" to mean "broad ford," reflecting its widened, fordable expanse formed by the Witham's natural broadening. Today, it functions as a recreational area with marinas and waterfront developments, preserving its role as one of Britain's oldest inland harbors. The Grand at marks the tidal limit of the River Witham and consists of a complex of sluice gates, a lock, and a road bridge essential for controlling water flow and enabling navigation. Built between 1764 and 1766 under an , it was designed by engineers John Grundy and Langley Edwards, with input from , featuring three gritstone channels on the upstream side and a wider lock on the downstream, protected by iron-bound timber doors and hydraulically operated gates to manage tidal surges. Opened on 3 1766, the structure facilitated fen drainage and port access, supporting 's expansion, and was modified in 1883 with additional lock gates; it holds Grade II listed status for its engineering innovation. Tattershall Castle, a 15th-century brick overlooking the River Bain—a tributary of the River —near village, stands as a prominent landmark linked to the river through the adjacent Witham Navigation and the short Tattershall Canal branch, constructed in the 1780s to connect local trade routes. Erected around 1440 by Ralph Cromwell, of , on the site of a 13th-century , it rises five storeys with facetted angle towers, an embattled , machicolations, and intricate brickwork influenced by Flemish mason Baldwin Dutchman, including a vaulted and ornate chimney pieces. Abandoned after the 17th century and restored in 1911–1925 by Lord Curzon, the castle is owned by the and designated a Grade I listed building and scheduled for its exceptional defensive architecture.

Cultural Significance

The River Witham has played a pivotal economic role in Lincolnshire's history, serving as a vital trade artery through the medieval . During the , emerged as a major export hub for , surpassing all other English ports before 1300 and facilitating extensive European commerce along the river's course. Grain, including corn shipments, was also transported downstream via the Witham to sustain urban centers like , with 's riverside granaries supplying the capital's needs in earlier centuries. In modern times, the river supports leisure boating, with regular cruises such as those operated by the Boston Belle offering scenic trips along the Witham and into , while angling remains popular, particularly for roach, , , and pike in sections like the Upper Witham managed by local associations. The river features prominently in literary works by , the renowned poet who grew up in the region and drew inspiration from its landscapes. Tennyson's poetry often evokes the Witham's meandering flow and surrounding , as seen in trailside artworks along the Water Rail Way that illustrate lines from poems like "The Lady of Shalott," linking the river to themes of isolation and natural beauty. Local surrounding the Witham centers on its recurrent floods, which have shaped communal narratives of resilience, with historical inundations—such as those documented in 19th-century accounts of mid- —embedded in tales of the river's unpredictable power and the efforts to tame it. Recreational pursuits along the River Witham emphasize its accessibility for leisure, including the 33-mile Water Rail Way path, a traffic-free trail paralleling the river from Lincoln to , ideal for walking and amid restored wetlands and historic sites. events and competitions further enhance its appeal, while the Lincoln waterfront at Brayford Pool draws visitors for its harbor views and boat tours, contributing to the city's status as a key draw in . The river also fosters community ties through events like 's Waterfront Festival, held along the Haven section of the Witham, featuring maritime displays, music, and family activities that celebrate local heritage. As a enduring emblem of Lincolnshire's identity, the Witham symbolizes the county's agricultural roots, industrial ingenuity, and natural tranquility, exemplified by artifacts like the , a Celtic masterpiece dredged from its waters and recognized as a pinnacle of prehistoric artistry.

References

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