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 River Great Ouse is a river in England, the longest of several British rivers called "Ouse". From Syresham in Northamptonshire, the Great Ouse flows through Buckinghamshire, Bedfordshire, Cambridgeshire and Norfolk to drain into the Wash and the North Sea near Kings Lynn. With a course of about 143 mi (230 km), mostly flowing north and east, it is the fifth longest river in the United Kingdom. The Great Ouse has been historically important for commercial navigation, and for draining the low-lying region through which it flows; its best-known tributary is the Cam, which runs through Cambridge. Its lower course passes through drained wetlands and fens and has been extensively modified, or channelised, to relieve flooding and provide a better route for barge traffic. The unmodified river would have changed course regularly after floods.
The River Ancholme is a river in Lincolnshire, England, and a tributary of the Humber. It rises at Ancholme Head, a spring just north of the village of Ingham and immediately west of the Roman Road, Ermine Street. It flows east and then north to Bishopbridge west of Market Rasen, where it is joined by the Rase. North of there it flows through the market town of Brigg before draining into the Humber at South Ferriby. It drains a large part of northern Lincolnshire between the Trent and the North Sea.
The River Glen is a river in Lincolnshire, England with a short stretch passing through Rutland near Essendine.
North Lincolnshire is a unitary authority area in Lincolnshire, England, with a population of 167,446 in the 2011 census. The borough includes the towns of Scunthorpe, Brigg, Haxey, Crowle, Epworth, Bottesford, Kirton in Lindsey and Barton-upon-Humber. North Lincolnshire is part of the Yorkshire and Humber region.
Brigg (/'brɪg/) is a market town in North Lincolnshire, England, with a population of 5,076 in the, the population increased to 5,626 at the 2011 census. The town lies at the junction of the River Ancholme and east–west transport routes across northern Lincolnshire. As a formerly important local centre, the town's full name of Glanford Brigg is reflected in the surrounding area and local government district of the same name. The town's urban area includes the neighbouring hamlet of Scawby Brook.
The Foss Dyke, or Fossdyke, connects the River Trent at Torksey to Lincoln, the county town of Lincolnshire, and may be the oldest canal in England that is still in use. It is usually thought to have been built around AD 120 by the Romans, but there is no consensus among authors. It was refurbished in 1121, during the reign of King Henry I, and responsibility for its maintenance was transferred to the city of Lincoln by King James I. Improvements made in 1671 included a navigable sluice or lock at Torksey, and warehousing and wharves were built at Brayford Pool in the centre of Lincoln.
Sir John Rennie FRSA was the second son of engineer John Rennie the Elder, and brother of George Rennie.
The Caistor Canal was a 4-mile (6.4 km) canal in Lincolnshire, England, constructed between 1793 and 1798. It fell into disuse sometime after 1850 and was legally abandoned in 1936. It ran from the River Ancholme, near South Kelsey toward Caistor through six locks, terminating at Moortown, 3.5 miles (5.6 km) away from its intended terminus at Caistor. Parts of it were dredged in 2010, to aid flood defences in South Kelsey.
The Horncastle Canal was a broad canal which ran 11 miles from the River Witham to Horncastle in Lincolnshire, England, through twelve locks largely following the course of River Bain. The canal opened in 1802, and was abandoned for navigation in 1889.
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.
South Ferriby is a village in North Lincolnshire, England. It is situated on the south bank of the Humber Estuary and 3 miles (5 km) west from the Humber Bridge. North Ferriby is directly opposite on the Estuary's north bank. Village population was 651 in 2011.
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.
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.
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.
Horkstow is a village and civil parish in North Lincolnshire, England, 4 miles (6.4 km) south-west from Barton-upon-Humber, 1 mile (1.6 km) south from South Ferriby and 9 miles (14.5 km) north from Brigg. It lies on the B1204, and 1 mile (1.6 km) east from the navigable River Ancholme. It is one of the five "Low Villages" – Worlaby, Bonby, Saxby All Saints, Horkstow and South Ferriby – between Brigg and the River Humber, so-called because of their position below the northern edge of the Lincolnshire Wolds. Horkstow was previously part of Glanford administrative district, and before that, the North Lindsey division of Lindsey, Lincolnshire.
Worlaby is a village and civil parish in North Lincolnshire, England, 6 miles (10 km) south-west from Barton-Upon-Humber and 5 miles (8 km) north-east from Brigg. The population of the civil parish at the 2011 census was 547. It lies on the B1204, and to the east of the River Ancholme. It is one of the five Low Villages – South Ferriby, Horkstow, Saxby All Saints, Bonby, and Worlaby – between Brigg and the River Humber, named so because of their position below the northern edge of the Lincolnshire Wolds. Worlaby was part of the Glanford district, a part of the former county of Humberside between 1974 and 1996. Before that it was in the North Lindsey division of Lindsey, Lincolnshire.
The River Torne is a river in the north of England, which flows through the counties of South Yorkshire and North Lincolnshire. It rises at the Upper Lake at Sandbeck Hall, in Maltby in South Yorkshire, and empties into the River Trent at Keadby pumping station. Much of the channel is engineered, as it plays a significant role in the drainage of Hatfield Chase, which it crosses.
The River Rase is 16 mile (25 km) long tributary of the River Ancholme that flows through Lincolnshire, in the east of England.
