River Glen, Lincolnshire
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Boothby Pagnall | |
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• location | River Welland, below Spalding |
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The River Glen is a river in Lincolnshire, England with a short stretch passing through Rutland near Essendine.
The river's name appears to derive from a
Naming
In the language of the
Course
The river has two sources, both in the low ridge of
Most of the water from the West Glen river no longer joins that from the East Glen, as it now flows along the Greatford Cut to join the River Welland upstream of
By the time the East and West rivers join, they are only just above the 35-foot (11 m) contour.
Beyond Guthram Gowt, the river flows in a north-easterly direction, and is flanked on both sides by drainage ditches because the land is low-lying. It passes through Pinchbeck and Surfleet to reach the tidal entrance sluice where it joins the River Welland.[4] The sluice is only navigable when the tidal level is the same as the river level.
History
Close to the year 500, the spread of Anglian settlement had recently reached Baston, at the other end of this Roman road, on the landward side of this fen but burial at the Urns Farm cemetery alongside King Street then stopped abruptly.[citation needed]
Compared to its neighbour, the Welland, there are few records of the history of the Glen. Dugdale, writing his book The History of Imbanking and Drayning of divers Fenns and Marshes in 1662, which was based on personal observations he made during a trip to the Fens in May 1657, and the records of the Fens Office, most of which were destroyed in the Great Fire of London in 1666, thought it was the least of the rivers he had seen, and recorded that it "serveth almost to none other use, but to carry away so much of its own water, with the rill descending from Burne, as can be kept between two defensible banks." The embanking of the lower river had thus already been done by the time of his account.[9]
Both the Bourne Eau and the Glen were affected by flooding, causing failure of the banks, which was addressed in the Black Sluice act of 1765. The history of navigation is intimately tied up with that of the Bourne Eau, since Bourne was the main centre of population above Spalding. The Bourne Eau act of 1781 appointed trustees, who were to scour and cleanse the river, and could charge tolls to fund the operation. Corn and wool passed down the river, bound for Boston, while coal and groceries were the principal cargo in the opposite direction. In 1792, Thomas Hawkes wrote about trade in timber, which was carried from Bourne to Spalding, and there was a boat which carried passengers to the market at Spalding on Tuesdays, but he comments that the service was erratic, as there was often too little or too much water for the vessels to operate. The Black Sluice Commissioners installed flood doors between the Glen and the Bourne Eau at Tongue End, to prevent high water levels in the Glen passing up the river to Bourne.[9]
Breaching of the banks by floodwater was a continual problem, with six breaches of the north bank recorded between 1821 and 1882, and eight of the south bank in the same period. Measurement showed that the river level rose by 9 or 10 inches (23 or 25 cm) for every 0.25 inches (6.4 mm) of rain falling on the river's catchment area. The arrival of railways in the area resulted in a rapid decline of river traffic. A railway from Boston to Spalding opened in 1848, while the line from Spalding opened to Bourne in 1866 and on to Sleaford in 1872. Although occasional boats were still reaching Bourne in 1857, the self-acting doors at Tongue End were replaced by a sluice in the 1860s, which prevented passage from the Glen to the Bourne Eau, although the right of navigation was not officially revoked until 1962,[9] as part of flood defence measures which included the replacement of the sluice by a pumping station in 1966.[13]
Once the route to Bourne was closed off, there was little trade on the river, although a short section of about 1 mile (1.6 km) was used by barges until the 1920s. Although the present head of navigation is at Tongue End, there is evidence that lighters capable of carrying 15 tons used to navigate to Kate's Bridge, where the Lincoln to Peterborough turnpike road crossed the river, and there are the remains of moorings at Greatford Hall, although navigation to there must have ceased after Kate's Bridge was rebuilt.[9]
In 1734, John Grundy, one of the pioneers in applying scientific principles to the solution of civil engineering problems, was asked by the Adventurers of Deeping Fen to consider the drainage of 47 square miles (120 km2) of fenland to the west of Spalding. His plans included the construction of a reservoir which covered 10 acres (4.0 ha), impounded by a sluice at Surfleet. At low tide, the water would be released, and the scouring action would deepen the channel, with a consequent improvement in drainage. Humphrey Smith directed the construction, with Grundy acting as engineer, which was completed in 1739, according to a plaque fixed to it at the time. The sluice had three openings, each 8 feet (2.4 m) wide, with pointed doors on the downstream site, which closed as the tide rose, and lifting gates on the upstream side, which would be raised to discharge the water.[14] The present sluice was erected by the Trustees of the Deeping Fen Drainage Act, 1856. The first stone was laid by Lord Kesteven on 17th February 1879 and the sluice opened in November 1879 at a total cost of £15,000.
Development
The Environment Agency are the navigation authority responsible for the river. They issue licences for its use, and operate Surfleet sluice when required. While the river is navigable for 11.5 miles (18.5 km) to Tongue End, the upper reaches above Pinchbeck Bars are only suitable for smaller boats, as there are no locations where it is possible to turn a boat which is over 30 feet (9.1 m) long.[15] However, the 8.9-mile (14.3 km) section of the river from its source to Guthram Gowt forms part of the proposed Fens Waterways Link, which will ultimately link the River Witham to the River Nene, via the South Forty-Foot Drain, the River Glen, the River Welland and some upgraded drains near Peterborough. Phase One, the connection of the South Forty-Foot Drain to The Haven at Boston by a new lock,[16] was completed by December 2008, and was officially opened on 20 March 2009.[17] Construction of the second phase of the project, which will involve making the South Forty-Foot Drain navigable from Donington to Guthram Gowt, where a connection with the River Glen will be made, has been delayed by the change in the economic climate, and the complexity of the task.[18]
Water quality
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
The water quality of the River Glen system was as follows in 2019.
Section | Ecological Status | Chemical Status | Length | Catchment | Channel |
---|---|---|---|---|---|
West Glen – Upper[20] | Poor | Fail | 14.0 miles (22.5 km) | 28.55 square miles (73.9 km2) | |
The Tham[21] | Moderate | Fail | 6.9 miles (11.1 km) | 9.38 square miles (24.3 km2) | |
West Glen – conf West Glen trib to conf East Glen River[22] | Moderate | Fail | 18.8 miles (30.3 km) | 32.56 square miles (84.3 km2) | |
Grimsthorpe Park Brook[23] | Good | Fail | 2.1 miles (3.4 km) | 8.82 square miles (22.8 km2) | |
East Glen River[24] | Poor | Fail | 17.9 miles (28.8 km) | 41.25 square miles (106.8 km2) | |
Glen[25] | Moderate | Fail | 16.7 miles (26.9 km) | 22.02 square miles (57.0 km2) | artificial |
The reasons for the quality being less than good include sewage discharge affecting most of the river, physical modification of channels, ground water abstraction, and poor management of agricultural and rural land adjacent to the river system. Like many 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.
Points of interest
See also
- Rivers of the United Kingdom
References
- ^ Schrijver, Peter, Studies in British Celtic Historical Phonology, Rodopi, 1995, p. 115
- ^ Historic England. "Bridge over East Glen River, Toft (1165586)". National Heritage List for England. Retrieved 29 December 2010.
- ^ Historic England. "Manthorpe Bridge (1165592)". National Heritage List for England. Retrieved 29 December 2010.
- ^ a b c d e 1:25000 map, Sheets 234, 247, 248, 249. Ordnance Survey.
- ^ Historic England. "Bridge over West Glen River, Greatford (1062685)". National Heritage List for England. Retrieved 29 December 2010.
- ^ Boyes & Russell 1977, pp. 248–250
- ^ "Fletland Mill cottage". Explore Lincolnshire. Archived from the original on 30 November 2010.
- ^ Historic England. "Kate's Bridge, Baston (1062703)". National Heritage List for England. Retrieved 29 December 2010.
- ^ a b c d e Boyes & Russell 1977, pp. 251–253
- ^ The Camelot Project. "From: The History of the Britons by Nennius". University of Rochester. Retrieved 21 March 2011.
- ^ Thomas Green. "Lincolnshire and the Arthurian Legend" (PDF). pp. 2–4. Retrieved 21 March 2011.
- ^ "Aerial photograph of Guthram Gowt". Bing Multi-Map. Retrieved 23 January 2010.
- ^ "History of the Draining of the Fens in the Black Sluice Area". The Black Sluice Internal Drainage Board. Archived from the original on 28 April 2011. Retrieved 29 December 2010.
- ^ Skempton 2002, p. 277
- ^ Cumberlidge 2009, pp. 124–125.
- ^ IWA Head Office Bulletin – March 2008 – Issue 134
- ^ "Newsletter 17". Lincolnshire Waterways Partnership. March 2009: 3, 13.
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(help) - ^ "Newsletter 23". Lincolnshire Waterways Partnership. October 2010: 12.
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(help) - ^ "Glossary (see Biological quality element; Chemical status; and Ecological status)". Catchment Data Explorer. Environment Agency. Retrieved 15 May 2017.
- ^ "West Glen – Upper". Catchment Data Explorer. Environment Agency. Retrieved 13 July 2018.
- ^ "The Tham". Catchment Data Explorer. Environment Agency. Retrieved 13 July 2018.
- ^ "West Glen – conf West Glen trib to conf East Glen River". Catchment Data Explorer. Environment Agency. Retrieved 13 July 2018.
- ^ "Grimsthorpe Park Brook". Catchment Data Explorer. Environment Agency. Retrieved 13 July 2018.
- ^ "East Glen River". Catchment Data Explorer. Environment Agency. Retrieved 13 July 2018.
- ^ "Glen". Catchment Data Explorer. Environment Agency. Retrieved 13 July 2018.
Bibliography
- Boyes, John; Russell, Ronald (1977). The Canals of Eastern England. David and Charles. ISBN 978-0-7153-7415-3.
- British Geological Survey, (solid & drift) 1:50,000 Series, Sheet 144.
- Cumberlidge, Jane (2009). Inland Waterways of Great Britain (8th Ed.). Imray Laurie Norie and Wilson. ISBN 978-1-84623-010-3.
- Mayes, P.; Dean, M.J. (1976). An Anglo-Saxon Cemetery at Baston, Lincolnshire. The King's England Press. ISBN 0-904680-05-3.
- Phillips, C.W. (1970). The Fenland in Roman Times. Royal Geographic Society. pp. Map 3 and the corresponding part of the gazetteer. ISBN 978-0-902447-02-8.
- Skempton, Sir Alec; et al. (2002). A Biographical Dictionary of Civil Engineers in Great Britain and Ireland: Vol 1: 1500 to 1830. Thomas Telford. ISBN 0-7277-2939-X.
- Wheeler, W.H. (1896). A History of The Fens of South Lincolnshire. Reprinted 1990 - Paul Watkins. ISBN 1-871615-39-9.
External links
Media related to River Glen, Lincolnshire at Wikimedia Commons