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River Great Ouse
River in England
River in England
| Field | Value |
|---|---|
| name | River Great Ouse |
| image | DSCN1566-goba-mooring-after-brownshill-staunch 1200x900.jpg |
| image_caption | The River Great Ouse after Brownshill Staunch, near Over in Cambridgeshire |
| map | River Great Ouse map.png |
| map_caption | Great Ouse catchment |
| mapframe | yes |
| mapframe-zoom | 7 |
| subdivision_type1 | Country |
| subdivision_name1 | United Kingdom |
| subdivision_type2 | Constituent country |
| subdivision_name2 | England |
| subdivision_type4 | Counties |
| subdivision_name4 | Northamptonshire, Buckinghamshire, Bedfordshire, Cambridgeshire, Norfolk |
| length | 230. km |
| discharge1_location | Denver Sluice Catchment area 3430 km2 |
| discharge1_avg | 15.8 m3/sCatchment area 3430 km2 |
| source1_location | Syresham, West Northamptonshire, Northamptonshire, England |
| source1_coordinates | |
| source1_elevation | 150 m |
| mouth | The Wash |
| mouth_location | King's Lynn, United Kingdom |
| mouth_coordinates | |
| mouth_elevation | 0 m |
| basin_size | 8380 km2 |
| tributaries_left | Tove |
| tributaries_right | Ouzel, Cam, Lark, Little Ouse, Wissey |
| mapframe-zoom = 7
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. Authorities disagree both on the river's source and its length, with one quoting 160 mi and another 143 mi. 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 name Ouse is from the Celtic or pre-Celtic *Udso-s, and probably means simply "water" or slow flowing river. Thus the name is a pleonasm. The lower reaches of the Great Ouse are also known as "Old West River" and "the Ely Ouse", but the entire length of the river is often referred to simply as the Ouse in informal usage (the word "Great" which originally meant simply big or, in the case of a river, long is used to distinguish this river from several others called the Ouse).
Course
The river has several sources close to the villages of Syresham and Wappenham in West Northamptonshire. It flows through Brackley, provides the Oxfordshire/Northamptonshire border, then into Buckinghamshire where it flows through Buckingham, the Milton Keynes urban area (at Stony Stratford and Newport Pagnell) and Olney, then Kempston in Bedfordshire, which is the current head of navigation.

Passing through Bedford, it flows on into Cambridgeshire through St Neots, Godmanchester, Huntingdon, Hemingford Grey and St Ives, reaching Earith. Here, the river enters a short tidal section before branching in two. The artificial, very straight Old Bedford River and New Bedford River, which remain tidal, provide a direct link north-east towards the lower river at Denver in Norfolk.
The river previously ran through Hermitage Lock into the Old West River, then joined the Cam near Little Thetford before passing Ely and Littleport to reach the Denver sluice. Below this point, the river is tidal and continues past Downham Market to enter the Wash at King's Lynn. It is navigable from the Wash to Kempston Mill near Bedford, a distance of 72 mi which contains 17 locks. It has a catchment area of 8380 km2 and a mean flow of 15.5 m3/s as measured at Denver Sluice.

Its course has been modified several times, with the first recorded modification in 1236, as a result of flooding. During the 1600s, the Old Bedford and New Bedford rivers were built to provide a quicker route for the water to reach the sea. In the 20th century, construction of the Cut-Off Channel and the Great Ouse Relief Channel have further altered water flows in the region, and helped to reduce flooding.
Improvements to assist navigation began in 1618, with the construction of sluices and locks. Bedford could be reached by river from 1689. A major feature was the sluice at Denver, which failed in 1713, but was rebuilt by 1750 after the problem of flooding returned. Kings Lynn, at the mouth of the river, developed as a port, with civil engineering input from many of the great engineers of the time. With the coming of the railways the state of the river declined so that it was unsuitable either for navigation or for drainage. The navigation was declared to be derelict in the 1870s.
A repeated problem was the number of authorities responsible for different aspects of the river. The drainage board created in 1918 had no powers to address navigation issues, and there were six bodies responsible for the river below Denver in 1913. When the Great Ouse Catchment Board was created under the powers of the Land Drainage Act 1930, effective action could at last be taken. There was significant sugar beet cargo traffic on the river between 1925 and 1959, with the last known commercial traffic sailing in 1974. Leisure boating had been popular since 1904, and the post-war period saw the creation of the Great Ouse Restoration Society in 1951, who campaigned for complete renovation of the river navigation. Until 1989, the river was in the care of the Anglian Water Authority until water privatisation, when the Environment Agency became the drainage and ecology authority as well as being the navigation authority.
The Ouse Washes are an internationally important area for wildlife. Sandwiched between the Old Bedford and New Bedford rivers, they consist of washland which is used as pasture during the summer but which floods in the winter, and are the largest area of such land in the United Kingdom. They act as breeding grounds for lapwings, redshanks and snipe in spring, and are home to varieties of ducks and swans during the winter months.
Wildlife

As the water quality has improved, otters have returned to the river in numbers such that fishing lakes now require fencing to protect stocks. Paxton Pits nature reserve near St Neots has hides from which otters are regularly seen. Coarse fishing is still popular, with a wide range of fish in the river, but it is many years since large sturgeon were caught. Seals have been recorded as far upstream as Bedford. Huntingdonshire seems to be the most popular area for breeding animals in recent years.
Tributaries

Tributaries of the River Great Ouse: (upstream [source] to downstream by confluence)
- Padbury Brook: Two streams that join to form one watercourse just south of Padbury in Buckinghamshire: the eastern twin starts near Addington and the Claydons and flows 5 mi northwest to join the western twin, which starts near Somerton in Oxfordshire. From here it flows due East, through Fewcott, Stoke Lyne, Fringford and Twyford, before joining its twin and flowing 5 mi north to join the Great Ouse east of Buckingham.
- River Leck
- River Tove
- River Ouzel (or Lovat)
- River Ivel
- River Kym
- River Cam
- Soham Lode
- River Lark
- River Little Ouse
- River Wissey
- Old Bedford River
- New Bedford River (also known as Hundred Foot Drain)
- River Nar
- Gaywood River
- Babingley River
Water sports
In 1944 the annual Boat Race between the Oxford and Cambridge universities took place on this river, between Littleport and Queen Adelaide, the first time that it had not been held on the Thames; it was won by Oxford. The 2021 Boat Race was again held on the river because of the COVID-19 pandemic. The Great Ouse has been used by three clubs from Cambridge University for the training of rowers, with the Boat Club (CUBC), the Women's Boat Club (CUWBC) and the Lightweight Rowing Club (CULRC), all using facilities at Ely; the clubs merged in 2020.
The Great Ouse is a very popular river for canoeing and kayaking, particularly around Bedford which is a regional centre for the sport. Viking Kayak Club organise the Bedford Kayak Marathon with canoe racing held along the Embankment on Bedford's riverside and dates back to the original Bedford to St Neots race in 1952, believed to be the first of its kind in the country.
Bedford also benefits from the presence of weirs and sluices, creating white water opportunities. Viking organise national ranking Canoe Slalom events at the Cardington Artificial Slalom Course (CASC), which was the first artificial whitewater course in the UK, opened in 1982 adjacent to Cardington Lock, in a partnership with the Environment Agency who use it as a flood relief channel. CASC is also the venue each year for the UK's National Inter Clubs Slalom Finals, the largest canoe slalom event by participation in the UK.
Since 1978, the Bedford River Festival has been held every two years, to celebrate the link between Bedford and the coast. In addition to craft often seen on the river, the 2008 festival featured a reconstruction of a 1st-century currach, consisting of a wicker framework covered in cow hide, and capable of carrying ten people.
Notes
References
Bibliography
References
- [http://nrfa.ceh.ac.uk/data/station/info/33035 Ely Ouse at Denver Complex] {{Webarchive. link. (28 October 2017 gauging station.)
- (2012). "Headwaters: Walking to British River Sources". Frances Lincoln Limited.
- Owen, Susan. (2005). "Rivers and the British Landscape". Carnegie.
- Pokorny, Julius. "[[Indogermanisches etymologisches Wörterbuch]]".
- Mills, Anthony David. (2003). "A Dictionary of British Place Names". Oxford University Press.
- {{harvnb. Blair. 2006
- (1996). "Nitrogen fluxes through the upper estuary of the Great Ouse, England: the role of the bottom sediments.". Inter Research Science.
- "NRFA Station Mean Flow Data for 33035 - Ely Ouse at Denver Complex".
- "The RSPB: Ouse Washes". The RSPB.
- Register of Crabhouse Nunnery, British Library MS, and others
- {{harvnb. Blair. 2006
- (1940). "The Draining of the Fens". Cambridge University Press.
- {{harvnb. Boyes. Russell. 1977
- {{harvnb. Boyes. Russell. 1977
- No tolls were charged on the river below St Ives or on the New Bedford, and those responsible for drainage complained about damage to the sluices and to banks by the horses used for towing boats. A bill for a new act of Parliament to regulate the situation was defeated in 1777 after fierce opposition, and it was not until 1790 that a 'Haling Act', the '''{{visible anchor. Ouse Navigation Act 1790''' ([[30 Geo. 3]]. c. 83), was passed, which ensured that tolls were charged and landowners were repaid for damage to the banks caused by horses. These measures were a success, as there were few complaints once the new system was in place.{{harvnb. Boyes. Russell. 1977
- {{harvnb. Boyes. Russell. 1977
- {{harvnb. Adolphus. Ellis. 1837
- {{harvnb. Boyes. Russell. 1977
- {{harvnb. Boyes. Russell. 1977
- {{harvnb. Boyes. Russell. 1977
- {{harvnb. Boyes. Russell. 1977
- {{harvnb. Boyes. Russell. 1977
- Jim Shead's Canal pages. "Great Ouse Relief Channel".
- {{harvnb. Cumberlidge. 2009
- {{harvnb. Cumberlidge. 2009
- {{harvnb. Cumberlidge. 2009
- {{harvnb. Cumberlidge. 2009
- Cumberlidge. 2009
- Two locks would be required to raise boats from the Relief Channel to the River Nar.[http://www.waterways.org.uk/Waterways/PrincipalNavigations/RiverNartotheGreatOuseFloodReliefChannelLinkUnderRestoration Inland Waterways Association: ''Kings Lynn to the Great Ouse Flood Relief Channel Link''] {{Webarchive. link. (4 December 2008 , accessed 10 October 2009)
- "SLIDESHOW: Seal in the River Great Ouse".
- (11 August 2015). "Sunbathing seals make long trip inland from the Wash". BBC News.
- (January 2026). "River great ouse flooding - river great ouse flooding }}{{Dead link".
- "Get-a-map online". [[Ordnance Survey]].
- (February 2004). "Celebrate the 1944 University Boat Race!". BBC.
- (2020-11-26). "The Boat Race 2021 to be raced at Ely, Cambridgeshire".
- "CUBC: ''Facilities''".
- "CUWBC: ''Facilities''".
- "Visit Shefford, Bedford Embankment".
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