River Ouse, Yorkshire

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River Ouse
Dawn over the River Ouse - geograph.org.uk - 1088602.jpg
The River Ouse in York
Ouse (Yorkshire).png
River Ouse
Location
Country England
County Yorkshire
Physical characteristics
Source River Ure
  locationCuddy Shaw Reach, near Linton-on-Ouse
  coordinates 54°2′4″N1°16′30″W / 54.03444°N 1.27500°W / 54.03444; -1.27500
  elevation33 ft (10 m)
Mouth Humber Estuary
  location
Trent Falls
  coordinates
53°42′8″N0°41′46″W / 53.70222°N 0.69611°W / 53.70222; -0.69611 Coordinates: 53°42′8″N0°41′46″W / 53.70222°N 0.69611°W / 53.70222; -0.69611
  elevation
0 ft (0 m)
Length52 mi (84 km)
Basin size4,133 sq mi (10,704 km2)
Discharge 
  location Skelton [1]
  average1,830 cu ft/s (51.7 m3/s)

The River Ouse ( /ˈz/ OOZ) is a river in North Yorkshire, England. Hydrologically, the river is a continuation of the River Ure, and the combined length of the River Ure and River Ouse makes it, at 129 miles (208 km), the sixth longest river of the United Kingdom and (including the Ure) the longest to flow entirely in one county. The length of the Ouse alone is about 52 miles (84 km) but the total length of the river is disputed.

Contents

It is a matter of opinion as to whether the River Ouse is formed at the confluence of the River Ure and the much smaller Ouse Gill Beck at Cuddy Shaw Reach near Linton-on-Ouse, about six miles downstream of the confluence of the River Swale with the River Ure. An alternative opinion is recorded in a publication published in The Yorkshire Post in a series dated 1891, written and illustrated by Tom Bradley. His description and bird’s eye view maps - specifically in his account of the River Swale - suggests that the River Ouse starts at the confluence of the Swale and the Ure. His narrative states that the Ouse has no specific source, simply flowing from the stated confluence until it runs into the Humber at the confluence of the Ouse and Trent.

Continuing the path of the Ouse downstream from Linton-on-Ouse, it then flows through the city of York and the towns of Selby and Goole before joining with the River Trent at Trent Falls, near the village of Faxfleet, then entering the Humber Estuary.

The Ouse's system of tributaries includes the Derwent, Aire, Don, Wharfe, Rother, Nidd, Swale, Ure, and Foss. Together they drain a large part of the Pennines, and much of the Yorkshire Dales and North York Moors.

The Ouse valley is a wide, flat plain; heavy rainfall higher in the river's drainage basin can bring severe flooding to settlements. In recent years York, Selby, and villages in between have been flooded.

Sources

The 2010 Floods in York, caused by the River Ouse A flooded Queen's Staith - viewed from Ouse Bridge - geograph.org.uk - 1730987.jpg
The 2010 Floods in York, caused by the River Ouse

The traditional source of the Ouse is in the village of Great Ouseburn, and is marked by a stone column reading "OUSE RIVER HEAD... OUSEGILL SPRING Ft. YORK 13 miles BOROUGHBRIDGE 4 miles". [2] The site is 38 yards (35 m) from the present course of Ouse Gill Beck, a small stream earlier known as Usekeld Beck, meaning "Spring or source of the Ouse" (from Old Norse kelda "spring"). [3]

The start of the Ouse is now considered to be the point where Ouse Gill Beck joins the River Ure, 1.6 miles (2.5 km) south east of Great Ouseburn.

Etymology

The origin of the name is uncertain. The name was first recorded in about 780 as Usa. It has been speculated that the name is of Romano-British origin, from an assumed word udso-, assumed to be derived from the Indo-European root wed-, meaning "water". [4] Other sources prefer a Proto-Celtic. [5]

It has been suggested that the Ouse was once known as the 'Ure', but there seems to be no supporting evidence for this claim. The suggestion that the name derives from the Romano-British name of the Ure, assumed to be Isurā from the Roman name for Aldborough, and over time evolved into Isis and finally the Saxon Ouse, would go some way to explaining how the little tributary Ouse Gill Beck usurps the name of the much larger River Ure. [6] However the form Ouse is little changed from the eighth century.

The York district was settled by Norwegian and Danish people, so parts of the place names could be old Norse. Referring to the etymological dictionary "Etymologisk ordbog", ISBN   82-905-2016-6 dealing with the common Danish and Norwegian languages - roots of words and the original meaning: Os - the mouth of a river. The old Norse wording oss, gradation form ouso.

The Ouse is navigable throughout its length. Seagoing vessels use the river as far as Howdendyke. The inland port of Goole also accepts seagoing vessels on a regular basis. Goole also offers access to the Aire and Calder Navigation. At Selby there is access to the Selby Canal. The river is tidal up to Naburn; the resultant tidal bore is known locally as "the Aegir". [7]

At Naburn there is a weir with locks, so that boats of 150 feet (45.7 m) length and 15 feet (4.6 m) beam can reach York. [8] [9] Above York there is another weir with locks at Linton-on-Ouse, which allows boats of 66 feet (20 m) length to proceed to the River Ure Navigation. [10] Adjacent to the lock is Linton Lock Hydro plant. This is capable of generating enough electricity to power 450 homes. [11]

The navigation authority is Associated British Ports from Trent Falls to Goole railway swing bridge at Skelton, and the Canal & River Trust upstream from there. [10]

In the 18th and 19th centuries, there was considerable commercial traffic on the river, mainly from Selby, which then had a custom house, downstream. After the 1826 opening of the Aire and Calder Navigation, most traffic became concentrated on the port of Goole. This continues, although the coal trade which formed the backbone of the river trade has ceased.

Settlements

(From the confluence of Swale and Ure)

(Joins Trent at Trent Falls to form Humber) [10]

Flooding

With both the Ouse and the Foss running through York, flooding has been a problem throughout its documented history. Flooding is known to have occurred in 1263, 1316, 1564, 1625, 1638, 1947, 1978, 1982, 2000, 2007, 2010, and 2015. [12] [13] In November 2000, the floods reached a height of 5.4 metres (18 ft) above sea level, [14] whilst over the Christmas period of 2015, the level reached 5.2 metres (17 ft). [15] A barrier was installed on the mouth of the River Foss in York city centre in 1989, [16] so that when the Ouse was in flood, water would not run upstream of the Foss and flood the city. [17] Flooding occurs typically due to heavy rainfall further upstream in the catchment area of the Ouse (Swale, Ure, Nidd) which covers 3,300 square kilometres (1,300 sq mi), (the Foss catchment is 200 square kilometres (77 sq mi). [18]

Low-lying land around the villages of Kelfield, Riccall, Wistow and Cawood, which are south of York, are designated as a floodplain, though it can cause damage to properties there. In February 2020, it was estimated that over 3,000 acres (1,200 ha) of fields were under floodwater, making the size comparable to that of Windermere, Englands' largest natural lake. [19]

As the Ouse is tidal as far inland as Naburn, this means that flooding can occur due to heavy rainwater or tidal surges in the downstream settlements of Selby and Goole. [20]

See also

Related Research Articles

River Aire River in Yorkshire, England

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Aire and Calder Navigation Canal in West Yorkshire, England

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River Foss River in North Yorkshire, England

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River Derwent, Yorkshire

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Selby Town and civil parish in North Yorkshire, England

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Bridges of York

There are nine bridges across the River Ouse within the city of York, England, and sixteen smaller bridges and passages across the narrower River Foss.

River Ure River in North Yorkshire, England

The River Ure in North Yorkshire, England is approximately 74 miles (119 km) long from its source to the point where it becomes the River Ouse. It is the principal river of Wensleydale, which is the only major dale now named after a village rather than its river. The old name for the valley was Yoredale after the river that runs through it.

Adlingfleet Village in the East Riding of Yorkshire, England

Adlingfleet is a drained, fertile, former marshland village in the East Riding of Yorkshire, England, that forms part of the civil parish of Twin Rivers. It is 6.5 miles (10.5 km) east-southeast of Goole town centre. Its sea wall along the far north-east is set back from the Ouse estuary leaving the largest single reedbed in England.

Barlby Village in North Yorkshire, England

Barlby is a linear village in North Yorkshire, England. It is situated 2 miles (3 km) to the north-east of the market town of Selby, and is bordered to the west by the River Ouse and to the east by the A19 Barlby bypass. Across the bypass is Barlby's smaller sister village, Osgodby with which it forms the civil parish of Barlby with Osgodby.

Blacktoft Village and civil parish in the East Riding of Yorkshire, England

Blacktoft is a village and civil parish in the East Riding of Yorkshire, England. The village is situated on the north bank of the River Ouse, 1 mile (1.6 km) west from where it joins the River Trent and becomes the Humber. It is approximately 6 miles (10 km) east from Howden and 23 miles (37 km) south-east from the county town of York. Blacktoft lies within the Parliamentary constituency of Haltemprice and Howden an area that mainly consists of middle class suburbs, towns and villages. The area is affluent, placed as the 10th most affluent in the country in a 2003 Barclays Private Clients survey, and has one of the highest proportions of owner-occupiers in the country.

Naburn Village and civil parish in North Yorkshire, England

Naburn is a small village and civil parish in the unitary authority of the City of York in North Yorkshire, England. It lies on the eastern side of the River Ouse about 4 miles (6.4 km) south of York. According to the 2001 census the parish had a population of 470, increasing to 516 at the 2011 census.

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River Wiske

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Yokefleet Hamlet in the East Riding of Yorkshire, England

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Selby Canal

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Topographical areas of Yorkshire

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Bedale Beck Watercourse in North Yorkshire, England

Bedale Beck is a river that flows through the eastern end of Wensleydale and passes through Crakehall, Bedale and Leeming before entering the River Swale at a point between Morton-on-Swale and Gatenby. Between source and mouth its length is 25.7 miles (41 km).

References

  1. Ouse at Skelton gauging station. This station only covers 1,280 sq mi (3,315 km2) or 31% of the catchment area.
  2. "Great Ouseburn Parish Website" . Retrieved 31 August 2014.
  3. Smith, A. H. (1961). The Place-names of the West Riding of Yorkshire. 5. Cambridge University Press. p. 5.
  4. Smith, A. H. (1962). The Place-names of the West Riding of Yorkshire. 7. Cambridge University Press. pp. 133–134.
  5. Watts, Victor, ed. (2010). "Ouse". The Cambridge Dictionary of English Place-Names. Cambridge University Press. p. 456. ISBN   978 0 521 16855 7.
  6. Ekwall, E. English River Names (Oxford University Press: 1928). Waite, Alice. Exploring the Yorkshire Ouse (Countryside Productions: 1988)
  7. Lewis, David (2017). River Ouse Bargeman (1 ed.). Barnsley: Pen & Sword. pp. 15–16. ISBN   978-1-47388-069-6.
  8. Szyca, G. (2011). Comprehensive Methods of the Minimum Safe Under Keel Clearance Valuation to the Restricted Tidal Waters. In: Weintrit, A. and Neumann, T. (Eds.) Methods and Algorithms in Navigation: Marine Navigation and Safety of Sea Transportation. London: Taylor and Francis Group, pp. 51–56.
  9. Broadhead, I. E. (1982). Portrait of the Yorkshire Ouse. London: Hale, p. 126.
  10. 1 2 3 "Yorkshire Ouse". Waterways Association. Retrieved 5 November 2015.
  11. "River Ouse set to power 450 homes near York". York Press. 8 March 2019. Retrieved 20 October 2020.
  12. "Flood Heights on the Ouse | York Civic Trust". yorkcivictrust.co.uk. Retrieved 20 October 2020.
  13. "86 spectacular photos from three of York's worst ever floods". York Press. 6 December 2015. Retrieved 20 October 2020.
  14. Laycock, MIke (16 February 2020). "Here's what happened when the Ouse last rose to 5.4 metres: 10 images from the 2000 floods". York Press. Retrieved 20 October 2020.
  15. "York floods 2015: How the devastating floods unfolded and how York rallied superbly". York Press. 28 July 2016. Retrieved 20 October 2020.
  16. Tapsell, S M; Tunstall, S M; Fordham, M (1993). "Flooding and Flood Defences in York" (PDF). environmentdata.org.uk. National Rivers Authority. p. 15. Retrieved 20 October 2020.
  17. Gosden, Emily; Finnigan, Lexi (28 December 2015). "York floods: Why did the Foss Barrier fail?". The Telegraph. Retrieved 20 October 2020.
  18. STF 2017, p. 11.
  19. Newton, Grace (27 February 2020). "The flooded Ouse washlands in Yorkshire contain almost as much water as Lake Windermere". The Yorkshire Post. Retrieved 20 October 2020.
  20. Longfield, Sean Anthony (1998). River response to recent environmental change in the Yorkshire Ouse basin, northern England (Report). Leeds: University of Leeds. p. 191. OCLC   59479441.

Sources