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The River Ouse (/ uː z / 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 ...
This is a list of current bridges and other crossings of the River Ouse in Yorkshire, and are listed from Ouse Gill Beck downstream to the river's mouth. The River Ouse is listed on mapping as starting where the Ouse Gill Beck enters the River Ure, just south of the village of Great Ouseburn , ( SE473604 ). [ 1 ]
The River Ouse flows to the east where it turns into the Humber, and the River Trent flows northwards. It curves to the east near the confluence, although this is largely engineered, rather than natural. A training wall was built on the western bank of the Trent after the First World War, in an attempt to keep the channel in a known position ...
Bridges across the River Ouse, Yorkshire (18 P) I. Isle of Axholme (5 C, 42 P) O. Ouse catchment (2 C, 25 P) T. Tributaries of the River Ouse, Yorkshire (1 C)
View of the River Ouse in York from Lendal Bridge Simplified map of Yorkshire's rivers. This is a list of named rivers that flow either wholly or partially within the boundaries of the four ceremonial counties that form Yorkshire. There are twenty five rivers of at least 20 kilometres (12 miles) in total.
Cawood Bridge is a swing bridge which spans the Yorkshire River Ouse in North Yorkshire, England. Construction was authorised in 1870, with the formation of the Cawood Bridge bridge company. [ 1 ] It was opened on 31 July 1872 to replace the ferry , and is located about halfway between Naburn and Selby .
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The River Foss is a left bank tributary of the River Ouse, situated near the York Castle. In the years 1947, 1978, 1982 and end of 2015 flooding occurred causing many areas to be under water. In 1982, a feasibility study was undertaken that indicated flood levels in the Foss are directly related to River Ouse levels.