The River Little Ouse, also known as the Brandon River, is a river in the east of England, a tributary of the River Great Ouse. For much of its length it defines the boundary between Norfolk and Suffolk.
The River Wissey is a river in Norfolk, eastern England. It rises near Bradenham, and flows for nearly 31 miles (50 km) to join the River Great Ouse at Fordham. The lower 11.2 miles (18.0 km) are navigable. The upper reaches are notable for a number of buildings of historic interest, which are close to the banks. The river passes through the parkland of the Arts and Crafts Pickenham Hall, and further downstream, flows through the Army's Stanford Training Area (STANTA), which was created in 1942 by evacuating six villages. The water provided power for at least two mills, at Hilborough and Northwold. At Whittington, the river becomes navigable, and is surrounded by fenland. A number of pumping stations pump water from drainage ditches into the higher river channel.
The Old Bedford River is an artificial, partial diversion of the waters of the River Great Ouse in the Fens of Cambridgeshire, England. It was named after the fourth Earl of Bedford who contracted with the local Commission of Sewers to drain the Great Level of the Fens beginning in 1630. It provided a steeper and shorter path for the waters of the Great Ouse, and was embanked to prevent them flooding the low ground of the South Fens. Throughout the project, the Earl and his Adventurers faced disruption from those who were opposed to drainage schemes. The project was deemed to have succeeded in draining the fens in 1637, but that decision was reversed in 1638. After a lull during the English Civil War, when much of the work was damaged, the Dutch engineer Cornelius Vermuyden worked with William Russell, the fifth Earl of Bedford to complete the drainage. Disruption and unrest continued while the work was carried out, resulting in the Adventurers employing armed guards. A second river, the New Bedford River, was cut parallel to the first channel, which then became the Old Bedford River. At some point, the Old Bedford River was split into two parts, when the upper section was diverted into the River Delph at Welches Dam, and the lower section was joined to the Counter Drain. Both parts retain the name, but are not connected to each other. The area between the two Bedford rivers acts as a large washland, which holds floodwater when the river channels cannot cope with the volume of water in them.
The River Wharfe is a river in Yorkshire, England originating within the Yorkshire Dales National Park. For much of its middle course it is the county boundary between West Yorkshire and North Yorkshire. Its valley is known as Wharfedale.
The River Ouse 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 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.
The Ouse is a 35 miles long river in the English counties of West and East Sussex. It rises near Lower Beeding in West Sussex, and flows eastwards and then southwards to reach the sea at Newhaven. It skirts Haywards Heath and passes through Lewes. It forms the main spine of an extensive network of smaller streams, of which the River Uck is the main tributary. As it nears the coast it passes through the Lewes and Laughton Levels, an area of flat, low-lying land that borders the river and another tributary, the Glynde Reach. It was a large tidal inlet at the time of the Domesday book in 1086, but over the following centuries, some attempts were made to reclaim some of the valley floor for agriculture, by building embankments, but the drainage was hampered by the buildup of a large shingle bar which formed across the mouth of the river by longshore drift.
The Derwent is a river in Yorkshire in the north of England. It flows from Fylingdales Moor in the North York Moors National Park, east then southwards as far as its confluence with the River Hertford then westwards through the Vale of Pickering, south through Kirkham Gorge and the Vale of York, joining the River Ouse at Barmby on the Marsh. The confluence is unusual in that the Derwent converges on the Ouse at a shallow angle in an upstream direction.
There are nine bridges across the River Ouse and eighteen smaller bridges and passages across the narrower River Foss within the city of York, England.
The siege of York in 1644 was a prolonged contest for York during the First English Civil War, between the Scottish Covenanter army and the Parliamentarian armies of the Northern Association and Eastern Association, and the Royalist Army under the Marquess of Newcastle. It lasted from 22 April until 1 July when the city was relieved by Prince Rupert of the Rhine. Rupert and Newcastle were defeated the next day at the decisive Battle of Marston Moor, and the siege resumed until the city was surrendered on easy terms on 16 July.
Marton-cum-Moxby is a civil parish in North Yorkshire, England. The population of the parish was less than 100 at the time of the 2011 Census, therefore its details were included with Farlington. It lies to the east of the villages of Stillington and Farlington, near Easingwold. The settlements are the hamlets of Marton-in-the-Forest and Moxby, both agricultural in character.
Stillington is a village and civil parish in the district and county of North Yorkshire, England. It lies on the York to Helmsley road about 10 miles (16 km) north of York. Stillington Mill was the endpoint of the Foss Navigation Act of 1793.
Crayke is a village and civil parish in North Yorkshire, England, about 2 miles (3.2 km) east of Easingwold.
Oulston is a village and civil parish in Hambleton district of North Yorkshire, England. It lies about 3 miles (5 km) north-east of Easingwold. Remains of a Roman villa have been found in the area. The village is within the Howardian Hills Area of Outstanding Natural Beauty
The River Wiske is a tributary of the River Swale in Yorkshire, England. The Wiske gives its name to several villages it passes through. The name Wiske is derived from an Old English word wisca meaning a water meadow. It was once known as the Foulbroke, a name for which some writers commented that it was well deserved.
Brandsby is a village in North Yorkshire, England. The village is the main constituent of the Brandsby-cum-Stearsby Civil Parish in the District of Hambleton. The village is mentioned in the Domesday book. It lies between Easingwold and Hovingham, some 12.3 miles (19.8 km) north of York.
The Ebor Way is a 70-mile (112 km) long-distance footpath from Helmsley, North Yorkshire to Ilkley, West Yorkshire, via the city of York, England. It takes its name from Eboracum, the Roman name for York.
The Centenary Way is a route devised to celebrate the 100th anniversary of North Yorkshire County Council. It was opened by Chris Brasher in 1989 to mark the Centenary of the governance by County Councils.
The River Foulness is a river in the East Riding of Yorkshire, England. Its name is derived from Old English fūle[n] ēa, meaning “dirty water”. Maintenance responsibilities for the river transferred from the Environment Agency to the Market Weighton Drainage Board on 1 October 2011. Market Weighton Drainage Board subsequently amalgamated with the Lower Ouse Internal Drainage Board on 1 April 2012 to create the Ouse and Humber Drainage Board. The river discharges into the Humber Estuary via Market Weighton Canal. Water levels within the river, its tributaries and the canal are managed and controlled by the Environment Agency. The river lies in an area known as the Humberhead Levels.
The Foss Barrier consists of a retractable floodgate and pumping station owned and managed by the Environment Agency. It straddles the River Foss in York, just above the confluence with the River Ouse. The barrier’s purpose is to prevent water from the Ouse flowing upstream into the Foss, raising water levels and flooding properties along the River Foss. The pumps next to the flood gate move water around the barrier via a side culvert so that it can continue to drain into the Ouse. This prevents water levels on the Foss rising when the barrier is closed. The Ouse’s normal water level at York is approximately 5 metres AOD. When the river level reaches 7.5 metres AOD, the barrier is lowered into the Foss, shutting it off from the Ouse. The electrically driven barrier takes less than five minutes to lower into position. The barrier operates as a ‘turn and lift’ gate so it opens and closes in a similar way to a garage door. The pump-house attached to the barrier maintain the water level in the Foss at around 6.5 metres AOD. When the flood subsides and the level of the Ouse drops back to 6.5 metres, the levels in both rivers are equalised so the barrier opens, and the pumps shut down.
Holgate Beck is a small watercourse that flows north-eastwards through Holgate across the west side of the City of York, England. Primarily flowing through Holgate, from which it derives its name, the beck drains a large part of Askham Bog and Hob Moor, then running underneath the various lines near York railway station. It empties into the River Ouse at Water End, being one of five main tributaries for the River Ouse in York, and consequently added to the flooding in the river and immediate environs. To counter this, some flood diversionary schemes have been implemented near to Askham Bog and Hob Moor.