River Ouse, Yorkshire in the context of "York"

The River Foss is in North Yorkshire, England. It is a tributary of the River Ouse. It rises in the Foss Crooks Woods near Oulston Reservoir close to the village of Yearsley and runs south through the Vale of York to the Ouse in the centre of York. The name most likely comes from the Latin word Fossa, meaning ditch. It is mentioned in the Domesday Book. 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 deals with the common Danish and Norwegian languages – roots of words and the original meaning. The old Norse word Fos (waterfall) means impetuous. The River Foss was dammed, and even though the elevation to the River Ouse is small, a waterfall was formed. This may have led to the name Fos which became Foss.

The responsibility for the management of the river's drainage area is the Foss Internal drainage board (IDB). It has responsibility for the area from Crayke to the pre-1991 city boundary of York covering 9,085 hectares and 162.54 km of waterways. The Foss IDB is part of the York Consortium of Drainage Boards that oversees 10 IDB's in the Yorkshire region.

The Humber /ˈhʌmbər/ is a large tidal estuary on the east coast of Northern England. It is formed at Trent Falls, Faxfleet, by the confluence of the tidal rivers Ouse and Trent. From there to the North Sea, it forms part of the boundary between the East Riding of Yorkshire on the north bank and North Lincolnshire on the south bank. Also known as the River Humber, it is tidal its entire length.

Below Trent Falls, the Humber passes the junction with the Market Weighton Canal on the north shore, the confluence of the River Ancholme on the south shore; between North Ferriby and South Ferriby and under the Humber Bridge; between Barton-upon-Humber on the south bank and Kingston upon Hull on the north bank (where the River Hull joins), then meets the North Sea between Cleethorpes on the Lincolnshire side and the long and thin headland of Spurn Head to the north.

Drax power station is a large biomass power station in Drax, North Yorkshire, England. It has a 2.6 GW capacity for biomass and had a 1.29 GW capacity for coal that was retired in 2021. Its name comes from the nearby village of Drax. It is situated on the River Ouse between Selby and Goole. Its generating capacity of 3,906 megawatts (MW), which includes the shut down coal units, is the highest of any power station in the United Kingdom, providing about 6% of the United Kingdom's electricity supply.

Opened in 1974 and extended in the 1980s, the station was initially operated by the Central Electricity Generating Board. Since privatisation in 1990 ownership has changed several times, and it is operated by the Drax Group. Completed in 1986, it was the newest coal-fired power station in England until it closed in 2021. Flue gas desulphurisation equipment was fitted between 1988 and 1995. The high and low pressure turbines were replaced between 2007 and 2012.

The West Riding of Yorkshire was one of three historic subdivisions of Yorkshire, England. From 1889 to 1974 the riding was an administrative county named County of York, West Riding. The lieutenancy at that time included the city of York and as such was named "West Riding of the County of York and the County of the City of York". The riding ceased to be used for administrative purposes in 1974, when England's local government was reformed.

Contemporary local government boundaries in Yorkshire largely do not follow those of the riding. All of South Yorkshire (except Finningley) and West Yorkshire were historically within its boundaries, as were the south-western areas of North Yorkshire (including Ripon), the Sedbergh area of Cumbria, the Barnoldswick and Slaidburn areas of Lancashire, the Saddleworth area of Greater Manchester and the part of the East Riding of Yorkshire around Goole and southwest of the River Ouse.

The River Don (also called River Dun in some stretches) is a river in South Yorkshire and the East Riding of Yorkshire, England. It rises in the Pennines, west of Dunford Bridge, and flows for 69 miles (111 km) eastwards, through the Don Valley, via Penistone, Sheffield, Rotherham, Mexborough, Conisbrough, Doncaster and Stainforth. It originally joined the Trent, but was re-engineered by Cornelius Vermuyden as the Dutch River in the 1620s, and now joins the River Ouse at Goole. Don Valley is a UK parliamentary constituency near the Doncaster stretch of the river.

The Trent, the third-longest river in the United Kingdom, has its source in Staffordshire, on the southern edge of Biddulph Moor. It flows through and drains the North Midlands into the Humber Estuary. The river is known for dramatic flooding after storms and spring snowmelt, which in the past have often caused the river to change course.

The river passes through Stoke-on-Trent, Stone, Staffordshire, Rugeley, Burton-upon-Trent and Nottingham before joining the Yorkshire Ouse at Trent Falls to form the Humber Estuary, which empties into the North Sea between Kingston upon Hull in Yorkshire and Immingham in Lincolnshire. The wide Humber estuary has often been characterised as the boundary between the Midlands and Northern England ("The North").

Fulford is a historic village and civil parish on the outskirts of York, within the York district, in the ceremonial county of North Yorkshire, England. It is located 2 miles (3 km) to the south of the city, on the east bank of the River Ouse.

The population of the civil parish at the 2011 census was 2,785. It is home to Imphal Barracks, headquarters of the British Army's 15th Infantry Brigade; soldiers and their families live in married quarters outside the barracks. Fulford is a headquarters for the Royal Military Police.