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 Vale of York is an area of flat land in the northeast of England. The vale is a major agricultural area and serves as the main north–south transport corridor for Northern England.
The East Riding of Yorkshire, or simply East Riding or East Yorkshire, is a county in Northern England. It borders North Yorkshire to the north and west and North Lincolnshire to the south. The coastal towns of Bridlington and Hornsea are popular with tourists from inland areas, and the port city of Kingston upon Hull is an economic, transport and tourism centre which also receives much sea freight from around the world. The current East Riding of Yorkshire came into existence in 1996 after the abolition of the County of Humberside and the ancient market town of Beverley is where the councils administrative HQ is situated. The landscape is mainly rural, consisting of rolling hills, valleys and flat plains with many small villages and some towns scattered amid the Yorkshire Wolds. Major settlements include Kingston upon Hull, Beverley, Bridlington and Goole. At the 2011 United Kingdom census, its population was 334,179.
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.
The Pennines, also known as the Pennine Chain or Pennine Hills, are a more-or-less continuous range of hills and mountains running between three regions of Northern England: North West England on the west, and North East England and Yorkshire and the Humber on the east. Commonly described as the "backbone of England", the range stretches northwards from the Peak District at the southern end, through the South Pennines, the Yorkshire Dales and North Pennines to the Tyne Gap, which separates the range from the Cheviot Hills across the Anglo-Scottish border. South of the Aire Gap is a western spur into east Lancashire, comprising the Rossendale Fells, West Pennine Moors and the Bowland Fells in North Lancashire. The Howgill Fells and Orton Fells in Cumbria are sometimes considered to be Pennine spurs to the west of the range. The Pennines are an important water catchment area with numerous reservoirs in the head streams of the river valleys.
Wensleydale is the dale or upper valley of the River Ure on the east side of the Pennines, one of the Yorkshire Dales in North Yorkshire, England.
Holderness is an area of the East Riding of Yorkshire, on the east coast of England. An area of rich agricultural land, Holderness was marshland until it was drained in the Middle Ages. Topographically, Holderness has more in common with the Netherlands than with other parts of Yorkshire. To the north and west are the Yorkshire Wolds. The Prime Meridian passes through Holderness just to the east of Patrington and through Tunstall to the north.
Swaledale is one of the northernmost dales (valleys) in Yorkshire Dales National Park, located in northern England. It is the dale of the River Swale on the east side of the Pennines in North Yorkshire.
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.
Yorkshire is a historic county of England, centred on the county town of York. The region was first occupied after the retreat of the ice age around 8000 BC. During the first millennium AD it was inhabited by celtic Britons and occupied by Romans, Angles and Vikings. The name comes from "Eborakon" an old Brythonic name which probably derives from "Efor" or "the place of the yew-trees." Many Yorkshire dialect words and aspects of pronunciation derive from old Norse due to the Viking influence in this region. The name "Yorkshire", first appeared in writing in the Anglo-Saxon Chronicle in 1065. It was originally composed of three sections called Thrydings, subsequently referred to as Ridings.
Lake Pickering was an extensive proglacial lake of the Devensian glacial. It filled the Vale of Pickering between the North York Moors and the Yorkshire Wolds, when the ice blocked the drainage, which had flowed north-eastwards past the site of Filey towards the Northern North Sea basin. The lake surface rose until it overflowed southwards and cut an exit between the Howardian Hills and the Yorkshire Wolds at Kirkham Priory between Malton and Stamford Bridge, so creating the River Derwent.
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.
The Geology of Yorkshire in northern England shows a very close relationship between the major topographical areas and the geological period in which their rocks were formed. The rocks of the Pennine chain of hills in the west are of Carboniferous origin whilst those of the central vale are Permo-Triassic. The North York Moors in the north-east of the county are Jurassic in age while the Yorkshire Wolds to the south east are Cretaceous chalk uplands. The plain of Holderness and the Humberhead levels both owe their present form to the Quaternary ice ages. The strata become gradually younger from west to east.
The Humberhead Levels is a national character area covering a large expanse of flat, low-lying land towards the western end of the Humber estuary in northern England. The levels occupy the former Glacial Lake Humber, an area bounded to the east by the Yorkshire Wolds and the northern Lincolnshire Edge, a limestone escarpment, and to the west by the southern part of the Yorkshire magnesian limestone ridge. In the north the levels merge into the slightly more undulating Vale of York close to the Escrick glacial moraine, and to the south merge into the Trent Vale.
The Yorkshire Dales Rivers Trust was formed in 2004 with a remit to improve, restore and conserve the rivers Swale, Ure, Wharfe and Nidd whose headwaters lie within the Yorkshire Dales National Park and the Nidderdale Area of Outstanding Natural Beauty. The trust is a member of the Association of Rivers Trusts which set up as a charity in 2001 to represent member trusts and assist them with conserving river catchments across England and Wales.
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 Natural Areas of England are regions, officially designated by Natural England, each with a characteristic association of wildlife and natural features. More formally, they are defined as "biogeographic zones which reflect the geological foundation, the natural systems and processes and the wildlife in different parts of England...".
A National Character Area (NCA) is a natural subdivision of England based on a combination of landscape, biodiversity, geodiversity and economic activity. There are 159 National Character Areas and they follow natural, rather than administrative, boundaries. They are defined by Natural England, the UK government's advisors on the natural environment.
The River Burn is a river that flows wholly within North Yorkshire, England. The river starts as several small streams on Masham Moor and drains Colsterdale flowing eastwards before emptying into the River Ure just south of Masham. Conservation work on removinga weir and introducing fish to the river in 2016 has meant that salmon have been recorded spawning in the river for the first time in over 100 years.
