River Ure in the context of Wensleydale

The River Ouse (/uːz/ 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.

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.

Ripon (/ˈrɪpən/) is a cathedral city and civil parish in North Yorkshire, England, at the confluence of two tributaries of the River Ure, the Laver and Skell, noted for Ripon Cathedral, which is architecturally significant, as well as the Ripon Racecourse and other features such as its market.

The city was originally known as Inhrypum. Bede records that Alhfrith, king of the Southern Northumbrian kingdom of Deira, gave land at Ripon to Eata of Hexham to build a monastery and the abbot transferred some of his monks there, including a young Saint Cuthbert who was guest-master at Ripon abbey. Both Bede in his Life of Cuthbert and Eddius Stephanus in his Life of Wilfred state that when Eata was subsequently driven out by Alhfrith, the abbey was given to Saint Wilfrid who replaced the timber church with a stone built church. This was during the time of the Anglian kingdom of Northumbria, a period during which it enjoyed prominence in religious importance in Great Britain. It was for a period under Viking control, and later suffered under the Normans. After a brief period of building projects under the Plantagenets, the city emerged with a prominent wool and cloth industry. Ripon became well known for its production of spurs during the 16th and 17th centuries, but would later remain largely unaffected by the Industrial Revolution.

Boroughbridge (/ˈbʌrəbrɪdʒ/ BURR-ə-brij) is a town and civil parish in North Yorkshire, England. Historically part of the West Riding of Yorkshire, it is 16 miles (26 km) north-west of York. Until a bypass was built the town lay on the main A1 road from London to Edinburgh, which crosses the River Ure here.

The civil parish includes the villages of Aldborough and Minskip.

The Yorkshire Dales are a series of valleys, or dales, in the Pennines, an upland range in England. They are mostly located in the ceremonial county of North Yorkshire, but extend into Cumbria and Lancashire; they are entirely within the historic boundaries of Yorkshire. The majority of the dales are within the Yorkshire Dales National Park, created in 1954. The exception is the area around Nidderdale, which forms the separate Nidderdale Area of Outstanding Natural Beauty.

The landscape of the Yorkshire Dales consists of sheltered glacial valleys separated by exposed moorland. The predominant rock is Carboniferous Limestone, which is particularly visible in the south-west in features such as Malham Cove. It is overlain in many areas by the Yoredale Series of alternating weak shales and hard limestones and sandstones, which give the dales their characteristic 'stepped' appearance. Most of the dales contain rivers, and the area contains seven primary catchments: the Swale, Ure, Wharfe, Aire, Nidd, Ribble, and Lune. There are several notable cave systems in the area, including part of the longest system in the United Kingdom, the Three Counties.

The River Swale in Yorkshire, England, is a major tributary of the River Ure, which becomes the River Ouse, that empties into the North Sea via the Humber Estuary. The river gives its name to Swaledale, the valley through which it flows.

The river and its valley are home to many types of flora and fauna typical to the Yorkshire Dales. Like similar rivers in the region, the river carves through several types of rock and has features typical of both river and glacial erosion. The River Swale has been a contributory factor in the settlements that have been recorded throughout its history. It has provided water to aid in the raising of crops and livestock, but also in the various mining activities that have occurred since Roman times and before.

The River Laver is a tributary of the River Skell, itself a tributary of the River Ure in North Yorkshire, England. The name is of Brittonic origin, from labaro, meaning "talkative", i.e. a babbling brook. The Afon Llafar in Wales shares the same name.

The Laver is noted as a fly fishing river, especially for brown trout and grayling.

The River Skell is a 12-mile-long (19 km) tributary of the River Ure in North Yorkshire, England.

Its source is in boggy ground on moorland 2 miles (3 km) north of Pateley Bridge. For its first 2 miles (3 km) the river is known as Skell Beck. Descending from the moor the river enters Skell Gill, a narrow wooded valley. The river valley gradually broadens, but remains well wooded, passing the village of Grantley and the 17th century Grantley Hall.

The Nidderdale National Landscape is an Area of Outstanding Natural Beauty in North Yorkshire, England, bordering the Yorkshire Dales National Park to the east and south. It comprises most of Nidderdale itself, part of lower Wharfedale, the Washburn valley and part of lower Wensleydale, including Jervaulx Abbey and the side valleys west of the River Ure. It covers a total area of 233 square miles (600 km). The highest point in the Nidderdale AONB is Great Whernside, 704 metres (2,310 ft) above sea level, on the border with the Yorkshire Dales National Park.

The area is said to contain "remains from over 6,000 years of human activity"; there is evidence of "almost continuous settlement over this time with the exception of the Roman period for which evidence is scanty".