The North Pennines are the northernmost section of the Pennines, a range of hills which run north–south through northern England. They run along the border between County Durham and Northumberland in the east and Cumbria in the west, and are bounded to the north by the Tyne Valley and to the south by the Stainmore Gap. Much of the region is moorland, and it contains significant industrial archaeology.
The North Pennines have been designated a national landscape and a UNESCO Global Geopark.
The River Tees (/tiːz/), in England, rises on the eastern slope of Cross Fell in the North Pennines and flows eastwards for 85 miles (137 km) to reach the North Sea in the North East of England. The modern-day history of the river has been tied with the industries on Teesside in its lower reaches, where it has provided the means of import and export of goods to and from the North East England. The need for water further downstream also meant that reservoirs were built in the extreme upper reaches, such as Cow Green.
The Pennines (/ˈpɛnaɪnz/), also known as the Pennine Chain or Pennine Hills, are an upland range mainly located in Northern England. Sometimes described as the "backbone of England" because of its length and position, the range runs from Derbyshire and Staffordshire in the north of the Midlands to Northumberland in North East England. From the Tyne Gap in the north, the range extends south through the North Pennines, Yorkshire Dales, South Pennines, and Peak District to end near the valley of the River Trent. The Border Moors and Cheviot Hills, which lie beyond the Tyne Gap, are included in some definitions of the range.
The range is divided into two by the Aire Gap, a wide pass formed by the valleys of the rivers Aire and Ribble. There are several spurs off the main Pennine range east into Greater Manchester and Lancashire, comprising the Rossendale Fells, West Pennine Moors, and Bowland Fells. The Howgill Fells and Orton Fells in Cumbria are also sometimes considered to be Pennine spurs. The Pennines are an important water catchment area, with numerous reservoirs in the head streams of the river valleys.
Cumberland (/ˈkʌmbərlənd/ KUM-bər-lənd) is an area of North West England which was historically a county. The county was bordered by Northumberland to the north-east, County Durham to the east, Westmorland to the south-east, Lancashire to the south, and the Scottish counties of Dumfriesshire and Roxburghshire to the north. The county included the city of Carlisle, part of the Lake District and North Pennines, and the Solway Firth coastline.
Cumberland had an administrative function from the 12th century until 1974, when it was subsumed into Cumbria with Westmorland as well as parts of Yorkshire and Lancashire. It gives its name to the unitary authority area of Cumberland, which has similar boundaries but excludes Penrith.
The Settle–Carlisle line (also known as the Settle and Carlisle (S&C)) is a 73-mile-long (117 km) main railway line in northern England. The route, which crosses the remote, scenic regions of the Yorkshire Dales and the North Pennines, runs between Settle Junction, on the Leeds–Morecambe line, and Carlisle, near the English-Scottish borders. The historic line was constructed in the 1870s and has several notable tunnels and viaducts such as the imposing Ribblehead.
The line is managed by Network Rail. All passenger services are operated by Northern apart from temporary diverted services (due to closures of the West Coast Main Line) and are part of the National Rail network. Stations serve towns such as Settle in North Yorkshire, Appleby-in-Westmorland in Cumbria and small rural communities along its route.