The Howgill Fells are uplands in Northern England between the Lake District and the Yorkshire Dales, lying roughly within a triangle formed by the town of Sedbergh and the villages of Ravenstonedale and Tebay. The name Howgill derives from the Old Norse word haugr meaning a hill or barrow, plus gil meaning a narrow valley.
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👉 Howgill Fells in the context of Great Langdale
Great Langdale is a valley in the Lake District National Park in North West England, the epithet "Great" distinguishing it from the neighbouring valley of Little Langdale. Langdale is also the name of a valley in the Howgill Fells, elsewhere in Cumbria.
It is a popular location for hikers, climbers, fell-runners and other outdoor enthusiasts who are attracted by the many fells ringing the head of the valley. Among the best-known features of Great Langdale are the Langdale Pikes, a group of peaks on the northern side of the dale. England's highest mountain, Scafell Pike, can be climbed by a route from Langdale. Langdale has views of, in particular, Dungeon Ghyll Force waterfall, Harrison Stickle and Pike of Stickle.
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Howgill Fells in the context of Pennines
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.
Howgill Fells in the context of Yorkshire Dales National Park
The Yorkshire Dales National Park is a 2,178 km (841 sq mi) national park in England which covers most of the Yorkshire Dales, the Howgill Fells, and the Orton Fells. The Nidderdale area of the Yorkshire Dales is not within the national park, and has instead been designated a national landscape. Most of the park is within North Yorkshire, with a sizeable area in Cumbria and a small part in Lancashire. The park was designated in 1954, and extended in 2016. More than 95% of the land in the park is privately owned; there are over 1,000 farms in this area.
In 2020, the national park was named an International Dark Sky Reserve. This means that the area has "low levels of light pollution with good conditions for astronomy".
Howgill Fells in the context of Orton Fells
The Orton Fells is an upland area in Northern England, mostly consisting of limestone hills, plateaus and moorlands. Historically in Westmorland, the area lies within the modern county of Cumbria and is bounded by the Lake District to the west, the Eden Valley to the north and east, and the Yorkshire Dales and Howgill Fells to the south. The area mostly falls within the boundaries of the Yorkshire Dales National Park while a small part of the western fells is in the Lake District National Park. The fells are one of 159 National Character Areas defined by Natural England.
Most settlements are in the lower land of the central upland region and the area is bounded by the villages of Orton, Great Asby, Little Asby, Crosby Ravensworth and Crosby Garret. Other settlements in the area include Ravenstonedale, Soulby, Maulds Meaburn, King's Meaburn, Morland, and Cliburn, and many of the settlements have conservation area status. Abrasion by glaciers and natural weathering of the limestone has created deep fissures, breaking the pavement into blocks, most of which was damaged by mining over the centuries. The Great Asby Scar, near Great Asby, and Orton Scars, near Orton, are two remaining examples in Britain.