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England: Sovereign state: United Kingdom: Postcode district ... Little Langdale is a valley in the Lake District, England, containing Little Langdale Tarn and a ...
Lingmoor Fell is a fell in the English Lake District, situated eight kilometres (five miles) west of Ambleside.The fell reaches a height of 469 m (1,540 ft) and divides the valleys of Great Langdale and Little 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 .
Other valleys such as Little Langdale, Eskdale and Dunnerdale are served by minor roads. The last of these is connected with the first two by the Wrynose and Hardknott passes respectively; both of these passes are known for their steep gradients and are together one of the most popular climbs in the United Kingdom for cycling enthusiasts. [20]
The bridge dates back to the 17th century, and became a listed building in 1967. [1] Built of slate, it consists of a 15-foot (4.6 m) segmental arch and a flatter span built of slabs, and incorporates a natural boulder in midstream.
The following is a list of Sites of Special Scientific Interest (SSSIs) in Cumbria, England, United Kingdom. In England the body responsible for designating SSSIs is Natural England, which chooses a site because of its fauna, flora, geological or physiographical features. [1] As of July 2012 there were 278 SSSIs within Cumbria.
Great Carrs, in common with many fells, has easy slopes to the west and crags to the east. These crags- falling directly from the summit- form the head of Greenburn. A steep sided, rather marshy valley, Greenburn is a part of the Little Langdale system, its waters joining the River Brathay at Little Langdale Tarn.
Ting Mound. The Ting Mound or Thing Moot at Fellfoot Farm, Little Langdale, Cumbria, England is an Ancient Monument (a 'nationally important' archaeological site). It is a natural mound which has been deliberately terraced, possibly in the tenth century, although it has not been dated archaeologically.
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