About Glaramara
Glaramara is a fell in the English Lake District in Cumbria. It is a substantial fell that is part of a long ridge that stretches for over six kilometres from Stonethwaite in Borrowdale up to the important mountain pass of Esk Hause. The summit of Glaramara at 783 m (2, 569 ft) is the central point of this ridge, which separates the valleys of Langstrath and Grains Gill. However, the ridge has two additional fells, numerous subsidiary tops and several small tarns making its traverse an appealing and challenging walk. NameThe fell’s unusual and pleasant-sounding name, previously only applied to the summit rocks, has now been accepted as the name for the whole fell. Like many fells of the district the name comes from a series of Old Norse words which in this case is translated as “Hill with the mountain hut by a chasm”. TopographyGlaramara’s most striking feature is Combe Gill on its northern slopes, a classic example of a hanging valley that was formed by glacial erosion during the last ice age. The gill is full of crags and according to Alfred Wainwright contains the only natural cave in the Lake District, these are the Dove Nest Caves, a rock slip from Dove Nest Crags has partly covered the cave which has three entrances. On its east and west flanks the fell falls away steeply with rocky slopes and scree to the valleys. To the south the ridge continues from the summit of Glaramara for two kilometres over various tops (some of which are Hewitts or Nuttalls) with little loss of height to the adjoining fell of Allan Crags before descending to Esk Hause.
Glaramara Description
Glaramara is a fell in the English Lake District in Cumbria. It is a substantial fell that is part of a long ridge that stretches for over six kilometres from Stonethwaite in Borrowdale up to the important mountain pass of Esk Hause. The summit of Glaramara at 783 m (2, 569 ft) is the central point of this ridge, which separates the valleys of Langstrath and Grains Gill. However, the ridge has two additional fells, numerous subsidiary tops and several small tarns making its traverse an appealing and challenging walk. NameThe fell’s unusual and pleasant-sounding name, previously only applied to the summit rocks, has now been accepted as the name for the whole fell. Like many fells of the district the name comes from a series of Old Norse words which in this case is translated as “Hill with the mountain hut by a chasm”. TopographyGlaramara’s most striking feature is Combe Gill on its northern slopes, a classic example of a hanging valley that was formed by glacial erosion during the last ice age. The gill is full of crags and according to Alfred Wainwright contains the only natural cave in the Lake District, these are the Dove Nest Caves, a rock slip from Dove Nest Crags has partly covered the cave which has three entrances. On its east and west flanks the fell falls away steeply with rocky slopes and scree to the valleys. To the south the ridge continues from the summit of Glaramara for two kilometres over various tops (some of which are Hewitts or Nuttalls) with little loss of height to the adjoining fell of Allan Crags before descending to Esk Hause.