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High Stile : ウィキペディア英語版
High Stile

High Stile is a mountain in the western part of the Lake District in northwest England. It is the eleventh highest English Marilyn, standing 807 metres (2,648 ft) high, and has a relative height of 362 metres (1,187 ft).
It is the highest in the range of fells extending north west from Great Gable towards Loweswater, and together with its satellites, Red Pike and High Crag, forms a trio of fells overlooking the lake and village of Buttermere. On this side are high crags, wild combes and a small tarn, Bleaberry Tarn. High Stile is most easily ascended as part of a traverse of the three fells.
==Topography==
The Western Fells occupy a triangular sector of the Lake District, bordered by the River Cocker to the north east and Wasdale to the south east. Westwards the hills diminish toward the coastal plain of Cumberland. At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley.〔Alfred Wainwright: ''A Pictorial Guide to the Lakeland Fells, Volume 7 The Western Fells'': Westmorland Gazette (1966): ISBN 0-7112-2460-9〕 The highest section of the northern branch is formed by the trio of Buttermere fells, High Crag, High Stile and Red Pike.
The Buttermere Fells, also known as Buttermere Edge,〔Bill Birkett:''Complete Lakeland Fells'': Collins Willow (1994): ISBN 0-00-713629-3〕 form the watershed between Buttermere and Upper Ennerdale. The Ennerdale flanks are steep and rough with areas of crag, the lower slopes being planted with a ribbon of conifers. Across the narrow ridge-top to the north are deep corries and dark walls of crag, glowering down over the lake. The ridge continues south east to Haystacks and the Great Gable group. Beyond Red Pike to the west are Starling Dodd, Great Borne and the Loweswater Fells.
All three Buttermere Fells throw out a short spur towards the lake with deep combs hollowed out between them. North west of High Stile is Bleaberry Comb, backed by the wall of Chapel Crags. Nestled deep within is Bleaberry Tarn, a pool which is on continual shadow from November to March. Despite the steep contours of the rock walls above, the tarn is only about deep, and is well stocked with trout.〔Blair, Don: ''Exploring Lakeland Tarns'': Lakeland Manor Press (2003): ISBN 0-9543904-1-5〕 Bleaberry Tarn is drained into Buttermere by Sourmilk Gill, reaching the lake mere yards from its outlet. A belt of trees has been planted along the shoreline. Birkness Comb,〔〔 also called Burtness Comb on Ordnance Survey maps, lies between the truncated and unnamed northern ridges of High Crag and High Stile. The lack of a retaining moraine means that this hollow has no tarn, Comb Beck running uninterrupted to the Lake. Grey Crag and Eagle Crag are the main faces on High Stile. These corries being scooped out of the northern face result in the connecting ridges between the three Buttermere Fells being fine and narrow.
The Ennerdale flanks have a tier of crag at around , The Knors and Raven Crag being the principal features. At the foot of the slopes are the massed conifers of the Ennerdale Forest, all contributing to the difficulty of access. There are no paths on the southern flank of High Stile.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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