High Stile
From Wikipedia, the free encyclopedia
| High Stile | |
|---|---|
 High Stile from Red Pike | |
| Highest point | |
| Elevation | 807 m (2,648 ft) |
| Prominence | 362 m (1,188 ft) |
| Parent peak | Great Gable |
| Listing | Marilyn, Hewitt, Wainwright, Nuttall |
| Coordinates | 54°31′18″N 3°17′02″W / 54.52167°N 3.28381°W |
| Geography | |
  High Stile Location in the Lake District National Park | |
| Location | Cumbria, England |
| Parent range | Lake District, Western Fells |
| OS grid | NY170148 |
| Topo map | OS Landranger 89, Explorer OL4 |
High Stile is a mountain in the western part of the Lake District in North West England. It is the eleventh-highest English Marilyn, standing 807 metres (2,648 ft) high, and has a relative height of 362 metres (1,188 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.
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.[1] 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,[2] 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.
High Stile above
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 15 ft (4.6 m) deep, and is well stocked with trout.[3] 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,[1][2] 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 2,000 ft (610 m), 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.
Geology
The summit area is formed of the siltstone, sandstone, conglomerate, tuff, lapilli tuff and andesite sills of the Eagle Crag Member. The northern slopes display the underlying olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone of the Buttermere Formation. In the direction of Red Pike are intrusions of the granophyric granite.[4]
In Burtness Comb, a prominent bank of debris runs along the outer flank of the upper cirque, then turns down into the lower cirque, ending in a block strew at the intake wall. It marks the course of a rock avalanche which fell from Grey Crag on the summit rim of High Stile, and was channeled along the foot of the glacier some 11,000 years ago.[5] It is unique in the Lake District.
There are the remains of a small copper-mine near the shore of Buttermere. This was worked from 1569 to 1570 and again in the 1820s.[6]
