5069 x 3375 px | 42,9 x 28,6 cm | 16,9 x 11,3 inches | 300dpi
Altre informazioni:
horizontal photo of a man in appropriate clothing walks along a stony path alongside a rocky summit on a mountain in low misty cloud in the English lake District in England Great Britain UK Europe. St Sunday Crag is a fell in the English Lake District, part of the Fairfield group in the Eastern Fells. It is a prominent feature in the Patterdale skyline, with a distinctive rounded shape. Indeed it figures so finely in views from the upper reach of the lake that it is sometimes referred to as 'the Ullswater Fell'. [1] St Sunday Crag is the high point on the north eastern ridge of Fairfield, which runs for two miles before descending to the valley floor behind Patterdale village. From the flat Fairfield summit a rough slope descends over the subsidiary top of Cofa Pike to the col at Deepdale Hause (c2, 200 ft). This is a narrow point on the ridge, deeply scarred by pedestrian traffic. The ground now rises again to St Sunday Crag, soaring above the dales on either side. Beyond the summit there is a swift drop to the lower plateau of Birks and beyond this is the further satellite of Arnison Crag. The top of St Sunday Crag is triangular in plan with a third ridge running off due east. This crosses a depression (The Cape) before the lower top of Gavel Pike (2, 572 ft) is reached. From below this is a shapely pyramid worthy of the "pike" designation, although its subsidiarity is all to plain from above. Below Gavel Pike is the further top of Lord's Seat before the short east ridge falls away over rough ground to Deepdale. It is the north western face above Grisedale that is St Sunday Crag's chief glory. The long graceful curve of the top is set above a wall of crag half a mile long, the whole face being neatly symetrical. A series of vertical gullys slice through the crags, which together with the intervening ridges provide sport for scramblers and climbers. The crags peter out at about 1, 800 ft, to be replaced by a steep scree slope falling to the valley floor, a further