St Sunday Crag: Difference between revisions
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'''St Sunday Crag''' is a fell in [[Westmorland]], in [[Lake District]]. It is part of the [[Fairfield (fell)|Fairfield]] group in the Eastern Fells and is a prominent feature in the [[Patterdale]] skyline, with its 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'.<ref name="richards">Richards, Mark: ''Near Eastern Fells'': Collins (2003): ISBN 0-00-711366-8</ref> | '''St Sunday Crag''' is a fell in [[Westmorland]], in the [[Lake District]]. It is part of the [[Fairfield (fell)|Fairfield]] group in the Eastern Fells and is a prominent feature in the [[Patterdale]] skyline, with its 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'.<ref name="richards">Richards, Mark: ''Near Eastern Fells'': Collins (2003): ISBN 0-00-711366-8</ref> | ||
==Geography== | ==Geography== | ||
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 at 2,200 feet. 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 (fell)|Birks]] and beyond this is the further satellite of [[Arnison Crag]]. | 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 at 2,200 feet. 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 (fell)|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 at 2,572 feet is reached. From below this is a shapely pyramid worthy of the "pike" designation, although its subsidiarity is all too plain from above. Below Gavel Pike is the further top of Lord's Seat before the short eastern ridge falls away over rough ground to Deepdale. | 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 at 2,572 feet is reached. From below this is a shapely pyramid worthy of the "pike" designation, although its subsidiarity is all too plain from above. Below Gavel Pike is the further top of Lord's Seat before the short eastern ridge falls away over rough ground to Deepdale. | ||
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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 symmetrical. 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 feet, to be replaced by a steep scree slope falling to the valley floor, a further 800 feet below. Fine views of this face can be had from [[Helvellyn]] and [[Birkhouse Moor]] across the valley. | 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 symmetrical. 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 feet, to be replaced by a steep scree slope falling to the valley floor, a further 800 feet below. Fine views of this face can be had from [[Helvellyn]] and [[Birkhouse Moor]] across the valley. | ||
To the south east of the fell is the valley of Deepdale, separating St Sunday Crag from [[Hart Crag]] and [[Hartsop above How]]. This face too is steep and rough, although without sustained outcropping of rock. Between Gavel Pike and Birks is Cold Cove, a hanging valley cut off by Deepdale. All of the becks from St Sunday Crag reach the head of Ullswater at Patterdale. | To the south-east of the fell is the valley of Deepdale, separating St Sunday Crag from [[Hart Crag]] and [[Hartsop above How]]. This face too is steep and rough, although without sustained outcropping of rock. Between Gavel Pike and Birks is Cold Cove, a hanging valley cut off by Deepdale. All of the becks from St Sunday Crag reach the head of Ullswater at Patterdale. | ||
==Geology== | ==Geology== | ||
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==Ascents== | ==Ascents== | ||
The main starting point for ascents is Patterdale, either by climbing or traversing Birks. Arnison Crag can also be thrown in for good measure and the | The main starting point for ascents is Patterdale, either by climbing or traversing Birks. Arnison Crag can also be thrown in for good measure and the north-east ridge gives fantastic rearward views of Ullswater. A further Patterdale alternative is the Elmhow zig-zag which climbs the Grisedale face just north of the crags. Lord's Seat and the east ridge can be climbed from Deepdale, starting from the car park at Bridgend. St Sunday Crag can also be ascended from the east by making first for Grisedale Tarn. This puts the summit into reach from Grasmere or Dunmail Raise. | ||
St Sunday Crag now finds itself on Alfred Wainwright's popular [[Coast to Coast Walk]], vastly increasing the traffic across the top. | St Sunday Crag now finds itself on Alfred Wainwright's popular [[Coast to Coast Walk]], vastly increasing the traffic across the top. | ||
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{{DEFAULTSORT:Saint Sunday Crag}} | {{DEFAULTSORT:Saint Sunday Crag}} | ||
{{Wainwrights|1}} | |||
Latest revision as of 16:12, 7 June 2017
| St Sunday Crag | |||
| Westmorland | |||
|---|---|---|---|
| |||
| Range: | Lake District Eastern Fells | ||
| Summit: | 2,759 feet NY369135 54°30’46"N, 2°58’34"W | ||
St Sunday Crag is a fell in Westmorland, in the Lake District. It is part of the Fairfield group in the Eastern Fells and is a prominent feature in the Patterdale skyline, with its 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]
Geography
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 at 2,200 feet. 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 at 2,572 feet is reached. From below this is a shapely pyramid worthy of the "pike" designation, although its subsidiarity is all too plain from above. Below Gavel Pike is the further top of Lord's Seat before the short eastern 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 symmetrical. 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 feet, to be replaced by a steep scree slope falling to the valley floor, a further 800 feet below. Fine views of this face can be had from Helvellyn and Birkhouse Moor across the valley.
To the south-east of the fell is the valley of Deepdale, separating St Sunday Crag from Hart Crag and Hartsop above How. This face too is steep and rough, although without sustained outcropping of rock. Between Gavel Pike and Birks is Cold Cove, a hanging valley cut off by Deepdale. All of the becks from St Sunday Crag reach the head of Ullswater at Patterdale.
Geology
Geologically the summit area is andesite, overlaying the St Sunday Crag Member, a 50m thick layer of rhyodactic lapilli-tuff which breaks the surface on the east ridge.[2]
Summit and view
Given the fine ridges to either side, the summit of St Sunday Crag is surprisingly level and green. Two cairns sit upon the highest area, where rocks protrude through the turf. A further cairn at the northern end of the summit area marks the prime viewpoint for Ullswater. A quartz cross, now hard to find amid the bilberry, lies above the crags marking the top of East Chockstone Gully.[1] The view takes much of the District, Striding Edge and the crags of Fairfield being particularly prominent.[3] Gavel Pike provides good views of the head of Deepdale.
Ascents
The main starting point for ascents is Patterdale, either by climbing or traversing Birks. Arnison Crag can also be thrown in for good measure and the north-east ridge gives fantastic rearward views of Ullswater. A further Patterdale alternative is the Elmhow zig-zag which climbs the Grisedale face just north of the crags. Lord's Seat and the east ridge can be climbed from Deepdale, starting from the car park at Bridgend. St Sunday Crag can also be ascended from the east by making first for Grisedale Tarn. This puts the summit into reach from Grasmere or Dunmail Raise.
St Sunday Crag now finds itself on Alfred Wainwright's popular Coast to Coast Walk, vastly increasing the traffic across the top.
Name
Saint Sunday is a local name for Saint Dominic, though it is not certain how this saint's name became attached to the fell.[1]
References
- ↑ 1.0 1.1 1.2 Richards, Mark: Near Eastern Fells: Collins (2003): ISBN 0-00-711366-8
- ↑ Woodhall, DG: Geology of the Keswick District- a brief explanation of the geological map. 1:50,000 Sheet 29: British Geological Survey (2000)
- ↑ Alfred Wainwright: A Pictorial Guide to the Lakeland Fells, Book 1: ISBN 0-7112-2454-4