Green Crag: Difference between revisions
No edit summary |
|||
(One intermediate revision by the same user not shown) | |||
Line 21: | Line 21: | ||
Green Crag is the highest of a series of rocky tops which stand out from the [[Birker Fell]] moorland. Running from north to south these outcrops present a fine serrated skyline when viewed from Eskdale. Birker Fell itself is roughly square and about two miles across, with Eskdale to the north and the [[River Duddon]] to the south. | Green Crag is the highest of a series of rocky tops which stand out from the [[Birker Fell]] moorland. Running from north to south these outcrops present a fine serrated skyline when viewed from Eskdale. Birker Fell itself is roughly square and about two miles across, with Eskdale to the north and the [[River Duddon]] to the south. | ||
Above the wooded valley of Eskdale there is a skirt of crags before the open moor is reached. Over this edge tumble the waterfalls of Stanley Force and Birker Force, the former easily reached by made paths from the road. The farmers of Eskdale once extracted peat from the plateau and the remains of graded paths and peat huts can still be found on the fellside.<ref name=richards/> On this flank the remains of Gate Gill iron mine can also be found. Haematite was won from a number of levels here in the 1880s.<ref name=adams>Adams, John: ''Mines of the Lake District Fells'': Dalesman (1995) ISBN 0-85206-931-6</ref> The Duddon flanks have shallower gradients, divided by dry stone walls into long strips of pasture land. This rough grazing supports a series of farms along the valley between [[Ulpha]] and [[Seathwaite]]. | Above the wooded valley of Eskdale there is a skirt of crags before the open moor is reached. Over this edge tumble the waterfalls of Stanley Force and Birker Force, the former easily reached by made paths from the road. The farmers of Eskdale once extracted peat from the plateau and the remains of graded paths and peat huts can still be found on the fellside.<ref name=richards/> On this flank the remains of Gate Gill iron mine can also be found. Haematite was won from a number of levels here in the 1880s.<ref name=adams>Adams, John: ''Mines of the Lake District Fells'': Dalesman (1995) ISBN 0-85206-931-6</ref> The Duddon flanks have shallower gradients, divided by dry stone walls into long strips of pasture land. This rough grazing supports a series of farms along the valley between [[Ulpha]] and [[Seathwaite, Lancashire]]. | ||
To the east of Green Crag is a marshy depression before the ground rises again to Harter Fell. The western boundary is formed by the [[Birker Fell]] Road, an unenclosed route from Ulpha to Eskdale Green with fine views of the [[Scafells]]. Summiting at 885 feet with hairpin climbs at either end, the road is frequently closed in winter by snow and ice. Beyond the road the moorland climbs via Seat How to the summit of Yoadcastle. From here it turns south, forming a more definite ridge on the long march to Black Combe. | To the east of Green Crag is a marshy depression before the ground rises again to Harter Fell. The western boundary is formed by the [[Birker Fell]] Road, an unenclosed route from Ulpha to Eskdale Green with fine views of the [[Scafells]]. Summiting at 885 feet with hairpin climbs at either end, the road is frequently closed in winter by snow and ice. Beyond the road the moorland climbs via Seat How to the summit of Yoadcastle. From here it turns south, forming a more definite ridge on the long march to Black Combe. | ||
The high point of the fell lies on a line of | The high point of the fell lies on a line of tors which break through the peat and fellgrass toward the east of the plateau. Travelling south from the Eskdale rim the tops are Kepple Crag, Great Whinscale, Crook Crag (1,538 feet), Green Crag and White How. The crest then turns west toward the Fell Road, passing over [[Great Worm Crag]] (1,400 feet), considered by some to be a separate fell.<ref name=richards/> | ||
To the west of the summit ridge is Low Birker Pool, a tarn which feeds [[Birker Force]]. This shallow tarn is contained by a low moraine and overlooked by Tarn Crag.<ref name=blair>Blair, Don: ''Exploring Lakeland Tarns'': Lakeland Manor Press (2003): ISBN 0-9543904-1-5</ref> | To the west of the summit ridge is Low Birker Pool, a tarn which feeds [[Birker Force]]. This shallow tarn is contained by a low moraine and overlooked by Tarn Crag.<ref name=blair>Blair, Don: ''Exploring Lakeland Tarns'': Lakeland Manor Press (2003): ISBN 0-9543904-1-5</ref> |
Latest revision as of 11:32, 28 February 2021
Green Crag | |||
Cumberland | |||
---|---|---|---|
Summit of Green Grag from the plateau to the north | |||
Range: | Lake District Southern Fells | ||
Summit: | 1,604 feet SD200982 54°22’25"N, 3°13’57"W |
Green Crag is a fell in the Lake District's Southern Fells: it is in Cumberland, between Eskdale and the Duddon valley.
Landscape
The headwaters of Eskdale and the Duddon are separated by a ridge falling south west from the summit of Crinkle Crags. This line of high ground continues over many twists and turns for 15 miles, finally meeting the sea on the slopes of Black Combe. From Crinkle Crags the first fells on this ridge are Hard Knott, Harter Fell and Green Crag.
Alfred Wainwright considered the remainder of the range unworthy of inclusion in his influential Pictorial Guide to the Lakeland Fells, stating that "south and west from Green Crag the scenery quickly deteriorates. This summit has therefore been taken as the boundary of fellwalking country." Later guidebook writers have been more gereous, adding Great Worm Crag, Yoadcastle, Whitfell, Buck Barrow, Black Combe and the low hills around Devoke Water to their hill lists.[1][2] Wainwright himself later relented and included these lesser hills in a supplementary volume, The Outlying Fells of Lakeland.
Green Crag is the highest of a series of rocky tops which stand out from the Birker Fell moorland. Running from north to south these outcrops present a fine serrated skyline when viewed from Eskdale. Birker Fell itself is roughly square and about two miles across, with Eskdale to the north and the River Duddon to the south.
Above the wooded valley of Eskdale there is a skirt of crags before the open moor is reached. Over this edge tumble the waterfalls of Stanley Force and Birker Force, the former easily reached by made paths from the road. The farmers of Eskdale once extracted peat from the plateau and the remains of graded paths and peat huts can still be found on the fellside.[1] On this flank the remains of Gate Gill iron mine can also be found. Haematite was won from a number of levels here in the 1880s.[3] The Duddon flanks have shallower gradients, divided by dry stone walls into long strips of pasture land. This rough grazing supports a series of farms along the valley between Ulpha and Seathwaite, Lancashire.
To the east of Green Crag is a marshy depression before the ground rises again to Harter Fell. The western boundary is formed by the Birker Fell Road, an unenclosed route from Ulpha to Eskdale Green with fine views of the Scafells. Summiting at 885 feet with hairpin climbs at either end, the road is frequently closed in winter by snow and ice. Beyond the road the moorland climbs via Seat How to the summit of Yoadcastle. From here it turns south, forming a more definite ridge on the long march to Black Combe.
The high point of the fell lies on a line of tors which break through the peat and fellgrass toward the east of the plateau. Travelling south from the Eskdale rim the tops are Kepple Crag, Great Whinscale, Crook Crag (1,538 feet), Green Crag and White How. The crest then turns west toward the Fell Road, passing over Great Worm Crag (1,400 feet), considered by some to be a separate fell.[1]
To the west of the summit ridge is Low Birker Pool, a tarn which feeds Birker Force. This shallow tarn is contained by a low moraine and overlooked by Tarn Crag.[4]
Geology
The summit knoll is formed by plagioclase-phyric andesite lavas of the Birker Fell Formation of the Borrowdale Volcanic Group.[5]
Summit
The summit of Green Crag is composed of naked rock and the ordinary walker will only find access from the north or west, mild scrambling being required.[6] The view from the small cairn on the summit gives a fine prospect of the southern fells, together with a sight of the sea due south.[1][6]
Ascents
Green Crag can be climbed from the Birker Fell Road, where there are some suitable off-road spaces for parking. From Eskdale the best access is via the sled gate (which is to say a path used for dragging peat on sleds) which climbs near Birker Force. The plateau can also be reached in the vicinity of Kepple Crag. From the Duddon there are waymarked paths through the conifer plantations, beginning at the various Forestry car-parks.[1]
References
- ↑ 1.0 1.1 1.2 1.3 1.4 Richards, Mark: Southern Fells: Collins (2003): ISBN 0-00-711367-6
- ↑ Birkett, Bill: Complete Lakeland Fells: Collins Willow (1994): ISBN 0-00-218406-0
- ↑ Adams, John: Mines of the Lake District Fells: Dalesman (1995) ISBN 0-85206-931-6
- ↑ Blair, Don: Exploring Lakeland Tarns: Lakeland Manor Press (2003): ISBN 0-9543904-1-5
- ↑ British Geological Survey: 1:50,000 series maps, England & Wales Sheet 38: BGS (1998)
- ↑ 6.0 6.1 Wainwright, Alfred: A Pictorial Guide to the Lakeland Fells, Book Four — The Southern Fells (1960)