Blea Rigg
| Blea Rigg | |
|---|---|
 Blea Rigg
Location in Lake District, UK
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| Highest point | |
| Elevation | 541 m (1,775 ft) |
| Prominence | c. 20 m |
| Parent peak | Harrison Stickle |
| Listing | Wainwright |
| Coordinates | 54°27′39″N 3°04′42″W / 54.46076°N 3.07827°WCoordinates: 54°27′39″N 3°04′42″W / 54.46076°N 3.07827°W |
| Geography | |
| Location | Cumbria, England |
| Parent range | Lake District, Central Fells |
| OS grid | NY302078 |
| Topo map | OS Explorer OL7 |
Blea Rigg is a fell in the English Lake District, lying between the valleys of Easedale and Great Langdale. One of the Central Fells, it is a broad plateau with a succession of rocky tops. Many routes of ascent are possible, beginning either from Grasmere or Great Langdale, though the paths are often poorly marked and hard to follow.
The main spine of the Central Fells runs north to south from the Vale of Keswick to its greatest elevation at High Raise. A long ridge runs out eastward from here, so that the range as a whole resembles the letter 'L'. This eastward ridge begins as Blea Rigg and then continues over Silver How and Loughrigg Fell, before petering out near the head of Windermere.
Blea Rigg is a broad plateau, around a mile wide and two miles long, climbing roughly east to west. It connects via a narrower section between Stickle and Codale Tarns to Sergeant Man and ultimately High Raise in the west. Stickle Tarn is the larger of the two waterbodies, a 50 ft deep corrie tarn with the level increased by a stone faced dam. It is used to supply water to the residents of Great Langdale. Codale Tarn is a shallow pool set amid rough ground, a little to the north east.
Blea Rigg has a number of named tops in addition to the summit. Travelling west to east these are Great Castle How (1,640 ft), Little Castle How (1,581 ft), Swinescar Pike (1,348 ft) and Lang How (1,358 ft) Silver How could also be considered part of Blea Rigg, were it not for Wainwright's decision to accord it a separate chapter in his Pictorial Guide to the Lakeland Fells.
Drainage from the southern side of the fell is via a number of feeders to Stickle Gill and Great Langdale Beck. Among the tributaries is White Gill, its ravine being an interesting route of ascent. Water from the northern flanks reaches Grasmere via Easedale Beck and its feeders. Crags look down over Easedale Tarn and Blindtarn Moss to the north, while further rough ground looms over the Great Langdale road.
The summit of the fell is formed of the Pavey Ark Member, pebbly sandstone and breccia from the Borrowdale Volcanic series. There is no history of mining within the area of the fell.
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Wikipedia