Raven Crag | |
---|---|
Highest point | |
Elevation | 461 m (1,512 ft) |
Prominence | c. 45 m |
Parent peak | High Seat |
Listing | Wainwright |
Coordinates | 54°33′35″N3°04′40″W / 54.55963°N 3.07778°W Coordinates: 54°33′35″N3°04′40″W / 54.55963°N 3.07778°W |
Geography | |
Location | Cumbria, England |
Parent range | Lake District, Central Fells |
OS grid | NY304188 |
Topo map | OS Explorer OL4 |
Raven Crag is a fell in the English Lake District that overlooks Thirlmere reservoir. It has subsidiary summits The Benn and Castle Crag.
The fell is the high point on a 2-mile-long spur running up the western shore of Thirlmere, branching off from the main ridge of the central fells just east of High Tove. Subsidiary tops include The Benn (also known as Benn Man, 1,463 feet (446 m)) and Castle Crag (1,381 feet (421 m)), the site of an Iron Age settlement. The ridge has been extensively planted with conifers as part of the Thirlmere Forest, the face of Raven Crag appearing as a lone oasis of naked rock amid the trees.
Raven Crag is bordered to the west by the long valley of Shoulthwaite Gill, which is a tributary of the River Greta. To the north the ridge drops to a depression, crossed by the Keswick–Ambleside road, before climbing again onto High Rigg.
Raven Crag and the Benn exhibit rock of the Birker Fell Formation, composed of plagioclase-phyric andesite lavas with subordinate sills. Between the two is an area of garnet bearing porphyritic andesite. Castle Crag Fort overlays volcaniclastic sandstone. [1]
The main face of the fell stands over Thirlmere Dam, and appears from there as a sheer 500 feet (150 m) crag, the higher fells behind being hidden by the ridge. Raven Crag is most commonly climbed from the dam, via a steep waymarked path through the forestry. This ends with made paths and some short sections of boardwalk. The ridge between Raven Crag and High Tove can also be gained from Armboth, or an ascent can be made from 'behind' via Shoulthwaite. This can include visits to The Benn and the earth ramparts of Castle Crag. [2] [3]
The highest point is an outcrop of rock with a small cairn, partially screened by conifers. The view from the summit is limited by the trees, but the eastward panorama opens up from the brink of the crag itself and there is an aerial view of the Thirlmere dam. The reservoir is also seen end on to the south. The Benn and Castle Crag provide a close-up view of Raven Crag from the north. [2] [3]
Pillar is a mountain in the western part of the English Lake District. Situated between the valleys of Ennerdale to the north and Wasdale to the south, it is the highest point of the Pillar group. At 892 metres (2,927 feet) it is the eighth-highest mountain in the Lake District. The fell takes its name from Pillar Rock, a prominent feature on the Ennerdale side, regarded as the birthplace of rock climbing in the district.
Great Gable is a mountain in the Lake District, United Kingdom. It is named after its appearance as a pyramid from Wasdale, though it is dome-shaped from most other directions. It is one of the most popular of the Lakeland fells, and there are many different routes to the summit. Great Gable is linked by the high pass of Windy Gap to its smaller sister hill, Green Gable, and by the lower pass of Beck Head to its western neighbour, Kirk Fell.
Harter Fell is a fell in the western part of the English Lake District, located between the Eskdale and Duddon valleys. Its height is 649 m (2128 ft). There are several walking routes to the summit.
Great Dodd is a mountain or fell in the English Lake District. It stands on the main ridge of the Helvellyn range, a line of mountains which runs in a north-south direction between the lakes of Thirlmere and Ullswater in the east of the Lake District. Great Dodd, with a height of 857 m is the highest of the fells in this range to the north of Sticks Pass.
Raise is a fell in the English Lake District. It stands on the main spine of the Helvellyn range in the Eastern Fells, between Thirlmere and Ullswater.
High Seat is a fell in the centre of the English Lake District. Despite being below 2,000 ft it is the highest point for about 5 miles in any direction; a consequence of the curious fact that the centre of the district is lower than the surrounding parts.
White Side is a fell in the English Lake District. It is situated to the east of Thirlmere and to the west of Glenridding valley. This places White Side in the Helvellyn range of the Eastern Fells, with Raise to the north and Helvellyn Lower Man to the south, both of which are of greater height.
Stybarrow Dodd is a mountain or fell in the English Lake District. It stands immediately north of Sticks Pass on the main ridge of the Helvellyn range in the Eastern Fells, which is situated between the lakes of Thirlmere and the Ullswater.
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 (1,187 ft).
High Rigg is a small fell located in the English Lake District, approximately three miles southeast of the town of Keswick. It occupies an unusual position, surrounded on all sides by higher fells but not connected by any obvious ridge. This separation from its fellows ensures that it is a Marilyn.
Bleaberry Fell is a fell in the Lake District in Cumbria, England, with a height of 590 metres (1,936 feet). It stands on the main watershed between Borrowdale and Thirlmere and can be climbed from either flank. Walla Crag is a subsidiary top of Bleaberry Fell.
Ullscarf is a fell in the English Lake District close to the geographical centre of the Cumbrian hills. It forms part of the watershed between the Derwentwater and Thirlmere catchments, a ridge running broadly north-south.
High Tove is a fell in the English Lake District, close to the geographical centre of the Cumbrian hills. It forms part of the watershed between the Derwentwater and Thirlmere catchments, a ridge running broadly north-south.
Armboth Fell is a fell in the English Lake District, regarded by Alfred Wainwright as the centre of Lakeland. It is named for the former settlement of Armboth. The fell is a domed plateau, three-quarters of a mile across, jutting out to the east of the Derwentwater-Thirlmere watershed, in the Borough of Allerdale. The fell is wet underfoot, with large areas clad in heather. The eastern slopes above Thirlmere have been planted with conifers.
Steel Fell is a fell in the English Lake District, lying between Thirlmere and Grasmere. It is triangular in plan, the ridges running north, west and south east. Steel Fell rises to the west of the Dunmail Pass road and can be climbed from the summit, or from Grasmere and Wythburn.
Tarn Crag is a fell in the Central Fells of the English Lake District. Strictly the name refers only to the rock face looking down upon Easedale Tarn, but Alfred Wainwright applied it to the entire ridge lying between the Easedale and Far Easedale valleys in his Pictorial Guide to the Lakeland Fells
Calf Crag is a fell in the English Lake District, on the eastern side of the High Raise massif.
Lingmoor Fell is a fell in the English Lake District, situated eight kilometres west of Ambleside. The fell reaches a height of 469 m (1,540 ft) and divides the valleys of Great Langdale and Little Langdale. The fell's name originates from the Old Norse word lyng meaning “heather covered”. The actual summit of the fell is named as Brown How on Ordnance Survey maps.
Watson's Dodd is a fell in the English Lake District, a minor rise on the main ridge of the Helvellyn range in the Eastern Fells, but a prominent shoulder on the west side of that range.
The Central Fells are a group of hills in the English Lake District. Reaching their highest point at High Raise, they occupy a broad area to the east of Borrowdale. The Central Fells are generally lower than the surrounding hills, the Lake District's dome-like structure having a slight dip in the middle. The range extends from the boggy ridge between Derwentwater and Thirlmere in the north, to the rock peaks of the Langdale Pikes in the south.