Bleaberry Fell














































Bleaberry Fell

Bleaberry Fell from Hause Gate.jpg
Bleaberry Fell seen from Hause Gate on the
opposite side of Derwent Water

Highest point
Elevation 590 m (1,940 ft)
Prominence 40 m (130 ft)
Parent peak High Seat
Listing Wainwright
Coordinates
54°33′56″N 3°06′26″W / 54.56565°N 3.10733°W / 54.56565; -3.10733Coordinates: 54°33′56″N 3°06′26″W / 54.56565°N 3.10733°W / 54.56565; -3.10733 
Geography



Bleaberry Fell is located in Lake District

Bleaberry Fell

Bleaberry Fell



Location in Lake District, UK


Location
Cumbria, England
Parent range
Lake District, Central Fells
OS grid NY285195
Topo map
OS Explorer OL4

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.




Contents






  • 1 Topography


  • 2 Ascents


  • 3 Geology


  • 4 Summit


  • 5 References





Topography


Situated in the central area of the national park, four kilometres (2½ miles) south of Keswick, Bleaberry Fell is the northernmost top on the ridge that separates the valleys containing the lakes of Derwent Water (Borrowdale) and Thirlmere. This ridge, which also contains the fells of High Seat and High Tove, is notoriously boggy underfoot, but Bleaberry Fell is mostly dry and the heather-covered summit gives an excellent all-round vista. To the east the fell has the rock faces of Iron Crag and Goat Crags as it falls away towards the Thirlmere valley.



Ascents


The fell is usually climbed from the car park in Great Wood in Borrowdale, firstly ascending Walla Crag via Cat Gill and then continuing south-easterly for two kilometres (1¼ miles) to Bleaberry Fell which is clearly in view. The fell can also be climbed from Keswick, an 11-kilometre (7-mile) round trip, again going by Walla Crag. Walla Crag is in fact part of Bleaberry Fell, being the outlying north western crags, but is given the status of a separate fell by Lake District writers due to its excellent views and popularity.


Another possible starting point is the hamlet of Dale Bottom on the main Keswick to Ambleside road. It is possible to continue from Bleaberry Fell southerly along the ridge to take in the other Wainwright fells of High Seat and High Tove following a line of old fenceposts. This ridge is very boggy.[1][2]



Geology


The summit of the fell is representative of the Birker Fell Formation. This is composed of plagioclase-phyric andesite lavas and subordinate sills. To the south en route to High Seat are garnet-bearing porphyric andesite. Much of the northern section is overlain by peat and till.[3]



Summit


The top is heather-clad and carries a number of cairns. Bleaberry Fell's central position is rewarded by a fine all-round view, all of the major fell groups being visible. Derwentwater can be brought into sight by moving to the north-west cairn.[1][2]



References




  1. ^ ab Wainwright, A (1958). A Pictorial Guide to the Lakeland Fells, Book 3 The Central Fells. Westmorland Gazette..mw-parser-output cite.citation{font-style:inherit}.mw-parser-output q{quotes:"""""""'""'"}.mw-parser-output code.cs1-code{color:inherit;background:inherit;border:inherit;padding:inherit}.mw-parser-output .cs1-lock-free a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/6/65/Lock-green.svg/9px-Lock-green.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output .cs1-lock-limited a,.mw-parser-output .cs1-lock-registration a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/d/d6/Lock-gray-alt-2.svg/9px-Lock-gray-alt-2.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output .cs1-lock-subscription a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/a/aa/Lock-red-alt-2.svg/9px-Lock-red-alt-2.svg.png")no-repeat;background-position:right .1em center}.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration{color:#555}.mw-parser-output .cs1-subscription span,.mw-parser-output .cs1-registration span{border-bottom:1px dotted;cursor:help}.mw-parser-output .cs1-hidden-error{display:none;font-size:100%}.mw-parser-output .cs1-visible-error{font-size:100%}.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration,.mw-parser-output .cs1-format{font-size:95%}.mw-parser-output .cs1-kern-left,.mw-parser-output .cs1-kern-wl-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right,.mw-parser-output .cs1-kern-wl-right{padding-right:0.2em}


  2. ^ ab Mark Richards: The Central Fells: Collins (2003):
    ISBN 0-00-711365-X


  3. ^ British Geological Survey: 1:50,000 series maps, England & Wales Sheet 29: BGS (1999)













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