- Causey Pike
Infobox Mountain
Name = Causey Pike
Photo = Causey_Pike_from_Derwentwater.jpg
Caption = Causey Pike with its distinctive bump seen from Derwentwater
Elevation = 637 m (2,090 ft)
Location =Cumbria , ENG
Range =Lake District ,North Western Fells
Prominence = 40 m| Parent peak =Scar Crags
Coordinates =
Topographic
OS "Landrangers" 89, 90, "Explorer" OL4
Grid_ref_UK = NY218208
Listing = Hewitt, Nuttall, Wainwright
Translation =
Language =
Pronunciation =Causey Pike is a fell in the English
Lake District . It is situated in theNewlands Valley , 5 km south west of the town of Keswick. Even though it has a modest height of 637 metres (2,090 feet) it is one of the most distinctive fells when viewed from theDerwent Water and Keswick area due to its distinguishing summit "nobble" which catches the eye. The fell is one of 214 fells described byAlfred Wainwright in his series of "Pictorial Guides to the Lakeland Fells ": Causey Pike features in Book Six, "The North Western Fells".Topography
The
North Western Fells occupy the area between the rivers Derwent and Cocker, a broadly oval swathe of hilly country, elongated on a north-south axis. Two roads cross from east to west, dividing the fells into three convenient groups. The central sector, rising betweenWhinlatter Pass andNewlands Pass , includes Causey Pike. The highest ground in the North Western Fells is an east-west ridge in this central sector, beginning withGrasmoor aboveCrummock Water and then gradually descending eastwards overCrag Hill , Sail,Scar Crags and Causey Pike.Causey Pike is separated from Barrow and
Outerside to the north by Stonycroft Gill. Southward across Rigg Beck isArd Crags . Causey Pike has a long blunt ended shoulder running eastward to the Newlands Valley, dropping steeply from its terminus at Rowling End.Geology
The ridge is composed of the laminated
mudstone andsiltstone of the Kirkstile Formation, usually associated with theSkiddaw group. The summit knobble is representative of the Buttermere Formation, anolistostrome of disrupted, sheared and foldedmudstone ,siltstone andsandstone . Rowling End reveals the large olistoliths ofgreywacke sandstone of the Robinson Member.British Geological Survey: 1:50,000 series maps, "England & Wales Sheet 29": BGS (1999)]Ascents
The direct ascent of the fell is usually started from the Newlands valley at Stonycroft where there is some car parking space; this route is steep at the beginning and the end with an easier section in the middle, the final 20 metres of ascent being a rocky scramble. An easier and longer alternative from the same starting point goes by an old track which used to serve the cobalt mine on the slopes of
Scar Crags , this approaches the fell "from the back" reaching Sail pass and then crossing the summit of Scar Crags before attaining Causey Pike. The fell is also part of the horseshoe walk known as the Coledale Round which is usually started at the village of Braithwaite just west of Keswick (but can also be started in the Newlands Valley) and includes the additional fells ofGrisedale Pike ,Hopegill Head ,Grasmoor , Eel Crag, Sail and Scar Crags. It is a strenuous 11 mile (18 km) ridge walk with over 4000 feet (1200 m) of ascent.ummit and View
The summit of the fell is quite unique: it is a narrow ridge with the highest point being on the "nobble" but with four other smaller bumps of almost equal height further on. The scree slopes around the summit have yielded some
fossil s:Trilobite s,Trace fossil s andGraptolite s are found on rare occasions. The view from the summit is extensive with Derwentwater, the Newlands valley,Skiddaw ,Blencathra and theHelvellyn range seen very well.Fell Race
There is an annual Causey Pike fell race which takes place in March; it starts and finishes in the Newlands Valley and has a distance of 4.5 miles (7 km) with 542 metres (1780 feet) of climbing. The 2005 race was won in a time of 32 minutes 51 seconds.
References
*A Pictorial Guide to the Lakeland Fells,The North Western Fells:Alfred Wainwright: ISBN 0-7112-2459-5
*Complete Lakeland Fells, Bill Birkett, ISBN 0-00-713629-3
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