- Whiteless Pike
Infobox Mountain
Name = Whiteless Pike
Photo = Whiteless Pike.jpg
Caption = Whiteless Pike from Whiteless Edge
Location =Cumbria , ENG
Range =Lake District ,North Western Fells
Elevation = 660 m (2,165 ft)
Prominence = "c". 35 m
Parent peak =Crag Hill
Grid_ref_UK = NY180189
Topographic
OS "Landranger" 89, "Explorer" OL4
Listing = Wainwright, Hewitt, NuttallWhiteless Pike (660 metres high/2,165ft) is a
fell in the north-westernEnglish Lake District . It stands immediately east ofCrummock Water and forms a perfectpyramid shape when viewed fromRannerdale . In his celebrated guide to theLakeland fells,Alfred Wainwright called it "theWeisshorn ofButtermere ".Alfred Wainwright : "A Pictorial Guide to the Lakeland Fells , Book 6, The North Western Fells": Westmorland Gazette (1964): ISBN 0-7112-2459-5] There are good views ofGreat Gable and theScafells from the summit.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 Whiteless Pike.The highest ground in the North Western Fells is an east-west ridge in this central sector, beginning with
Grasmoor aboveCrummock Water and then gradually descending eastwards overCrag Hill , Sail,Scar Crags andCausey Pike . Grasmoor has the greatest elevation, but Crag Hill stands at the hub of the range. It sends out a subsidiary ridge to the south west, stepping down overWandope and Whiteless Pike toward Buttermere village.From the broad plateau of Wandope, the fine and airy ridge of Whiteless Edge descends south west to the depression at Saddle Gate (2,065 ft). A short climb then leads to the summit of Whiteless Pike. The ridge now turns south and falls to the wide shoulder of Whiteless Breast (1,440 ft), from where the slope continues down to Buttermere village. This is not however the end of the ridge, which twists sharply north west to continue to
Rannerdale Knotts . Both sides of the ridge are steep throughout.The eastern face of the fell drains via several feeders into Sail Beck, bound for Crummock Water via Buttermere Village. The north western flanks supply Rannerdale Beck, another feeder of Crummock Water which flows between Whiteless Pike and Grasmoor. The sharp elbow in the ridge, between Whiteless Pike and Rannerdale Knotts, forms the head of Squat Beck, a tributary of Rannerdale.
Geology
The summit of the fell is a part of the Kirkstile Formation,
Ordovician rocks of theSkiddaw group. This is primarily laminatedmudstone andsiltstone . The Causey Pike Fault runs across to the south and Whiteless Breast and the lower slopes are examples of the Buttermere Formation, anolistostrome of disrupted sheared and folded mudstone, siltstone andsandstone . Within this are minor intrusions ofbasalt ..British Geological Survey: 1:50,000 series maps, "England & Wales Sheet 29": BGS (1999)] . There is no history of mining on the fell.ummit and view
Whiteless Pike has a small peaked summit overlain with loose stones and bearing a
cairn . The steep slopes add foreground to the view, which includes a fine prospect of theScafells . TheHelvellyn range andWestern Fells are well seen, with the rather drab close-up of Grasmoor perhaps the only disappointment. Buttermere, Crummock andLoweswater complete the view.Ascents
Buttermere provides the obvious starting point, climbing on a good path up Whiteless Breast and onto the ridge. From the shore of Crummock Water, access can be gained into Rannerdale, brancking off up the course of Squat Beck to the elbow in the ridge between Rannerdale Knotts and Whiteless Pike. Circuits of Rannerdale via the complete ridge of Rannerdale Knotts can also be made.Bill Birkett: "Complete Lakeland Fells": Collins Willow (1994): ISBN 0-00-713629-3]
References
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