- Hindscarth
Infobox Mountain
Name = Hindscarth
Photo = Hindscarth.jpg
Caption = Hindscarth and Robinson fromCatbells . By [http://www.madaboutmountains.com Ann Bowker] .
Elevation = 727 m (2,385 ft)
Location =Cumbria , ENG
Range =Lake District ,North Western Fells
Prominence = 71 m
Parent peak =Dale Head
Coordinates =
Topographic
OS "Landrangers" 89, 90, "Explorer" OL4
Grid_ref_UK = NY215165
Listing = Hewitt, Wainwright, Nuttall
Translation = pass used by the red deer
Language = Norse
Pronunciation =Hindscarth is a
mountain between the valleys ofButtermere and Newlands, in the north-western part of the EnglishLake District . The fell's name is derived from two words from theOld Norse language , "Hind" and "Skarth", and means the pass used by the red deer.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. Hindscarth stands in the southern sector. The principal ridge in this group of fells runs east from Buttermere, climbing over Robinson, Hindscarth andDale Head . It then turns north, descending gradually towardDerwentwater , the main tops beingHigh Spy ,Maiden Moor andCatbells .The ridge from Robinson to Dale Head forms the heads of Little Dale and Newlands, bypassing the intervening summit of Hindscarth. This stands off to the north, forming the dividing wall between the two valleys. The long north west ridge steps down over several tiers of crag to the confluence of its bordering streams. The southern face of Hindscarth looks down over
Honister Pass .Ascents
A popular ascent starts from a parking area nearby
Newlands Chapel and passes over theScope End ridge before continuing up crags to the summit. Due to their proximity, Hindscarth and Robinson are often combined into a single walk starting from Newlands. The fell is also part of a longer walk includingCatbells ,High Spy ,Dale Head and along the "Littledale Edge" ridge to Robinson — the Newlands Horseshoe.Geology
Hindscarth is an example of the Buttermere Formation, an
olistostrome of disrupted, sheared and foldedmudstone ,siltstone andsandstone . British Geological Survey: 1:50,000 series maps, "England & Wales Sheet 29": BGS (1999)]Mining
The northern ridge of Hindscarth which falls away to the Newlands valley has at its foot (at Scope End) one of the most famous former mines in the Lake District. The Goldscope mine has been designated as a major national important site by
English Heritage who have stated that it should receive priority treatment for its protection and preservation. The mine was opened in 1564 and developed in its early days by German miners, who worked its rich veins oflead andcopper . The mine was considered so important in its early days that it was requisitioned for the Crown by Elizabeth I from its then-owner, theEarl of Northumberland . There are considerable spoil heaps on the Newlands Beck side of Scope End and the shaft inside the hillside was sunk to such a considerable depth that it became uneconomical to pump out the water, leading to the closure of the mine at the end of the 19th century.ummit and View
The summit carries an untidy
cairn amid some embedded rocks. Elsewhere there are patches of grass and gravel. A hundred yards south is a larger cairn, marked as a Shelter onOrdnance Survey maps. The view north into the Newlands catchment is excellent, backed bySkiddaw . All of the major fell groups with the exception of High Street can be seen.References
*
Alfred Wainwright : "A Pictorial Guide to the Lakeland Fells , Book 6, The North Western Fells": Westmorland Gazette (1964): ISBN 0-7112-2459-5
* Bill Birkett: "Complete Lakeland Fells": Collins Willow (1994): ISBN 0-00-713629-3
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