- Grey Knotts
Infobox Mountain
Name = Grey Knotts
Photo = Grey_Knotts_from_above_the_Stonethwaite_valley.jpg
Caption = Grey Knotts seen from above the Stonethwaite valley
Location =Cumbria , ENG
Range =Lake District ,Western Fells
Elevation = 697 m (2,287 ft)
Grid_ref_UK = NY217125
Topographic
OS "Landranger" 89, 90 OS "Explore Outdoor Leisure" 4
Parent Peak =Brandreth
Prominence = "c." 15 m
Listing = Wainwright, NuttallGrey Knotts is a
fell in the EnglishLake District , it is situated one kilometre south of theB5289 road as it crosses the Honister Pass, it is well seen from midBorrowdale as it rises above Seatoller. Grey Knotts reaches a height of 697 metres (2287 feet) and is part of a ridge which ascends from the woodland behind Seatoller and continues south-west and then south for four kilometres toGreat Gable . The fell's name really only applies to the summit rocks but has been adopted for the entire fell with the high ground in this area locally known as Seatoller Fell onOrdnance Survey maps.Topography
Grey Knotts is a “Wainwright” fell and also qualifies as a Nuttall but this must be a borderline case as it barely has the required 15 metres of prominence to the adjoining higher fell of Brandreth.
All the highlights of Grey Knotts are situated on the eastern (Borrowdale) side of the fell, Raven Crag, known as Gillercombe Buttress to rock climbers, it is a popular area for
bouldering using the large amount of large boulders that have become detached from the main crag, there are also several conventional climbing routes up the main crag. Gillercomb (spelt like this on map) is a fine example of ahanging valley from which issues the stream of Sour Milk Gill which descends into Borrowdale in a series of picturesque cascades.Geology
The principal rock types are the
plagioclase -phyricandesite lava s of the Birker Fell Formation.British Geological Survey: 1:50,000 series maps, "England & Wales Sheet 29": BGS (1999)]Graphite Mine
Also on the Borrowdale side of the fell at the upper end of Newhouse Gill at grid reference gbm4ibx|NY231128 is the site of the former Borrowdale
graphite (then called Plumbago) mines. The mine was started in the 16th century by German immigrants, the graphite found was in a very pure form and in the early days was just used for marking sheep. However, later it was found to be suitable for lining the casting moulds for canon and musket balls and led to its value soaring in the 17th century as England, France and Holland built up their armies. The graphite was also used inpencil making and in 1790 led to the founding of the Cumberland pencil industry based in Keswick. The mine closed in 1891 after new techniques meant that the graphite did not have to be so pure and the Borrowdale mine became uneconomic.Ascents
Grey Knotts can be ascended from Seathwaite or Seatoller in Borrowdale or from the top of the Honister Pass. The route from Seathwaite goes up Newhouse Gill thus allowing the walker to inspect the old graphite mines while the path from Seatoller has to use the B5289 road for a kilometre before going onto the fell and following a wall for some distance then climbing the northern end of Raven Crag to reach the summit. Grey Knotts is often climbed from the top of the Honister Pass which gives the advantage of starting at a height of 356 metres (1167 feet). Walkers often use Grey Knotts as a stepping stone for the ascent of Great Gable from Honister Pass also passing over the adjoining fells of Brandreth and Green Gable on the way.
ummit and View
The top of the fell is dotted with grey tors of rock and two of these give the fell twin tops of equal height, the eastern top has an Ordnance Survey
trig point . There are also several small tarns on the summit as well as some fence posts which can be an aid to navigation. The view from the summit is very good with the Buttermere valley well seen to the north west and theScafell massif standing out to the south.References
* cite book|title=A Pictorial Guide to the Lakeland Fells, Western Fells
author=Alfred Wainwright
year=2005
isbn=0-7112-2460-9
* cite web|url=http://www.cumbria-industries.org.uk/wad.htm
title=Industries of Cumbria - Wad
author=Dave Bridge
accessdate=2008-05-18
* cite journal|journal=RRCPC Newsletter
title=Borrowdale Wad Mine
author=Samuel Carradice
volume=38
issue=2
date=May 2001
url=http://www.rrcpc.org.uk/newsletters/NL_V38_N2_A7.htm
accessdate=2008-05-18
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