Pike of Stickle

Infobox Mountain
Name = Pike of Stickle
Photo = Pike_of_Stickle_from_Loft_Crag.jpg
Caption = Pike of Stickle as seen from the neighbouring fell of Loft Crag
Elevation = 709 m (2,326 ft)
Location = Cumbria, ENG
Range = Lake District, Central Fells
Prominence = "c." 54 m
Parent peak = High Raise
Coordinates =
Topographic
OS "Explorer" OL6
Grid_ref_UK = NY273073
Listing = Hewitt, Wainwright, Nuttall
Translation =
Language =
Pronunciation =

Pike of Stickle, also known as Pike O’ Stickle, is a fell in the English Lake District. It reaches a height of 709 metres (2,326 feet) and is situated in the central part of the national park in the valley of Great Langdale. The fell is one of the three fells (the others being Harrison Stickle and Loft Crag) which make up the picturesque Langdale Pikes, one of the best known areas in Lakeland. A "stickle" is a hill with a steep prominent rocky top, while a "pike" is a hill with a peaked summit, the name therefore being partly tautological.

Topography

The Langdale Pikes form a raised rocky parapet around the southern and eastern edges of a high tableland centred upon Thunacar Knott. Pike Of Stickle stands at the western end of this system and its crags fall south from the summit, presenting an arresting view from the valley floor 2,000 ft below, or from further afield.

Loft Crag stands next along the rampart, with Thorn Crag and Harrison Stickle further to the east. 'Behind' Pike of Stickle to the north is the depression of Harrison Combe, beyond which are the twin tops of Thunacar Knott. Westward the height of the land gradually falls away to Martcrag Moor, a wide plateau with a few small tarns near the summit (1,795 ft). Martcrag Moor represents the end of the Central Fells as defined by Alfred Wainwrightcite book |author=Wainwright, A |title= A Pictorial Guide to the Lakeland Fells, Book 3 The Central Fells |publisher= Westmorland Gazette |year= 1958] , providing a high level connection to Rossett Pike in the Southern Fells.

Geology

The rearward slopes show evidence of the Pavey Ark Member, pebbly sandstone and breccia. The Langdale face displays several strata, from the top The Lingmell Formation, Crinkle Member and Bad Step Tuff. These are composed, respectively, of tuff, lapilli-tuff and breccia; rhyolitic tuff and breccia; and rhyolitic lava-like tuff.British Geological Survey: 1:50,000 series maps, "England & Wales Sheet 38": BGS (1999)] .

ummit and View

Despite the peaked profile the summit is wide enough for a sizeable cairn surrounded by a small level area. Loft Crag and Gimmer Crag steal the attention in the foreground while Bowfell impresses across Langdale. A wide swathe of the Southern Fells is in view, whilst even distant Skiddaw puts in an appearance.Mark Richards: "The Central Fells": Collins (2003): ISBN 0-00-711365-X]

Ascents

Pike of Stickle rises steeply from Langdale, culminating in a narrow tapering summit which gives excellent views of the head of the valley, the fells of Bow Fell and Crinkle Crags showing well. The fell is invariably climbed from Great Langdale with either the New or Old Dungeon Ghyll Hotels as the starting points. There are a number of routes, the most common ascent being a path that slants across the hillside from the New hotel passing between Thorn Crag and Gimmer Crag and then turning left at the col. A quieter route is by Troughton Beck; the walker starts from the Old hotel and goes four kilometres towards the head of the valley before bearing right and following a zig-zag path at the side of Troughton Beck. This route gives the walker an unusual view of the fell from this unfrequented side. There is another route directly up the Stickle Stone Shoot: this route is steep and has become severely eroded in recent years and is no longer recommended as a means of ascent or descent. The Langdale or Borrowdale sides of Stake Pass can also be used, giving access onto Martcrag Moor.

tone Axe Factory

Pike of Stickle is famous as the site of a neolithic stone axe factory; it is situated on the scree slope on the steep southern slope of the fell and is one of the most important prehistoric axe factories in Europe. The factory was set up here because of a vein of greenstone, a very hard volcanic rock, which comes to the surface around the head of the valley. Evidence of axe manufacture have been found in many areas of Great Langdale but it is the screes of Pike of Stickle which have yielded the most discoveries. There is a small cave at the top of the Stickle Stone Shoot near the summit of the fell which was part of the stone axe factory.

References