Harrison Stickle

Coordinates: 54°27′25″N 3°06′38″W / 54.45687°N 3.11056°W / 54.45687; -3.11056
Source: Wikipedia, the free encyclopedia.

Harrison Stickle
Nuttall
Coordinates54°27′25″N 3°06′38″W / 54.45687°N 3.11056°W / 54.45687; -3.11056
Geography
LocationCumbria, England
Parent rangeLake District, Central Fells
OS gridNY281074
Topo mapOS Explorer OL6

Harrison Stickle is a

Langdale Pikes, the others being Pike of Stickle and Loft Crag
. Together they make up one of the most picturesque, and probably the best-known, mountain groups in the District. A "stickle" is a hill with a prominent rocky top.

Topography

The Langdale Pikes form a raised rocky parapet around the southern and eastern edges of a high tableland centred upon Thunacar Knott. Harrison Stickle is the high point of this system and its crags fall south and east from the summit, presenting an arresting view from the valley floor 2,000 feet (610 m) below, or from further afield.

To the north, the main ridge of the central fells passes over Thunacar Knott before climbing to High Raise. The craggy eastern face of this ridge continues north as far as Harrison's near neighbour, Pavey Ark, visually the most impressive face in the area. The south-western border of Harrison Stickle is formed by the deep ravine of Dungeon Ghyll, which cuts through the parapet of the Langdale Pikes and into the lower hinterland of Harrison Combe. Across the Ghyll westwards are Thorn Crag, Loft Crag and finally Pike of Stickle. Below the steep eastern face of Harrison Stickle lie Stickle Tarn and its ghyll, thus ensuring that all drainage from the fell is to Great Langdale. The tarn is a waterfilled corrie about 50 feet (15 m) deep, this being enhanced by a dam. The water is used for public consumption in Great Langdale.[1]

Langdale Pikes
, in the centre of the group

Geology and archaeology

Harrison Stickle's summit area is composed of the pebbly sandstone and breccia of the Pavey Ark Member.[2]

Several

neolithic period. The sites on Pike O'Stickle have been well described as the Langdale axe industry, but they have been found to be much more widespread than originally thought. The rock was roughly shaped on site, and then traded across the country, where the final polishing could be undertaken. Such polished axes have been found in Buckinghamshire for example as well as in East Anglia
. The axes varied widely in size, shape and function, and most were designed to be fitted with either wooden or bone handles (using pointed butt ends or narrow waists).

Summit

The summit is a short rocky ridge with a cairn at each end, the northern one being higher. The view from Harrison Stickle is as good as the view of it — a surprisingly rare occurrence — with all of the major fell groups visible.[3][4]

Ascents

The fell is usually climbed from New Dungeon Ghyll Hotel in Great Langdale, and there are a number of possible routes up. The simplest first follows Stickle Beck to Stickle Tarn; a path then leads up the western side of Pavey Ark to reach the summit. The fell is almost invariably combined with other nearby peaks to make a longer circular walk.[3][4]

References

Wikimedia Commons has media related to Harrison Stickle.
  1. ISBN 0-9543904-1-5
  2. ^ British Geological Survey: 1:50,000 series maps, England & Wales Sheet 38: BGS (1999)
  3. ^ a b Wainwright, A (1958). A Pictorial Guide to the Lakeland Fells, Book 3 The Central Fells. Westmorland Gazette.
  4. ^
    ISBN 0-00-711365-X
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