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427:, visually the most impressive face in the area. The southwestern 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
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248:. Two slate workings, Elterwater Quarry and Spout Cragg Quarry have been more or less continually working using modern methods. Elterwater is the larger of the two, and like Spout Cragg, is operated by the Burlington Stone company. There are various other local quarries now fallen into disuse, such as Lingmoor, Banks, Thrang Crag and Colt Howe.
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and many famous climbers have stayed at the hotel or drunk in the bar. In climbing circles it is known as the "ODG". Further down the valley there is the New
Dungeon Ghyll hotel, built in 1862. Campsites in the area include the National Trust site near Dungeon Ghyll and the Baysbrown Farm campsite at
418:
Harrison
Stickle is the high point of the Langdale Pikes and its crags fall south and east from the summit, presenting an arresting view from the valley floor 2,000 feet (610 metres) below, or from further afield. To the north, the main ridge of the central fells passes over Thunacar Knott before
568:. There are also rock-climbing spots on the valley floor, such as Raven Crag, Gimmer Crag, and White Ghyll, providing some of the most spectacular rock routes in the UK. The Langdale Leisure Limited company, consisting of a hotel, timeshare lodges and leisure facilities, operates in the valley.
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on the north side of the valley, starting on the fell slopes between
Harrison Stickle and Loft Crag/Pike o' Stickle. It is narrow, and a No Through Route for walkers. Much more open is Stickle Ghyll, which descends from Stickle Tarn. There is a well–trodden path from the Stickle Ghyll car park
306:
Among the best-known features of Great
Langdale are the Langdale Pikes, a group of peaks on the northern side of the dale. From below, they appear as a sharp rocky ridge, though they are precipitous only on their southern side; to the north, the land sweeps gently to
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Loft Crag has a summit elevation of 2,238 feet (682 metres). It lies between
Harrison Stickle and Pike o’ Stickle and is usually climbed in conjunction with these two peaks. The fell has a small sharp summit, below which rises Gimmer Crag, which is one of the top
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which has been dammed to create additional capacity. The stone-faced barrage is low enough not to spoil the character of the pool, and the water is used for public consumption in the hotels and homes below. The tarn has a depth of around 50 feet (15 metres).
126:, and other outdoor enthusiasts who are attracted by the many fells ringing the head of the valley. Among the best-known features of Great Langdale are the Langdale Pikes, a group of peaks on the northern side of the dale. England's highest mountain,
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Pike of
Stickle, also known as Pike o’ Stickle, reaches a height of 709 metres (2,326 ft). The rearward slopes show evidence of the Pavey Ark Member, pebbly
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333:. The Langdale face displays several strata: from the top the Lingmell Formation, Crinkle Member and Bad Step Tuff. These are composed, respectively, of
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is a water-filled corrie about 50 feet (15 metres) deep, this being enhanced by a dam. The water is used for public consumption in Great
Langdale.
311:, the parent peak of the range. The Pikes themselves include (from west to east) Pike of Stickle, Loft Crag, Harrison Stickle, and Pavey Ark.
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opposite the New
Dungeon Ghyll hotel up to the tarn, parts of which have been improved with stone slabs to reduce
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mile (400 metres) across and drops about 400 feet (120 metres). To the southwest, it merges into the crags of
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The mouth of the valley is located at
Skelwith Bridge, which lies about two miles (three kilometres) west of
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746:"Brief Encounter, Middle Fell Bridge, Dungeon Ghyll, Cumbria, UK - Movie Locations on Waymarking.com"
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130:, can be climbed by a route from Langdale. Langdale has views of, in particular, Dungeon Ghyll Force
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847:"The Old Dungeon Ghyll Hotel in Langdale has a fascinating history in the Lake District area"
423:. The craggy eastern face of this ridge continues north as far as Harrison's near neighbour,
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routes including
Bowfell, Crinkle Crags, the Langdale Pikes and England's highest mountain,
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Middle Fell Bridge here is the bridge centring in the plot of the landmark film 1945
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head, created on the slopes of the Pike of Stickle and traded all over prehistoric
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516:, known as Dungeon Ghyll Force, is up a path behind the Old Dungeon Ghyll Hotel.
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rock and was pioneered in the early 1880s by the father of British rock climbing
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suitable for making polished axes which have been found distributed across the
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19:"Langdale" redirects here. For the community in British Columbia, Canada, see
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Pavey Ark is 700 metres (2,297 feet) high. The main face is a little over
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and later, was also one of the centres of the Lakeland slate industry.
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Neolithic Britain: new stone age sites of England, Scotland, and Wales
824:. By Brown, Christopher Stephen. Kogan Page Publishers. p. 340.
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Great Langdale was an important site during the Neolithic period for
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349:-like tuff. The altitude places Loft Crag and Gimmer Crag within
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Great Langdale had a productive stone axe industry during the
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The Langdale Pikes and the Langdale Boulders, Great Langdale.
592:. The hotel and the Hikers Bar have a long association with
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Landon, Letitia Elizabeth (1832). "poetical illustration".
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The sustainable enterprise: profiting from best practice
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greenstone quarried or perhaps just collected from the
588:, and who was later buried in Holy Trinity Church in
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is three kilometres (two miles) west-southwest. The
836:Mini case-study of business–community partnership.
580:and inn. It was bought by the historian Professor
646:British Geological Survey: 1:50,000 series maps,
388:venues in the Lake District. The crag is made of
192:are found on the Langdale Boulders at Copt Howe.
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40:Great Langdale seen from the top of Rossett Pike
951:Sites of Special Scientific Interest in Cumbria
900:(nb: provisional research only – see Talk page)
797:"Camping in the Lake District – Great Langdale"
107:. Langdale is also the name of a valley in the
976:National Trust properties in the Lake District
266:period. The area has outcrops of fine-grained
204:. The Langdale valley contains two villages,
818:Grayson, David (2005). "12.4 The community".
770:Landon, Letitia Elizabeth (1832). "picture".
576:The Old Dungeon Ghyll Hotel was originally a
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685:: 1:50,000 series maps: sheet 38; BGS (1998)
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491:, at the head of the Oxendale valley, and
871:A Year in the Life of the Langdale Valley
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898:Cumbria County History Trust: Langdales
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782:Fisher's Drawing Room Scrap Book, 1833
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773:Fisher's Drawing Room Scrap Book, 1833
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479:Bow Fell at the head of Great Langdale
161:as the source of a particular type of
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700:Pictorial Guide to the Lakeland Fells
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495:on the southern side of the valley.
874:. Frances Lincoln Ltd. p. 13.
487:. Other notable Langdale fells are
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68:Great Langdale valley shown within
27:. For people with the surname, see
23:. For the former Alabama town, see
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177:. It also supplied stone for some
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868:Bill Birkett (15 November 2004).
483:Great Langdale's highest fell is
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556:Old Dungeon Ghyll from Side Pike
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345:tuff and breccia; and rhyolitic
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971:Archaeological sites in Cumbria
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744:bill&ben (24 August 2010).
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704:: Westmorland Gazette (1958):
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369:are also potentially visible.
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244:were centres of the Lakeland
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118:It is a popular location for
648:England & Wales Sheet 38
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414:A waterfall in Stickle Ghyll
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157:Great Langdale is known to
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956:Stone Age sites in England
702:, Book 3 The Central Fells
560:There are several popular
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536:'s poetical illustration,
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394:Walter Parry Haskett Smith
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282:in the Langdale Valley on
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21:Langdale, British Columbia
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16:Valley in Cumbria, England
683:British Geological Survey
619:. Routledge, 1992. 1992.
725:Exploring Lakeland Tarns
540:(1832), to a picture by
534:Letitia Elizabeth Landon
981:South Lakeland District
785:. Fisher, Son & Co.
776:. Fisher, Son & Co.
584:who donated it to the
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220:. Great Langdale is a
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258:Langdale axe industry
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927:54.44912°N 3.07333°W
147:producing stone axes
64:class=notpageimage|
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503:Dungeon Ghyll is a
341:-tuff and breccia;
240:Great Langdale and
961:Valleys of Cumbria
932:54.44912; -3.07333
666:: Collins (2003):
612:Rodney Castleden,
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529:Cultural reference
481:
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294:The Langdale Pikes
190:cup and ring marks
183:stone wrist-guards
101:North West England
42:
29:Langdale (surname)
881:978-0-7112-2449-0
695:Alfred Wainwright
664:The Central Fells
572:Old Dungeon Ghyll
274:. The rock is an
181:items, including
25:Langdale, Alabama
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753:. Retrieved
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723:Blair, Don:
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650:: BGS (1999)
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630:. Retrieved
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590:Chapel Stile
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566:Scafell Pike
562:fell walking
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542:Thomas Allom
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419:climbing to
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280:scree slopes
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252:Axe industry
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206:Chapel Stile
199:
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128:Scafell Pike
124:fell-runners
122:, climbers,
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966:Westmorland
930: /
755:17 February
471:Other fells
945:Categories
915:54°26′57″N
904:360 photos
853:10 October
803:10 October
632:10 October
626:0415058457
601:References
512:. Another
421:High Raise
351:sightlines
309:High Raise
276:epidotised
268:greenstone
242:Elterwater
224:formed by
218:High Close
210:Elterwater
179:Bronze Age
918:3°04′24″W
514:waterfall
441:Pavey Ark
435:Pavey Ark
425:Pavey Ark
379:Loft Crag
373:Loft Crag
343:rhyolitic
327:sandstone
264:Neolithic
202:Ambleside
196:Geography
187:Neolithic
163:Neolithic
132:waterfall
594:climbing
485:Bow Fell
390:Rhyolite
226:glaciers
212:, and a
80:NY305065
548:Tourism
510:erosion
450:⁄
367:Skiddaw
359:Bowfell
339:lapilli
331:breccia
153:History
113:Cumbria
95:in the
70:Cumbria
878:
828:
731:
708:
670:
623:
505:ravine
461:corrie
357:while
214:hamlet
175:Europe
138:, and
120:hikers
93:valley
91:is a
876:ISBN
855:2009
826:ISBN
805:2009
757:2019
729:ISBN
706:ISBN
668:ISBN
634:2009
621:ISBN
578:farm
464:tarn
429:tarn
365:and
347:lava
335:tuff
329:and
286:and
208:and
173:and
353:to
216:at
167:axe
99:in
947::
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.