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270:(also called Hawthorn Pot and Nostril Pot) is another entrance into the system situated about 100 metres (330 ft) due west of Death's Head Hole, in a shakehole by a kink in the wall. A tight rift leads directly onto a 49-metre (161 ft) pitch which lands in a tall fissure passage. To the west, the passage terminates in a large chamber and a mud choke. To the east the passage divides, with one branch heading towards Eyeholes before becoming too tight, and the other passing through a dug-out constriction into a muddy crawl that finishes on a ledge 21 metres (69 ft) above the floor of the Death's Head Main Chamber, opposite East Passage.
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across the eastern verge, but is hollow below, so as to connect the chasm with a more shallow cavity beyond. The most peculiar feature, however, consists in a second bar-like bridge of limestone somewhat more slender than the first, spanning the secondary rift in exactly the opposite direction to that assumed by the former, so as to meet the greater bar in the middle of its course and form part of the same trellice bridgework. In this manner two cavities, like those of the orbits in a skull are produced; and the result is wonderfully curious and fine.
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260:. It passes under an aven, and eventually lowers to a silted crawl after 150 metres (490 ft). The aven has been climbed for 43 metres (141 ft) to a choked inlet. The stream enters East Passage from a low crawl after 50 metres (160 ft), called Dolphin Passage. This gets larger, and passes a small passage heading towards Eyeholes, a choked pothole located some 50 metres north-east of the entrance to Death's Head Hole, before reaching a very wet section. This has been forced through to the bottom of
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The fenced entrance shaft descends some 64 metres (210 ft) onto a loose boulder slope which leads to a second pitch of 6 metres (20 ft) into the Main
Chamber, a large chamber with a waterfall entering at the east end. An excavated 10-metre (33 ft) deep scaffolded shaft in the bottom
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in 1889, when they reached the bottom of the Main
Chamber, and noted the stream entering from the east. In 1892 the cave was referred to as "Hell Hole" by the local historian and writer Harry Speight, who mistakenly reported that "the true bottom has never been reached". The inlet passage in Lost
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Here is another chasm like the
Fairies' Workshop, not so richly adorned, but still radiant in its embellishments, yet possessing a most remarkable configuration, indeed, that of the head and jaws of a human skeleton. The main shaft of the hole represents the mouth; a bridgelike bar of rock passes
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The entrance to Big Meanie was dug open by
Manchester University Speleological Society (MUSS) in 1971. The connection with Death's Head Hole was opened up in the same year by a joint team from MUSS, Happy Wanderers Cave and Pothole Club, and Northern Cave Club digging through a boulder obstacle.
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The waterfall in the Main
Chamber was climbed in 1949 by members of the Gritstone Club, who explored East Passage and Dolphin Passage, the inlet from Long Drop Cave. The connection with Long Drop Cave was made after bailing the short section of waterlogged passage, by the Gritstone Club in 1981.
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Head spring in Ease Gill. It is thought that what is now the main cave is relatively recent, and that some 350,000 years ago water sinking at
Rumbling Hole followed a phreatic trunk route along the fault, entering Death's Head Hole at the end of East Passage, flowed across what is now the Main
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Johns' Cave was noted by the
Yorkshire Ramblers on their original exploration in 1928, but the water was assumed to originate from Gavel Pot. The connection with Lost Johns' Cave was opened up, by a team from a variety of clubs, in 2011.
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corner of the chamber soon leads into a stream passage some 100 metres (330 ft) long which ends at a 4-metre (13 ft) waterfall into the main Lost Johns' Master Cave about 200 metres (660 ft) from its terminal sump.
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and Big Meanie. The stream which flows through the cave originates from Long Drop Cave, and flows through to Lost Johns' Cave as a tributary, to eventually emerge from the
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315:, and hence to a resurgence in the Leck Beck Valley some 100 metres (330 ft) above the current resurgence, which is now covered with glacial till.
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Chamber, into the passages below Big Meanie. From here the water flowed through a continuation of the now-blocked passage to
Glasfurds Chamber in
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An aven is hole in the roof of a cave passage that may be either a rather large blind roof pocket or a tributary inlet shaft into the cave system
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A 23-metre (75 ft) climb up the waterfall in the Main
Chamber enters East Passage, a well decorated phreatic passage with a
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Balderstone described the entrance shaft to Death's Head Hole in detail in 1881 in
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650:(3 ed.). Clapham, Lancaster: Dalesman Publishing Company. p. 40.
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period. Its development has been largely determined by the same vertical
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Northern Caves. Volume 3. The Three
Counties System and the North-West
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Northern Caves. Volume 3. The Three Counties System and the North-West
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Northern Caves. Volume 3. The Three Counties System and the North-West
236:, an 87-kilometre (54 mi) cave system which spans the borders of
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661:
Sutcliffe, Roger (1985). "The Death's Head Hole – Long Drop Link".
631:
Nunwick, Mick (April–May 2012). "Going Head to Head on Leck Fell".
483:
Waltham, A.C.; Simms, M.J.; Farrant, A.R.; Goldie, H.S. (1997).
418:
Allen, Tim (February–March 2012). "The True Length Unravelled".
458:
Brook, Dave; Griffiths, J; Long, M.H.; Ryder, P.F. (1994).
433:
Brook, Dave; Griffiths, J; Long, M.H.; Ryder, P.F. (1994).
512:. Newton Abbot: David & Charles. pp. 289–290.
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Balderstone, Robert R; Balderstone, Margaret (1890).
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University of Leeds Speleological Association Review
537:. London: Simpkin, Marshall and Co. pp. 72–73.
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487:. London: Chapman & Hall. pp. 30–34.
582:The Craven and North-west Yorkshire Highlands
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327:, and plumbed it at 200 feet (61 m):
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510:Limestone and Caves of North-West England
462:. Dalesman Publish Company. p. 89.
437:. Dalesman Publish Company. p. 91.
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334:A caver descending the entrance shaft
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393:Allshorn, Sam; Swire, Paul (2017).
723:Caves of the Three Counties System
535:Book, Ingleton, Bygone and Present
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606:Yorkshire Ramblers' Club Journal
585:. London: Elliot Stock. p.
554:Yorkshire Ramblers' Club Journal
485:Karst and Caves of Great Britain
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676:"Discoveries and Extensions".
1:
344:The first descent was by the
325:Ingleton - Bygone and Present
35:Entrance of Death's Head Hole
367:Caving in the United Kingdom
16:Cave in Lancashire, England
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152:335 metres (1,099 ft)
144:567 metres (1,860 ft)
646:Thornber, Norman (1959).
550:"The Leck Fell Pot-Holes"
397:. High Mead. p. 91.
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346:Yorkshire Ramblers' Club
136:120 metres (390 ft)
648:Pennine Underground1959
579:Speight, Harry (1892).
560:(15). Leeds: YRC: 60–64
548:Cuttriss, S.W. (1922).
663:Gritstone Club Journal
600:Folley, Innes (1930).
508:Waltham, A.C. (1974).
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117:54.207062°N 2.510612°W
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274:Geology and hydrology
234:Three Counties System
122:54.207062; -2.510612
718:Caves of Lancashire
232:and is part of the
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602:"Lost Johns' Cave"
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240:, Lancashire, and
218:Death's Head Hole
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198:Unrestricted
89:SD 6678 7916
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733:Karst caves
612:(19): 44–59
286:Great Scar
248:Description
205:Cave survey
189:verticality
120: /
96:Coordinates
738:Wild caves
712:Categories
519:0715361813
494:0412788608
469:1855680831
444:1855680831
373:References
282:formed in
268:Big Meanie
226:Lancashire
105:54°12′25″N
75:Lancashire
313:Gavel Pot
308:Leck Beck
290:from the
288:limestone
222:Leck Fell
178:Entrances
172:limestone
157:Discovery
149:Elevation
108:2°30′38″W
77:, England
71:Leck Fell
665:: 89–90.
361:See also
210:cavemaps
67:Location
633:Descent
616:14 July
564:14 July
420:Descent
319:History
238:Cumbria
186:Hazards
165:Geology
83:OS grid
516:
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466:
441:
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284:Visean
194:Access
141:Length
689:Notes
300:fault
224:, in
133:Depth
618:2015
566:2015
514:ISBN
489:ISBN
464:ISBN
439:ISBN
399:ISBN
160:1889
587:278
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608:.
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381:^
244:.
73:,
620:.
610:6
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558:5
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407:.
181:3
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