Pate Hole is a solutional cave located adjacent to Asby Gill 1 kilometre (0.62 mi) south of Great Asby in Cumbria, England. It is 970 metres (3,180 ft) long and has a vertical range of 33 metres (108 ft). The entrance is normally dry, but in flood it becomes an impressive resurgence.[1] Its name derives from the north country word for badger.[2]

Pate Hole
The entrance to Pate Hole
Map showing the location of Pate Hole
Map showing the location of Pate Hole
Showing location of Pate Hole in Cumbria
LocationGreat Asby, Cumbria, England
OS gridNY 678 121
Coordinates54°30′13″N 2°29′53″W / 54.5035°N 2.4981°W / 54.5035; -2.4981[1]
Depth33 metres (108 ft)[1]
Length970 metres (3,180 ft)[1]
Elevation195 metres (640 ft)[1]
GeologyCarboniferous limestone
Entrances1
DifficultyIII[1]
Hazardsflooding[1]
Cave surveyOn Cavemaps

It consists of three main passages. From the entrance a stooping height passage heading south-east reaches a large 6 metres (20 ft) deep pool after 330 metres (1,080 ft) from which a stream emerges. This flows down a low passage to the north for some 270 metres (890 ft) where a sump is reached. The third main passage continues south underwater from the pool for 225 metres (738 ft) at a depth of 27 metres (89 ft) where it reaches a junction and becomes too restricted.[1]

The cave is formed in Carboniferous limestone,[3] and is thought to drain the Great Asby Scar area 3 kilometres (1.9 mi) to the south-west.[4] The resurgence is presumed to be St. Thomas's Well in Great Asby.[5]

The main part of the cave has been known for a long time, and it was an object of curiosity in the nineteenth century.[6] A brief foray into it was described in The Gentleman's Magazine in 1791,[7] and a description appeared in The Monthly Magazine in 1802.[2] The first full description complete with passage lengths appeared in 1813.[8] The first account of an exploration by cavers was in 1941 by members of the Yorkshire Ramblers' Club,[9] and in November 1946 it was surveyed by a group from Appleby Grammar School led by Brian Price.[10] The upstream sump was first dived for about 10 metres (33 ft) to a descending rift in 1960 by members of the Cave Diving Group, at which time the main part of the cave was re-surveyed by Warburton et alia. Further exploration took place in 1975-1976 by members of the same group to reach the current limit.[4]

References

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  1. ^ a b c d e f g h Brook, Dave (1994). Northern Caves Volume 3. The Three Counties System and the North West. Skipton: Dalesman Publishing Company Ltd. pp. 254–255. ISBN 1855680831.
  2. ^ a b Phillips, Richard (1 February 1802). "Account of Asby in the County of Westmoreland". The Monthly Magazine. XIII (1): 115–116. Retrieved 31 March 2017.
  3. ^ "Geology of Britain Viewer". British Geological Survey. Retrieved 30 December 2013.
  4. ^ a b Metcalfe, Dave (October 1978). "Pate Hole". Belfry Bulletin (366): 4. Retrieved 30 December 2013.
  5. ^ Hill, Elaine; Hall, Adrian (2015). Northern Sump Index 2015. Cave Diving Group. p. 288,343. ISBN 978-0-901031-08-2.
  6. ^ Bell, Thomas (1836). The scientific tourist through England, Wales & Scotland, Volume 2. Glasgow: A Fullarton and Co. p. 64.
  7. ^ "Letter from T.C." The Gentleman's Magazine. 70: 923. 1791. Retrieved 31 December 2013.
  8. ^ Bitton, John (1813). The Beauties of England and Wales. London: Longman & Co. pp. 152–153.
  9. ^ "Cave Exploration". Yorkshire Ramblers' Club Journal. 7 (24): 77–183. 1947. Retrieved 30 December 2013.
  10. ^ Price, Brian (1947). "Pate Hole, Westmorland (letter)". The British Caver (16): 87–88.