Stump Cross Caverns
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Stump Cross Caverns is a
limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe ...
cave system between
Wharfedale Wharfedale ( ) is the valley of the upper parts of the River Wharfe and one of the Yorkshire Dales. It is situated within the districts of Craven and Harrogate in North Yorkshire, and the cities of Leeds and Bradford in West Yorkshire. It i ...
and
Nidderdale Nidderdale, historically also known as Netherdale, is one of the Yorkshire Dales (although outside the Yorkshire Dales National Park) in North Yorkshire, England. It is the upper valley of the River Nidd, which flows south underground and then ...
in
North Yorkshire North Yorkshire is the largest ceremonial counties of England, ceremonial county (lieutenancy area) in England, covering an area of . Around 40% of the county is covered by National parks of the United Kingdom, national parks, including most of ...
,
England England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe b ...
.


Geography

The caverns at Stump Cross are located beneath
Greenhow Greenhow is a village in North Yorkshire, England, often referred to as Greenhow Hill. The term ''how'' derives from the Old Norse word ''haugr'' meaning a hill and a mound, so Greenhow literally means 'Green's hill or mound'. History It is s ...
hill, above sea level. Their name was taken from Stump Cross, which in ancient times marked the limit of Knaresborough Forest. The area above the caves consists largely of moorland, the nearest towns being
Pateley Bridge Pateley Bridge (known locally as Pateley) is a small market town in Nidderdale in the Borough of Harrogate, North Yorkshire, England. Historically part of the West Riding of Yorkshire, it lies on the River Nidd. It is in the Yorkshire Dales an ...
and
Grassington Grassington is a market town and civil parish in the Craven district of North Yorkshire, England. The population of the parish at the 2011 Census was 1,126. Historically part of the West Riding of Yorkshire, the town is situated in Wharfedal ...
. One mile of the caves have been open to the public for many years, although the entire system is much more extensive than the show caves, extending more than . It has not yet been fully explored. The system is located in a region of
limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe ...
extending from
Wharfedale Wharfedale ( ) is the valley of the upper parts of the River Wharfe and one of the Yorkshire Dales. It is situated within the districts of Craven and Harrogate in North Yorkshire, and the cities of Leeds and Bradford in West Yorkshire. It i ...
to Greenhow and the
Craven Fault The Craven Fault System is the name applied by geologists to the group of crustal faults in the Pennines that form the southern edge of the Askrigg Block and which partly bounds the Craven Basin. Sections of the system's component faults whic ...
.
Lead Lead is a chemical element with the symbol Pb (from the Latin ) and atomic number 82. It is a heavy metal that is denser than most common materials. Lead is soft and malleable, and also has a relatively low melting point. When freshly cu ...
has been mined in the region since the era of the
Roman empire The Roman Empire ( la, Imperium Romanum ; grc-gre, Βασιλεία τῶν Ῥωμαίων, Basileía tôn Rhōmaíōn) was the post- Republican period of ancient Rome. As a polity, it included large territorial holdings around the Mediter ...
.


History

The caves are thought to have been formed around 500,000 years ago, although the process by which they were created began during a much earlier period in which the region was covered by ocean. They were discovered in January 1860 by William and Mark Newbould, who were amongst a group of miners prospecting for lead veins in the Yorkshire Dales. Some sources have given the date of their discovery as 1858. By 1867 of the caves had been explored. In 1922 the caves were explored more thoroughly by Christopher Long, a student at
Caius College, Cambridge Gonville and Caius College, often referred to simply as Caius ( ), is a constituent college of the University of Cambridge in Cambridge, England. Founded in 1348, it is the fourth-oldest of the University of Cambridge's 31 colleges and one of th ...
. His discoveries included stalactites in a range of colours, suggesting that they were impregnated with iron and lead. Long claimed that he had also discovered an underground lake, but is said to have sealed its entrance when the caves' owners refused to allow him a share of the revenue generated by tourism to the site. The caverns were sold in 1926 to Septimus Wray, the owner of the Heysham Head Pleasure Gardens, for £400, who installed his son in law, Harry Deane Hornby to run them on his behalf. Septimus Wray's grandson, George Gill later took over the running of the caves, and installed electric lighting, and started to promote the caves as a tourist attraction with the caves remaining in his family until 2003. In 1963 Geoffrey Workman spent 105 days in the caves, a world record, as part of a study on the effects of isolation on the body. Stump Cross developed into a tourist destination in the decades that followed, gaining an information centre, gift shop and a two-bedroomed cottage for the owners. The caves gained Site of Special Scientific Interest designation, and the Reindeer Cave was opened to the public in 2000, forty-five years after it was first discovered. In 2001 the caves were affected by the cleanup of nearby farms during the foot-and-mouth crisis. By 2003 over 60,000 people visited the caves every year. In the same year they were put on the market by then-owner Gordon Hanley, a son of George Gill's second wife, for £675,000. Ownership of the site passed to the Bowerman family, who also part-own the
Richmond Brewery Company Richmond most often refers to: * Richmond, Virginia, the capital of Virginia, United States * Richmond, London, a part of London * Richmond, North Yorkshire, a town in England * Richmond, British Columbia, a city in Canada * Richmond, California, ...
, which in 2008 released an ale named after Stump Cross.


Fossils

Several
fossil A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved ...
s have been discovered in the Stump Cross system. The initial discoverers of the caves found four near-complete
reindeer Reindeer (in North American English, known as caribou if wild and ''reindeer'' if domesticated) are deer in the genus ''Rangifer''. For the last few decades, reindeer were assigned to one species, ''Rangifer tarandus'', with about 10 sub ...
fossils and a smaller skeleton believed to be that of an unborn reindeer. These have since been privately restored. Christoper Long's 1922 exploration revealed more prehistoric reindeer bones, and also those of
wolverine The wolverine (), (''Gulo gulo''; ''Gulo'' is Latin for " glutton"), also referred to as the glutton, carcajou, or quickhatch (from East Cree, ''kwiihkwahaacheew''), is the largest land-dwelling species of the family Mustelidae. It is a muscul ...
s. The wolverine bones are now on display at the site's visitor centre. Bison remains have also been found.


References


External links


Stump Cross Caverns website
{{coord, 54.06739, -1.86509, type:landmark_region:GB, display=title Show caves in the United Kingdom Nidderdale Caves of North Yorkshire Sites of Special Scientific Interest in North Yorkshire