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Pen Park Hole is a large cavern situated underground, at the edge of Filton Golf Course. The cavern was discovered accidentally in the 17th Century and the first descent was made by Captain Sturmy in 1669. The entrance is adjacent to the Southmead and Brentry housing estates of north Bristol. Access is tightly controlled by Bristol City Council. It was scheduled as a Site of Special Scientific Interest in 2016 on account of its geological origins, and its cave invertebrate community including the cave shrimp , which is normally known as a spring seepage or chalk aquifer species.

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rdf:type
rdfs:label
  • Pen Park Hole (en)
rdfs:comment
  • Pen Park Hole is a large cavern situated underground, at the edge of Filton Golf Course. The cavern was discovered accidentally in the 17th Century and the first descent was made by Captain Sturmy in 1669. The entrance is adjacent to the Southmead and Brentry housing estates of north Bristol. Access is tightly controlled by Bristol City Council. It was scheduled as a Site of Special Scientific Interest in 2016 on account of its geological origins, and its cave invertebrate community including the cave shrimp , which is normally known as a spring seepage or chalk aquifer species. (en)
foaf:name
  • Pen Park Hole (en)
name
  • Pen Park Hole (en)
geo:lat
geo:long
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/Pen_Park,_Southmead_(geograph_3858829).jpg
location
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thumbnail
location
photo
  • Pen Park, Southmead .jpg (en)
photo caption
  • Pen Park. The cavern is screened by trees in the background (en)
registry
  • Mendip Cave Registry (en)
georss:point
  • 51.510421 -2.598882
has abstract
  • Pen Park Hole is a large cavern situated underground, at the edge of Filton Golf Course. The cavern was discovered accidentally in the 17th Century and the first descent was made by Captain Sturmy in 1669. The entrance is adjacent to the Southmead and Brentry housing estates of north Bristol. Access is tightly controlled by Bristol City Council. It was scheduled as a Site of Special Scientific Interest in 2016 on account of its geological origins, and its cave invertebrate community including the cave shrimp , which is normally known as a spring seepage or chalk aquifer species. (en)
access
  • locked, controlled by Bristol City Council (en)
discovery
geology
grid ref UK
  • ST 5853 7922 (en)
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depth (μ)
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page length (characters) of wiki page
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foaf:isPrimaryTopicOf
geo:geometry
  • POINT(-2.5988819599152 51.51042175293)
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