Abercrombie Caves (original) (raw)

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The Abercrombie Caves, contained within the , are a series of limestone arch caves that are located in the Central West region of New South Wales, Australia. The caves are renowned for their karst qualities, namely the formation that has been eroded by water action that has developed from a sinkhole to become a blind valley. Several good examples of crayback formations exist in both entrances. The 1,434-hectare (3,540-acre) reserve is situated 75 kilometres (47 mi) south of Bathurst and 125 kilometres (78 mi) north of Goulburn, near the small village of Trunkey Creek. The caves are registered as a natural heritage site on the Register of the National Estate for its large diversity of karst morphological and sedimentological features. Camping in the reserve is permitted, with sixty campground sites and two cottages. The caves are open seven days a week during school holidays; and closed on Monday and Tuesday during school terms. (en)

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wiki-commons:Special:FilePath/Abercrombie_Caves_(3294433460).jpg?width=300

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5189560 (xsd:integer)

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7291 (xsd:nonNegativeInteger)

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999225649 (xsd:integer)

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Public (en)

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14.340000 (xsd:double)

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1842 (xsd:integer)

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The Archway the largest natural arch in the southern hemisphere (en)

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dbr:Limestone

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III (en)

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, New South Wales, Australia (en)

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(en)
Jenolan Caves Reserve Trust (en)
NSW National Parks & Wildlife Service (en)

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Abercrombie Caves (en)
Abercrombie Karst Conservation Reserve (en)

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Abercrombie Caves .jpg (en)

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Entrance to Abercrombie Caves, undated. (en)

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1 (xsd:integer)

dbp:state

nsw (en)

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protected (en)

dbp:url

http://www.environment.nsw.gov.au/NationalParks/parkHome.aspx%3Fid=N0350

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Abercrombie Caves at NSW NPWS (en)

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georss:point

-33.91144 149.35938

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rdfs:comment

The Abercrombie Caves, contained within the , are a series of limestone arch caves that are located in the Central West region of New South Wales, Australia. The caves are renowned for their karst qualities, namely the formation that has been eroded by water action that has developed from a sinkhole to become a blind valley. Several good examples of crayback formations exist in both entrances. (en)

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