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The cave was opened to the public in 1976. As of 2018, roughly 300 metres (980 ft) of cave passage is open to the public, one third of the total length of the cave. The tours end at a point called the Highway and exit the cave via a 250-metre (820 ft) man-made tunnel. The access building has been awarded the Europa Nostra prize.
Important local sights include the Aillwee Cave system and Doolin Cave with one of the world's largest stalactites. Population centres include Lisdoonvarna, Ballyvaughan, Kilfenora, Doolin, Lahinch, Ennistymon, Fanore and Kilshanny. Major activity centres include the Burren Outdoor Education Centre, the Burren Centre and the Boghill Centre.
The Burren (/ ˈ b ʌr ə n / BURR-ən; Irish: Boirinn, meaning 'rocky district') [1] is a karst/glaciokarst landscape centred in County Clare, on the west coast of Ireland. [2] It measures around 530 square kilometres (200 sq mi), within the circle made by the villages of Lisdoonvarna, Corofin, Gort and Kinvara. [3]
Aill na Cronain (Irish: Aill na Crónáin; Cronan's cliff) is an inland west-facing limestone crag in The Burren in County Clare, Ireland.It is popular with novice rock climbers due to the number of short single-pitch 10–20 metre rock climbing routes in the S to HS rock climbing grades. [1]
Doolin Cave (Irish: Pol an Ionain or Poll-an-Ionain) is a limestone cave near Doolin in County Clare, Ireland, on the western edge of The Burren. The name is the anglicised version of the Irish name Poll an Eidhneáin , which is said to translate into "Ivy Cliff Cave". [ 1 ]
View with karst limestone pavement in foreground. Poulnabrone dolmen is located on a low circular mound measuring c. 10 m (33 ft) in diameter. The site is east of the Poulanine and Glensleade valleys, beyond which are the rocky Baur and Poulnabrucky hills.
Possible cave entrances on Mars. The pits have been informally named (A) Dena, (B) Chloe, (C) Wendy, (D) Annie, (E) Abby (left) and Nikki, and (F) Jeanne. As of 2007 [update] seven putative cave entrances have been identified in satellite imagery of the planet Mars , all so far located on the flanks of Arsia Mons . [ 53 ]
Much of the water in the cave is fed from the sinks of Upper Pollnagollum, at the point where surface water runs off the shale bedrock and sinks into the permeable limestone. The terminus of the cave is a low bedding plane which eventually becomes too low to progress. The water resurges at the Killaney rising to the south of the cave.
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