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  2. Aillwee Cave - Wikipedia

    en.wikipedia.org/wiki/Aillwee_Cave

    The cave is typical of the Clare caves, consisting in the main of stream passage and ending in a sump. The general direction is east to west but turns due south some 600 metres (2,000 ft) into the cave. The cave is considerably older than most of the Clare caves and originally contained a large stream.

  3. The Burren - Wikipedia

    en.wikipedia.org/wiki/The_Burren

    The largest is the Carran depression, more than two miles long, up to a mile wide and over 200 feet deep. This is where the pre-glacial rivers of the area first eroded away the upper layers and started to dissolve the exposed limestone. Some of the smaller ones were created when caves underneath collapsed (one example of this is the Glen of Clab).

  4. Poulnabrone dolmen - Wikipedia

    en.wikipedia.org/wiki/Poulnabrone_dolmen

    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.

  5. Aill na Cronain - Wikipedia

    en.wikipedia.org/wiki/Aill_na_Cronain

    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]

  6. Doolin Cave - Wikipedia

    en.wikipedia.org/wiki/Doolin_Cave

    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 ]

  7. Pollnagollum - Wikipedia

    en.wikipedia.org/wiki/Pollnagollum

    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.

  8. Mount Rainier’s ice caves may be beautiful but they’re also ...

    www.aol.com/news/mount-rainier-ice-caves-may...

    Ice cave history. Mount Rainier was once known for its well-developed ice cave system, the Park Service said. Those melted away due to a warming climate. Now, ice caves are seasonal and more unstable.

  9. Ailladie - Wikipedia

    en.wikipedia.org/wiki/Ailladie

    The name Ailladie is an anglicized translation from the Irish language name, Aill an Daill, which means 'The Blind Man's Cliff' or 'Cliff of the Blind Person'. [3] [1] The cliffs are also referred to locally, and by anglers, as Ballyreen Cliffs and Ballyreen Point, which is an anglicised version of the name given to Ailladie's local townland of Irish: Baile Uí Rinn; 'Ó Rinn's homestead'.