Why this matters
Cloonconeen Point is a headland composed primarily of Carboniferous limestone, formed around 340 to 320 million years ago through the accumulation of marine sediments. The area is notable for its exposure of folded and faulted rock layers, reflecting the tectonic activity associated with the formation of the Appalachian and Variscan mountain belts.
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Cloonconeen Point is recorded as a headland in County Clare. Its open map record supplies this location and any linked names or public references.
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