Why this matters
Cúlfhaill is a sea cliff located in County Kerry, composed primarily of basalt formed during the Paleogene period, around 60 to 55 million years ago, as a result of volcanic activity associated with the opening of the North Atlantic. It is notable for its association with the broader basaltic formations of the region, including those found in the Kerry Slieve Mish Mountains.
What is recorded here
Cúlfhaill is recorded as a cliff in County Kerry. Its open map record supplies this location and any linked names or public references.
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