Faill an Fhíona

Faill an Fhíona is recorded as a headland in County Kerry. Its open map record supplies this location and any linked names or public references.

Faill an Fhíona is a headland composed primarily of basalt, formed during the Paleogene period through volcanic activity associated with the opening of the North Atlantic. It is notable for its columnar jointing, a result of the rapid cooling of lava flows, and for its coastal erosion features shaped by Atlantic wave action.