
What is recorded here
Cúinne an Mhionnáin 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 exposure that highlights the region's volcanic geological history.
Places near here
Ballydavid Signal TowerRuins · 786 yd
Hut site in Currach GráigeHut site · 1498 yd
Enclosure in Baile DháithEnclosure · 1642 yd
Moorestown CastleCastle · 1.4 mi
Brandon CreekViewpoint · 1.9 mi
Séipéal Bhréanainn [Saint Brendan's Catholic Church]church/chapel · 2.5 mi
Binn DiarmadaMountain / peak · 3.0 mi
Trá an FhíonaBeach / strand · 4.1 miOther information
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