The big wave
Aill na Searrach
The offshore break at Aillemore — the Foals' Cliff in Irish — only shows its full size when a large winter groundswell runs in from the northwest and the tide is right. On those days it produces a heavy, ledging wave that the Irish big-wave community rates among the better spots on the coast. It isn't Mullaghmore and it doesn't get the same attention, which is partly why the people who surf it prefer it. You can watch from the headland. Bring binoculars in January.
The beach that shouldn't exist
Sand in the wrong place
The Burren is limestone. Limestone doesn't make beaches — it dissolves, it cracks, it produces pavement and dolmens and turloughs, but not sand. Fanore beach is an anomaly: a long strand tucked between the karst and the sea, built up from shell and Atlantic sediment over thousands of years. It's a good swimming beach in summer. Walk the tide line and the geology of the place — stone immediately west, sand underfoot, limestone above — sits slightly wrong in a way that you keep noticing.
Where the stone runs out
The Burren edge
The Burren plateau covers roughly 250 square kilometres of north Clare. Fanore is one of the few places where you can stand and see the limestone terminate — it comes off the hills to the east, runs across the coastal flat, and stops at the beach. The karst pavement above the village holds arctic-alpine plants that survived here since the last Ice Age, sheltered in the limestone grikes. The gentian flowers in May. Orchids appear in April. The Burren's reputation as a botanical oddity is most accessible here, fifteen minutes' walk from a pub.