The Niarbyl is composed of sandstones belonging to the Dalby Group of rocks. At Niarbyl Bay the Dalby Group meets the rocks of the Manx Group of mudstones in a dramatic fault line, which can clearly be seen at the bottom of the cliffs on the mainland. The Dalby Group came from the ancient continent of Laurentia, of which Scotland and North America are parts. The Manx Group came from the ancient continent of Gondwana, of which southern England and Africa are parts, so what is exposed at Niarbyl Bay is the meeting of two continents. The fault is the only remnant of the Iapetus Ocean, which once separated the two continents.
Looking south down the west coast of the Isle of Man
Base of The Niarbyl
Cottages at Niarbyl Bay from the island
Looking north east from The Niarbyl
Top of the island
Looking north east from the island
Looking south east from the top of The Niarbyl
Looking west towards The Niarbyl
The Niarbyl Fault - North America meets Africa
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