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Dundawoona Point / Pointe an Dúin

Headland
Dundawoona Point / Pointe an Dúin
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What is recorded here

Dundawoona Point / Pointe an Dúin is a headland composed primarily of Silurian greywacke and volcanic rocks, formed around 440–420 million years ago during the Caledonian orogeny. The area is notable for its resistant rock formations that have withstood coastal erosion, contributing to the dramatic landscape of the Donegal coast.

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