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The Burren is underlain by limestones of the Lower Carboniferous (Visean) period. The limestone formed as sediments in a tropical sea which covered most of Ireland approximately 350 million years ago.
The Burren is located along Irelandâs mid-Western coast, stretching across approximately 72,000 ha of north Clare and south Galway. The region extends from sea level to heights of just over 300m.