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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.
Blanket Bogs Blanket bogs are found wherever there is high rainfall, which is typically in western Ireland and also in mountainous areas. They are called blanket bogs because of their appearance-from a distance they appear homogeneous and they hug the topography like a blanket. One of Ireland's most characteristic features is the bog. Covering 1,200,000 hectares (1/6th) of the island, Ireland contains more bog, relatively speaking, than any country in Europe except Finland. Across Europe, as well as in Ireland, bogs have been exploited in recent centuries as a source of fuel.