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The Burren, located in County Clare, Ireland, formed primarily through a combination of geological processes and glaciation. It consists mainly of limestone that was deposited around 350 million years ago in a shallow sea. Subsequent glacial activity during the last Ice Age carved out the landscape, exposing the limestone and creating the region's characteristic karst features, such as limestone pavements, sinkholes, and unique ecosystems. Erosion and weathering have further shaped the landscape, resulting in the distinctive terrain seen today.
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