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Bat's Head, located on the Jurassic Coast in Dorset, England, was formed through a combination of geological processes including erosion, sedimentation, and tectonic activity. The area consists of limestone and other sedimentary rocks from the Jurassic period, which have been shaped by the action of the sea and weathering over millions of years. The distinctive cliffs and headlands, including Bat's Head, were carved out as softer rock eroded away, leaving behind the more resistant rock formations. This ongoing geological activity has resulted in the dramatic coastal landscape seen today.

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