k Folds in rock, Cemaes Head, Pembrokeshire, Wales, UK Folds in rock, Cemaes Head, Pembrokeshire, Wales, UK. A plunging anticline is exposed. These are the highest cliffs in Pembrokeshire, at over 175m in height. The contorted strata comprise Silurian and Ordovician sedimentary rocks and LlanvirnCaradoc black mudstone folded during the Acadian orogeny 400 million years ago. The boulder cove at the foot of the cliffs is Traeth Godi r Coch., by ANDY DAVIESSCIENCE PHOTO LIBRARY Stock Photo - Afloimages
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Folds in rock, Cemaes Head, Pembrokeshire, Wales, UK Folds in rock, Cemaes Head, Pembrokeshire, Wales, UK. A plunging anticline is exposed. These are the highest cliffs in Pembrokeshire, at over 175m in height. The contorted strata comprise Silurian and Ordovician sedimentary rocks and Llanvirn Caradoc black mudstone folded during the Acadian orogeny 400 million years ago. The boulder cove at the foot of the cliffs is Traeth Godi r Coch., by ANDY DAVIES SCIENCE PHOTO LIBRARY
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Folds in rock, Cemaes Head, Pembrokeshire, Wales, UK

Folds in rock, Cemaes Head, Pembrokeshire, Wales, UK. A plunging anticline is exposed. These are the highest cliffs in Pembrokeshire, at over 175m in height. The contorted strata comprise Silurian and Ordovician sedimentary rocks and Llanvirn-Caradoc black mudstone folded during the Acadian orogeny 400 million years ago. The boulder cove at the foot of the cliffs is Traeth Godi r Coch., by ANDY DAVIES/SCIENCE PHOTO LIBRARY

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