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at its eastern end. The fault zone is thought to have been active as a normal fault throughout the deposition of the
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and forms part of the
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Dinas Island
Formation. The fault is exposed on the south side of
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125:(2 ed.). London: Geological Society. p. 64.
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65:List of geological faults of Wales
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29:Ordovician
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59:See also
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37:Caradoc
33:Ashgill
159:4°39′W
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
