Photo 20. Small scale folding in Ordovician turbidite sequences at Rhosneigr, southern Anglesey. Again, the rocks themselves were actually deposited in a submarine environment in the Lower Palaeozoic Welsh Basin, but were crumpled, folded and uplifted to their present location in the Late Silurian to Mid-Devonian
Photo 20. Small scale folding in Ordovician turbidite sequences at Rhosneigr, southern Anglesey. Again, the rocks themselves were actually deposited in a submarine environment in the Lower Palaeozoic Welsh Basin, but were crumpled, folded and uplifted to their present location in the Late Silurian to Mid-Devonian