Anglesey, 2012 – Photo 6

Small scale folds developed parasitic to the Rhoscolyn antiform, SW Anglesey the folds are plunging towards the north. These folds are developed in interbedded psammites and pelites in the core of the Rhoscolyn structure and are a result of the rheology contrast between the two lithologies. Courtesy of John Conneally

Small scale folds developed parasitic to the Rhoscolyn antiform, SW Anglesey the folds are plunging towards the north. These folds are developed in interbedded psammites and pelites in the core of the Rhoscolyn structure and are a result of the rheology contrast between the two lithologies. Courtesy of John Conneally