Overturned bedding at Trevayne Point

Coastal traverse and geology from Waterwynch to Saundersfoot, Pembrokeshire

The high cliff of Trevayne Point is just to the north of Lodge Valley beach. The rocks here are mostly pale grey sandstones of the Namurian age 'Millstone Grit Series' which have been folded into a nearly concentric anticline (on the left side of the cliff), with a near vertical, slightly overturned northern limb visible in the centre and right-hand side of the photo.