Josep Maria Puig Lopez , John Howell

Rocky shorelines form where basement highs are eroded and flooded during marine transgressive events. Despite the Mesozoic North Sea rift generated numerous platform margins and rotated fault blocks which acted as basement highs, rocky shoreline deposits have not been previously reported. In the rock record rocky shoreline deposits are usually represented by thin conglomerates overlying major unconformities, and are typically characterised by their ichnological aspects, rather than their depositional facies. This study uses the sedimentological aspects of modern and Miocene rocky shoreline conglomerates from Spain and Austria, to create facies models which are then applied to the recognition of rocky shorelines in the Mesozoic of the Central North Sea. Our results demonstrate that structureless, clast-supported, poorly-to-moderately sorted conglomerate deposits are associated with competent basement lithologies, which produce hard, resistant coastal cliffs in areas associated with volcanic centres which were previously overlooked in the subsurface. The basement lithologies in most of the Central North Sea favoured the formation of smaller coastal cliffs, with less resistant lithologies that did not generate or preserve gravel size particles, precluding the preservation of Mesozoic rocky shores in much of the North Sea’s stratigraphic record.