106 Pleistocene skeletal eolianites (crossbeds dipping to the right) and reddish paleosoils in upper part of cliff while below is the Miocene reef core lithofacies closer to water line. The bedding dipping to the left represents the sigmoidal boundaries. Cliff is slightly oblique to depositional strike). Punta de Els Bancals, west of Cala Pi, south east coast of Mallorca, Spain (Kendall and Pomar, 2004).