 More recent studies suggest an environment of shallow seafront and beach, which of course does not exclude the presence of Aeolian zones there.Lithofacies on the Smilów Quarry shows slightly inclined Beach foresets and abundant Plant roots in a series of barrier/foreshore–ackshore–eolian dune facies, that include even plants buried in whole Dune, while drifted plant fossils and tree logs occur on the main depositional surface.This inclined surface exposes most likely a long period of non deposition and washed plants, recovering at the same time the original tilt of the local beach.