 Starting with the shore prograding cycle, where the nearshore deposits show detailed Hummocky cross-stratification, at the time are covered by thin beach-welded facies showing irregular “massive” bedding and numerous Plant roots penetrating down from the undulated bounding surface.Superimposed are fine grained, very well sorted Sandstones with giant tabular Cross-bedding set interpreted as beach (Backshore depositional subsystem) Eolian Dune with complete Plant remains buried in the wind-transported Sand (Mostly, Herbaceous-Built Plants).The Direction of the Wind sedimentation is clearly visible on this deposits, where the stratification of the sand is well oriented.