 Kaolinized grey Mudstones with abundant Dispersed plant roots are related to more lagoonal depositional subsystems.The slightly smaller and fine built, brownish and yellow Sandstones that show detailes Cross-bedding are related to a more alluvial deposition, proabablly from the influence of a local Channel.On the Main Smilów Quarry the dominant shoreface depositional subsystem show detailed marks of clear Palaeocurrent directions, dispersed trough Cross-bedding inclinations that point to the West.