 Those deposits are abundant on the Antecki quarry.The most related to the shores, probably barrier-Lagoon and Delta depositional systems are clearly visible on the Smilów Quarry, where the exposure shows different lithofacies and strata, including fine-grained, white and light-grey Sandstones with Hummocky cross-stratification, with a series of tabular and trough Cross-bedding sets, probably related to nearmarine depositional subsystem.A more fine-medium-grained, grey to brownish sandstones also with flat-tabular-horizontal bedding with abundant drifted Plant Fossils and plant remains in situ is considered to be part of a clear foreshoreb–arrier–Eolian depositional subsystem, proabably related to a series of Dune fields, related to the Sea Barriers.