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The Hel Peninsula (the Southern Baltic, Poland) is an unusual example of a barrier spit that enters and progrades into unusually deep waters. Here, we categorize and examine the underwater geomorphology of the barrier spit terminus using a combination of bathymetry, side-scan sonar, seismic profiling, and grab and core sampling. The morphology of the spit is characterized by a sigmoid profile, with...
The cliff in Ustka is an active one. The area is one of the most eroded sea shores of the Polish coast. The Ustka Cliff mainly consists of Holocene sandy deposits, but its basis is built of glacial till and clay. Field search allowed to recognize the structure and sedimentary conditions of Holocene deposits exposed in the cliff. A comparison of dating results obtained for fossil soils and peat as...
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