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EN
The results of the geological interpretation of the seismoacoustic sediment profiling in an area of the Kepa Redlowska nearshore are presented. First, several seismoacoustic units were selected and then they were geologically interpreted. These were: Miocen muds (1), older till (2.1), marginal lake muds (2.2), younger till (2.3), sandy-gravelly, series (3) of water-glacial and river sediments (in an upper part also marine sediments) as well as contemporary sands (4) of a so called dynamic layer. A bathymetric scheme of the bottom and a morphological scheme of the lower surface floor bed of the sandy gravelly series (3 + 4) were worked out. Lateral and vertical successions of the selected units were analysed and their stratigraphic sequences were determined
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