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    Geological-tourist map of Pieniny National Park in scale 1: 25 000 is one of the 10 part series of maps, commissioned by the Ministry of Environment, a project financed by the NFEPandWM.

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    The data were obtained in the course of implementation of the “Geological map of the Baltic Sea bottom without Quaternary deposits 1:500 000”, which was developed by the Polish Geological Institute and published together with explanatory notes in 1999. The map shows the geological structure and morphology of the pre-Quaternary surface. It is complemented with geological cross-sections and seismic profiles. The map was based on new geophysical surveys using high resolution seismic reflection by which the geological structure of the area to a depth of several hundred meters was recognized.

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    Geological -tourist map of "Mierzeja Wiślana" Landscape Park in scale 1: 60 000 is one of the 5 part series of maps, commissioned by the Ministry of Environment, a project financed by the NFEPandWM

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    Geological -tourist map of Seaside Landscape Park in scale 1: 60 000 is one of the 5 part series of maps, commissioned by the Ministry of Environment, a project financed by the NFEPandWM.

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    Geological-tourist map of Gorce National Park in scale 1: 25 000 is one of the 10 part series of maps, commissioned by the Ministry of Environment, a project financed by the NFEPandWM.

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    Geological-tourist map of Ojcow National Park in scale 1: 25 000 is one of the 10 part series of maps, commissioned by the Ministry of Environment, a project financed by the NFEPandWM.

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    Geological-tourist map of Drawa National Park in scale 1: 40 000 is one of the 10 part series of maps, commissioned by the Ministry of Environment, a project financed by the NFEPandWM.

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    The GIS data were obtained during digitalisation the "Geological Map of Baltic Sea bottom of 1: 200 000" issued by the Polish Geological Institute in 1989-1995. The basic content of map includes lithological diversification of the southern Baltic surface sediments and their origin. In addition, if the surface layer has a thickness of less than about 20 cm, the underlying deposits are also shown. The basis of sediment types distinction was F. P. Shepard classification (triangles classification) using Wentworth grain classes. In classification applied sand is additionally divided into four subtypes. The map area is covered by 17 grain size types and subtypes of surface sediments.

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    Geological -tourist map of Romincka Primeval Forest Landscape Park in scale 1:40 000 is one of the 5 part series of maps, commissioned by the Ministry of Environment, a project financed by the NFEPandWM.

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    Data were derived from the study "Recognition and Visualisation of the Geological Structure of the Pomeranian Bay for Natural Resources Management", which was developed by the Polish Geological Institute and released in 2013. The aim of the study was more accurate than the previous recognition and visualization elements of the bottom morphology and the Cenozoic geological structure in the area of the Pomeranian Bay and the Polish part of the Oder Bank. The results are shown on geological maps at a scale of 1: 100 000 as well as on cross-sections and profiles. Analysis of data obtained from geophysical surveys, bottom soundings and laboratory analyses of the samples was the basis for verification of the prospects for aggregate deposits and valorisation of areas where they occur. The geochemical status of surface sediments was also determined and shown on the content maps of analyzed chemical elements.