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2008
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tom nr 78
7-31
EN
Geomorphological and geological studies in the vicinity of a Neolithic stronghold at Osłonki in Kujawy region revealed such landforms as ground moraine, glacial trough, and biogenic plains. They were formed under the impact of direct accumulation of an ice-sheet, its meltwater, and biogenic accumulation. Detailed analyses of the relief and deposits using palaeobiological studies made it possible to reconstruct relief development and environmental changes in the Pleni-Vistulian, Late Vistulian and Holocene. The landscape from the times when prehistoric man occupied this area is presented.
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tom Vol. 16
124-127
EN
In the study the morphology of Noteć-Warta Parolina (streamway) in the vicinity of Osiek upon Noteć and lithology of floodplain nearby the archaeological site in Żuławka Mała are presented. The genesis of identified forms i also show. The attempt of the age determination of the flooded dune in floodplain biogenic deposits is given
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tom Vol. 16
133-138
EN
In the study the analysis of the Piła vicinity morphology are presented. Detailed remark was given on long, branchy glacial gully that runs form end morainic hills of Strączyn-Zawada oscillation to the south-west part of Piła. In the vicinity of Mały Puźnik Lake and Duży Kuźnik Lake the lithology with recognized and there was the thickness of biogenic deposits determined
7
Content available Litologia i struktura kemu w Podstolicach
63%
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tom 32
EN
The article shows the stratigraphic diversity of chosen geochemical features of peatbogs deposits that are adjacent to Lakes Kuźniczek, Kuźniczek Mały and Kuźniczek Duży in Kuźnik wildlife reserve. Palaeoecological analysis of accumulation biogenic basins depositscan enable reconstructions of main changes of habitat conditions during the nearest history. Analysis of deposits lithology and geochemistry make possible to define hydrological conditions indispensable to produce special genetic types.
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