Zonation of glaciomarginal environment inferred from pleistocene deposits of mysliborz lakeland, nw poland

What is it about?

In the Pomeranian glaciomarginal zone (especially between end moraine and outwash plain) of NW Poland, three subenvironments of sedimentation have been recognized, with a gradual transition from glacial ice-contact subenvironment through transitional subenvironment to glaciofluvial subenvironment. The present paper focuses on three subenvironments in a glaciomarginal environment (between end moraine and outwash plain). Sedimentological analysis is used to identify the main depositional processes and to reconstruct spatial and temporal changes in that sedimentary environment.

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