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Par Collection Par Auteur- BÖSE, M., (Editeur scientifique) (3)
- KARUKÄPP, R. (1)
- KARCZEWSKI, A. (1)
- KRZYSZKOWSKI, D. (1)
- RAUKAS, A. (1)
- 1994 (3)
- Bilan de masse ; Déglaciation ; Géomorphologie ; Kame ; Lithologie ; Moraine ; Paléogéographie ; Pologne ; Variation climatique (1)
- Climatic variation ; Deglaciation ; Geomorphology ; Glacier mass balance ; Kame ; Lithology ; Moraine ; Palaeogeography ; Poland (1)
- Cold area ; Estonia ; Finland ; Glacial features ; Glacial tectonics ; Glaciation ; Lithuania ; Palaeogeography ; Quaternary ; Stratigraphy (1)
- Deglaciation ; Glacial features ; Glacial tectonics ; Moraine ; Palaeogeography ; Petrology ; Poland ; Stratigraphy (1)
- Déglaciation ; Glaciaire ; Glaciotectonique ; Moraine ; Paléogéographie ; Pologne ; Pétrologie ; Stratigraphie (1)
- Estonie ; Finlande ; Glaciaire ; Glaciation ; Glaciotectonique ; Lituanie ; Paléogéographie ; Quaternaire ; Stratigraphie ; Zone froide (1)
- conditions probably underwent a gradual change depending upon the stade of deglaciation (Dani-, Goti-, and Finiglacial). Flow tills and collpses of ice cavities were common in dead-ice areas, which is why organic layers with different ages often occur
- 1994
- zones. It is assumed that these specific features were influenced by the changing ice mass balance and by the substratum morphology.
- 1994
- , suggesting a re-advance. Petrological data suggest also a change of ice flow direction from north-south during the major advance to northeast-southwest during the readvance. Thus now, almost all marginal zones of the Late Weichselian glaciation in western
- 1994