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  • Last ice sheet dynamics and deglaciation in the North European Plain
  • Déglaciation ; Glaciaire ; Glaciotectonique ; Littoral ; Modèle ; Paléogéographie ; Pologne ; Stratigraphie
  • Coastal environment ; Deglaciation ; Glacial features ; Glacial tectonics ; Model ; Palaeogeography ; Poland ; Stratigraphy
  • the glacial dynamics during the Pomeranian phase in NW Poland, for which two different models exist. Investigations have been carried out at coastal cliffs east of Świnoujście, where it is possible to get good lithostratigraphic control of the Weichselian
  • A key problem when reconstructing the recession of the Weichselian ice sheet has been the difficulty of producing an acceptable glaciodynamic model for the southern Baltic Sea area. A recently started Polish-Swedish project aims at reconstructing
  • Last ice sheet dynamics and deglaciation in the North European Plain
  • Sedimentological investigations of the deposits show that the unit, the Simrishamn diamicton, is an in-situ glacioaquatic sediment. The aim of this study was to find out the origin and stratigraphic position of the unit as one part of a model
  • Last ice sheet dynamics and deglaciation in the North European Plain
  • Danemark ; Déglaciation ; Modèle ; Paléogéographie ; Quaternaire ; Radiation ; Variation climatique ; Vent ; Zone froide
  • Climatic variation ; Cold area ; Deglaciation ; Denmark ; Model ; Palaeogeography ; Quaternary ; Radiation ; Wind
  • Geomorphological, sedimentological and structural records of ice front dynamics during the Upper Plenivistulian: an example from the southeastern part of the Chelmno-Dobrzyń lakeland
  • Last ice sheet dynamics and deglaciation in the North European Plain
  • The dynamics of the last Scandinavian ice sheet in the territory of Poland displayed considerable variety. A 300 km2 study area near the maximum extent of the ice sheet was chosen to consider the landforms, the deposits and their internal structure
  • which developed during the positive, negative and steady-state ice balances. The main factors affecting the dynamics of the ice sheet at the time of its maximum extent and during the Kuyavian Subphase are also discussed.
  • Dynamics of the last ice sheet within the territory of Belarus
  • Last ice sheet dynamics and deglaciation in the North European Plain
  • Dynamics of the last Scandinavian ice-sheet and glaciodislocation metamorphism of unconsolidated deposits
  • Last ice sheet dynamics and deglaciation in the North European Plain
  • A new approach to Late Weichselian ice sheet dynamics in western Poland
  • Last ice sheet dynamics and deglaciation in the North European Plain
  • Last ice sheet dynamics and deglaciation in the North European Plain
  • was probably controlled by different dynamic zones in the ice-sheet during the first period of deglaciation.
  • Last ice sheet dynamics and deglaciation in the North European Plain
  • Last ice sheet dynamics and deglaciation in the North European Plain
  • Last ice sheet dynamics and deglaciation in the North European Plain
  • Last ice sheet dynamics and deglaciation in the North European Plain
  • Last ice sheet dynamics and deglaciation in the North European Plain
  • Last ice sheet dynamics and deglaciation in the North European Plain