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- > Last ice sheet dynamics and deglaciation in the North European Plain (supprimer)
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Par Collection Par Auteur- BÖSE, M., (Editeur scientifique) (3)
- KARUKÄPP, R. (1)
- CHRISTIANSEN, H.H. (1)
- MARKS, L. (1)
- RAUKAS, A. (1)
- 1994 (3)
- Alluvial cone ; Dating ; Deglaciation ; Denmark ; Geographical information system ; Glacial features ; Nivation hollow ; Palaeogeography ; Periglacial features ; Thermoluminescence (1)
- Cold area ; Estonia ; Finland ; Glacial features ; Glacial tectonics ; Glaciation ; Lithuania ; Palaeogeography ; Quaternary ; Stratigraphy (1)
- Cône de déjection ; Danemark ; Datation ; Déglaciation ; Glaciaire ; Niche de nivation ; Paléogéographie ; Périglaciaire ; Système d'information géographique ; Thermoluminescence (1)
- Estonie ; Finlande ; Glaciaire ; Glaciation ; Glaciotectonique ; Lituanie ; Paléogéographie ; Quaternaire ; Stratigraphie ; Zone froide (1)
- Glaciaire ; Glaciation ; Glaciotectonique ; Moraine ; Paléogéographie ; Pologne ; Stratigraphie (1)
- Glacial features ; Glacial tectonics ; Glaciation ; Moraine ; Palaeogeography ; Poland ; Stratigraphy (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
- of varying size, often with numerous secondary forms. Active ice zones represent probable ice streams within the ice sheet, reflected by outwash plains and previous subglacial channels. Different sediments in each zone suggest a coincidence of dead-ice
- was probably controlled by different dynamic zones in the ice-sheet during the first period of deglaciation.