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- > Late Vistulian (= Weichselian) and Holocene aeolian phenomena in central and northern Europe (supprimer)
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Par Collection Par Auteur- KOZARSKI, S., (Editeur scientifique) (3)
- MANIKOWSKA, B. (1)
- MYCIELSKA-DOWGIAŁŁO, E. (1)
- CICHOSZ-KOSTECKA, A. (1)
- GOŹDZIK, J. (1)
- SCHWAN, J. (1)
- 1991 (3)
- Dune ; Déflation éolienne ; Eolien ; Fluviatile ; Minéraux lourds ; Paléo-environnement ; Paléosol ; Pologne ; Sédimentologie ; Tardiglaciaire (1)
- Dune ; Déflation éolienne ; Eolien ; Fluviatile ; Minéraux lourds ; Paléo-environnement ; Pologne ; Quaternaire ; Sédimentologie ; Tardiglaciaire (1)
- Dune ; Eolian deflation ; Eolian features ; Fluvial processes ; Heavy minerals ; Lateglacial ; Palaeo-environment ; Palaeosol ; Poland ; Sedimentology (1)
- Dune ; Eolian deflation ; Eolian features ; Fluvial processes ; Heavy minerals ; Lateglacial ; Palaeo-environment ; Poland ; Quaternary ; Sedimentology (1)
- Eolian features ; Holocene ; Netherlands (The) ; Palaeo-environment ; Quaternary ; Soil ; Soil moisture ; Stratigraphy (1)
- Eolien ; Holocène ; Humidité du sol ; Paléo-environnement ; Pays-Bas ; Quaternaire ; Sol ; Stratigraphie (1)
- Late Vistulian (= Weichselian) and Holocene aeolian phenomena in central and northern Europe (3)
- Late glacial aeolian processes in the light of sediment analysis from Kamion profile near Wyszogród (1)
- Palaeowetness indicators in a Weichselian Late Glacial to Holocene aeolian succession in the southwestern Netherlands (1)
- Sedimentological record of aeolian processes from the Upper Plenivistulian and the turn of Pleni- and Late Vistulian in Central Poland (1)
- Late glacial aeolian processes in the light of sediment analysis from Kamion profile near Wyszogród
- Analysis of sediments from the Kamion locality in the Vistula valley near Wyszogród was carried out in order to gain more information about the fluvial and predominantly aeolian environments of sedimentation and weathering. Basing upon
- of the fossil wetness features. This work refers to a large exposure near Ossendracht in the southwestern Netherlands.
- As a result of differences in the duration of aeolian processes, their effects in glaciated and non-glaciated areas are distinct. In the glaciated area, infrequent but large dune sets developed in or near the vast sand fields, in the non-glaciated