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  • Cracow ; Dating ; Floodplain ; Fluvial deposit ; Fluvial processes ; Meander ; Palaeovalley ; Poland ; River bed ; Sedimentology ; Valley floor evolution ; Wisła
  • Flat-floored depressions without traces of paleomeanders occur frequently on the Vistula flood plain within the Sandomierz Basin. One of this, the Drwień depression extends along the southern Vistula valley side between Cracow and Niepołomice
  • . In the depression survived channel deposits laid down by the braided Vistula during the Late Glacial. In the western part the sandy-gravel deposits underlie a thin layer of peats in the eastern part the Younger Dryas and Preboreal channel deposits occur. Since
  • Late glacial and Holocene morphology and evolution of the Zapadnaya Beresina valley near Volozhin (Byelorussia)
  • Alluvial cone ; Belorussia ; Deforestation ; Floodplain ; Human impact ; Lateglacial ; Meander ; Palaeohydrology ; Quaternary ; Terrace ; Valley
  • The evolution of the Vistula river valley between Cracow and Niepołomice in late Vistulian and Holocene times
  • Evolution of the Vistula river valley during the last 15 000 years, part IV
  • Alluvium ; Climatic variation ; Drainage network ; Fluvial processes ; Holocene ; Human impact ; Poland ; Quaternary ; Sedimentology ; Valley ; Valley floor evolution ; Wisła
  • This is a new synthesis of the evolution of the section of the Vistula river valley. There are changes in the channel patterns and parameters, sedimentological characteristics of the different alluvial deposits of different ages, the reflection
  • of both climatic fluctuation and human activity in the valley floor morphology and in alluvia. - (DG)
  • Byelorussia ; Dating ; Floodplain ; Fluvial processes ; Geomorphogenesis ; Holocene ; Pleistocene ; Quaternary ; Stream ; Terrace ; Valley
  • . These changes were conditioned by a climate and established also in other valleys of East-European Lowland and in valleys of Poland. - (DG)
  • Cracow ; Floodplain ; Fluvial processes ; Geomorphogenesis ; Meander ; Poland ; Quaternary ; Valley ; Valley floor evolution ; Wisła
  • Climatic variation ; Cracow ; Fluvial processes ; Holocene ; Human impact ; Meander ; Paleogeomorphology ; Poland ; River bed ; Stream ; Valley ; Vegetation ; Wisła
  • New sites in the Vistula valley between Cracow and Niepołomice were discussed and 7 generations of Holocene meanders was distinguished, which cut off in 8 000, 6 700-6 200, 5 400-5 200, 4 400-4 000, 3 000, 2 200-2 100 BP and Little Ice Age. A clear