Abstract
The Vistula river valley near the city of Płock is characterized by the presence of a cascade of terraces, determining the circulation of water and matter. The relationship between the surface water of the Vistula river and the alluvial groundwater is discussed.
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References
Florek, E., W. Florek & E. Mycielska-Dowgiałło, 1987. Morphogenesis of the Vistula valley between Kępa Polska and Płock in the Late Glacial and Holocene. In L. Starkel (ed.), Evolution of the Vistula River Valley during the last 15000 years. Part II. Geographical Studies, Special Issue No. 4, Ossolineum, Wroclaw; 189-205.
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Wiśniewski, E., 1987. Evaluation of the Vistula valley between Warsaw and Płock Basins during the least 15000 years. In L. Starkel (ed.), Evolution of the Vistula river valley during the last 15 000 years. Part II. Geographical Studies, Special Issue No. 4, Ossolineum, Wroclaw: 171-187.
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© 1993 Springer Science+Business Media Dordrecht
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Bajkiewicz-Grabowska, E. (1993). Hydrological problems of the Vistula river valley near Płock. In: Hillbricht-Ilkowska, A., Pieczyńska, E. (eds) Nutrient Dynamics and Retention in Land/Water Ecotones of Lowland, Temperate Lakes and Rivers. Developments in Hydrobiology, vol 82. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-1602-2_19
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DOI: https://doi.org/10.1007/978-94-011-1602-2_19
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-4698-5
Online ISBN: 978-94-011-1602-2
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