The paper gives an overall report on historical floods in the Sázava River Basin, focused on the pre-instrumental period in particular. The paper presents the first more detailed chronology of flood events on the Sázava River within the time limits
The Sazava river exhibits great discharge fluctuations with extreme dry periods. The great waterwithdrawal for water supply purposes from the Zelivka river, the main tributary, produces pollution and an unfavourable effect in the water regime
Morphostratigraphie des terrasses fluviales de la Sazava dans le Massif Bohémien
Cours d'eau ; Géomorphologie ; Massif ancien ; Morphostratigraphie ; Quaternaire ; Sazava ; Tchèque république ; Terrasse fluviatile ; Čechý
The results of geomorphological research into the Sázava river terraces are presented. This terrace system is characteristic by its variable structure which is conditioned by specific hydrodynamic processes that existed during the late Cenozoic
evolution of the river valley. Two levels of Neogene fluvial sediments and seven Quaternary terrace accumulations along the Sázava course are distinguished. - (EN)
The goal of this study was to assess impact of flood on soil and vegetation cover in the Sázava river floodplain after an extreme spring flood in 2006.There was a significant difference in species' composition between eroded sites and sites on thick
This article deals with channel bars, flood accumulations of floodplain and bank scours as the most important geomorphologic effects of the spring flood in Sázava River in 2006. The article deals particularly with its spatial distribution
Terrasses de rivière sur le cours inférieur de la rivière Sázava de Vrabčí Brod à Kamenný Přivoz
Cours d'eau ; Gravier ; Géomorphologie ; Stratigraphie ; Sázava ; Tchèque république ; Terrasse ; Čechý
A detailed geomorphological analysis of terraces. comparison to the terrace system of the Vltava River was exerted for the arrangement of the Sázava terraces into the stratigraphical chronology. Maps of river terraces and gravel deposits. - (MS)
Aspects de l'évolution de la haute vallée de la Sázava
We present some new hypotheses of the formation of the upmost course of the Sázava River in the studied region. Especially important is the orientation of Stržský Brook and the findings of lacustrine sediments in the Veselská Depression westwards
Fluvial sediments in the Vltava, Berounka, Sázava and Labe valleys are preserved as extensive river terrace sequences. These accumulation terraces originated from an interaction of climate-morphogenetic and neotectonic processes in the late Cenozoic
This article presents the results of a geomorphological analysis of localities of Quaternary river terraces along the Želivka River and its historical-genetic interpretation in light of the formation of the Sázava terrace system. In addition