Add to ORKGInvestigations carried out in the Vistula River valley in the vicinity of Magnuszew (middle course) have shown the complexity of distribution of flood facies deposits. The type of lithological profile as well as sorption properties depends on site location in distinguished morphogenetic zones of floodplain: (1) terrace zone of meandering Vistula reworked by contemporary flows, (2) erosion troughs, (3) alluvial fans (crevasses), (4) contemporary terrace
The Warta River near Poznań (West Poland) represents a meandering lowland river modified by hydro-en...
W artykule przedstawiono przegląd osadów powodziowych i biogenicznych zdeponowanych w dnie Doliny Do...
Abstract: Today’s fl ood events along the River Wieprza assume a quite characteristic course entail-...
Because of large amount of deposited material and the varied discharge of water, the Middle Vistula ...
The paper presents the results of morphometric, structural and granulometric analyses carried out on...
The influence of morphodynamics of individual river valley zones on the anthropogenically induced di...
Within the channel zone of the Middle Vistula River, elevations of the Holocene alluvial basement oc...
Research carried out by the authors’ team in the valleys of many rivers in the Polish Lowlands has s...
Geological and geochemical investigations were carried out in the floodplain of the Vistula River Va...
A distinct zonality as shown in the occurrence of trace elements accumulated in the flood facies of ...
The problem concerns the catastrophic flood flow caused by the breaking of the dam of the artificial...
The examined area is located in southern Poland on Silesian Upland. According to geomorphologic regi...
The aim of the study was to identify and assess the lithological features typical for alluvial sedim...
W artykule poruszono problematykę rozwoju współczesnych ruchów masowych w strefie krawędziowej dolin...
The aim of the research carried out in the upper Czarna Hańcza valley was to explore the characteris...
The Warta River near Poznań (West Poland) represents a meandering lowland river modified by hydro-en...
W artykule przedstawiono przegląd osadów powodziowych i biogenicznych zdeponowanych w dnie Doliny Do...
Abstract: Today’s fl ood events along the River Wieprza assume a quite characteristic course entail-...
Because of large amount of deposited material and the varied discharge of water, the Middle Vistula ...
The paper presents the results of morphometric, structural and granulometric analyses carried out on...
The influence of morphodynamics of individual river valley zones on the anthropogenically induced di...
Within the channel zone of the Middle Vistula River, elevations of the Holocene alluvial basement oc...
Research carried out by the authors’ team in the valleys of many rivers in the Polish Lowlands has s...
Geological and geochemical investigations were carried out in the floodplain of the Vistula River Va...
A distinct zonality as shown in the occurrence of trace elements accumulated in the flood facies of ...
The problem concerns the catastrophic flood flow caused by the breaking of the dam of the artificial...
The examined area is located in southern Poland on Silesian Upland. According to geomorphologic regi...
The aim of the study was to identify and assess the lithological features typical for alluvial sedim...
W artykule poruszono problematykę rozwoju współczesnych ruchów masowych w strefie krawędziowej dolin...
The aim of the research carried out in the upper Czarna Hańcza valley was to explore the characteris...
The Warta River near Poznań (West Poland) represents a meandering lowland river modified by hydro-en...
W artykule przedstawiono przegląd osadów powodziowych i biogenicznych zdeponowanych w dnie Doliny Do...
Abstract: Today’s fl ood events along the River Wieprza assume a quite characteristic course entail-...