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  • Fluvial geomorphodynamics in the Danube River valley and tributary river systems near Regensburg during the Upper Quaternary. Theses, questions and conclusions
  • This paper highlights the most important results of detailed investigations in the Danube River Valley, east of Regensburg. For the hydrological important characteristics of the different river systems, refernce is made to the original thesis
  • Sedimentology and geomorphology of overbank flows on meandering river floodplains
  • River drainage basin.
  • Floodplain development based on selective preservation of sediments, Squamish River, British Columbia
  • In this study an elemental approach is used to characterize the fluvial sedimentology of a 20 km reach of the Squamish River in which channel planform changes progressively downvalley from braided to meandering. A model of floodplain growth based
  • Holocene floodplain evolution of small rivers in the uplands of Lower Saxony, Germany
  • The Holocene floodplain evolution of the river Ilme and its distal tributaries in the uplands of Lower Saxony has been reconstructed by shallow corings arranged in cross and longitudinal profiles. The AA. differentiate three Holocene fluvial units
  • Holocene river and slope dynamics in the Black Forest and Upper Rhine Lowlands under the impact of man
  • The investigations on the Holocene river activities and slope dynamics in the Black Forest and Upper Rhine Lowlands were carried out with geomorphological mehods. They include the analysis of sediments, the radiocarbon dating of organic material
  • of changes on the river development, which were induced by man and/or climate since Neolithic ages.
  • The development of the middle and lower course of the Weser river during the Late Pleistocene
  • After the retreat of the glacier of the Drenthian-1 advance the Weser River cut a new path northwards to the Magdeburg-Bremen meltwater channel. The pebbles in gravel in samples taken from 99 boreholes up to 50 m deep were analyzed to distinguish
  • A 20 years investigation of central European rivers covering the Alpine foreland, the central upland and the northern lowland resulted in a system of the fluvial facies, the textures of fluviatile terrace bodies and different terrace patterns
  • . Synchronous phases of alternating increased fluvial activity and quiescence on major and smaller rivers give proof of climatic control over the fluvial rhytmicity. Despite regional and human modification, the natural imprints remain visible and dominating.
  • Temporal and spatial variation in dissolved and solid load years in partial catchment areas of the upper Leine river (southern Lower Saxony)
  • Sedimentary behavior of the alpine Ruetz River (Stubai Valley, Tyrol, Austria) in historical times
  • The present study characterizes the entire spatial variation in sedimentological properties along a portion of the presently aggrading floodplain of the Galena River in southwest Wisconsin. Another theme of this study is the detailed
  • Alps (The) ; Carrying capacity ; Fluvial processes ; Grain size distribution ; Italy ; Mountain ; River bed ; Sediment transport ; United Kingdom ; Wales
  • This paper presents a comparison of the pre- and post-late Holocene palaeo landsurfaces and paleochannels using data from the Nene, Soar and Severn valleys. From this comparison it is argued that during the mid to late Holocene floodplains and river
  • in an untamed mountain torrent. These results may be used to formulate a probability model describing the movement of single coarse particles on the river bed. The individual step lengths are best described by a two-parameter gamma distribution and the rest