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  • Morphometry and morphodynamics of the lower Vistula channel mesoforms
  • The objective of this study is to determine the morphometry and morphodynamics of the prevailing mesoforms of the lower Vistula channel, i.e. unsteady movement of load. In view of the fact that these forms are the resultant of load movement
  • Sediment transport and morphodynamics of the beach and nearshore zone near Egmond, The Netherlands
  • of the nearshore zone is focused on the generation and the migration of bars, and on the parametrization of the morphodynamics. - (AGD)
  • Beach cusp morphodynamics
  • a period of 6 days. The results obtained provide a clear insight into the morphodynamics of natural beach cusps.
  • Morphodynamics of intertidal bars in wave-dominated coastal settings - a review
  • The aims of this review are to identify the dominant morphodynamic processes governing intertidal bar systems and provide a conceptual framework with which these bars can be further investigated. It is the dominant importance of tidal water level
  • morphodynamics.
  • Aspects of sediment- and morphodynamics of subtidal deposits of the Oosterschelde (The Netherlands).
  • A morphodynamic model for beach gradients
  • A reconstruction of the morphodynamics of a creek channel on the basis of the graining of alluvia, Cooper Creek basin, Australia
  • The article presents the use of granulometric analysis for the reconstruction of the morphodynamics of an ephemeral stream channel in an arid climatic area. Five deposit facies were identified: bed load, chute, channel bar, natural levee and channel
  • -fill deposits. The first two types were attributed to the morphodynamic erosion zone, while the other three, to the accumulation zone. The course of morphogenetic events in the phase of the disappearance of the flood wave during the last water flow
  • in the studied creek is presented, describing the character of the transport and deposition of alluvia. The fundamental role of the morphodynamics channel zone of accumulation is stressed in the functioning of ephemeral streams during the retreat
  • A catenary approach to the study of gravel layers and tropical landscape morphodynamics
  • into the contemporary morphodynamics of the study areas, particularly the transfer, storage and removal of materials from the valley systems. Palaeoenvironmental indicators were also found that enable the landscape evolution of this region to be more fully understood.
  • Crustal dynamics and morphodynamics of the Western European Rift system
  • of the Leine graben. The morphodynamic implications of the extinct and active rifting are depicted.
  • Morphodynamics and climate controls of two aeolian blowouts on the northern Great Plains, Canada
  • This paper presents the results of a long-term investigation of 2 blowouts in southwestern Saskatchewan. The morphodynamics of the blowouts were determined from a ten-year study between 1994 and 2004. The AA. compare measurements of sediment
  • of the climate controls and morphodynamics of continental blowouts.
  • Fan morphodynamics and slope instability in the Mucone River basin (Sila Massif, southern Italy) : significance of weathering and role of land use changes
  • In order to assess the fan morphodynamics and the slope evolution in the temporal range 1955-1996, multi-year air-photo interpretation and field surveys concerning morphodynamic processes and vegetation cover features were carried out in the Mucone
  • Beach morphodynamics of an atlantic coast embayment: Runkerry Strand, County Antrim
  • Relations between morphodynamics and fractal dimension of relief in some study areas of Italy
  • Solute transport as an indicator of morphodynamic zonation in a postglacial environment, West Pomerania, Poland
  • of those waters reveal considerable differences in surface water properties in the catchment. Hydrological pathways in the slope system and their importance to the supply of solutes to the channel system provided a basis for distinguishing 4 morphodynamic
  • Eolian sand transport at the Belgian Coast : morphodynamic implications and use in coastal management
  • to which each factor influences the moving sand cloud has been examined. Field sampling was done using a new sand trap. The experimental results are compared with theoretical formulae and linked to coastal morphodynamics. A new sand fencing technique has
  • Secondary flow deflection in the lee of transverse dunes with implications for dune morphodynamics and migration
  • Measurements of lee-side airflow response from an extensive array of meteorological instruments combined with smoke and flow streamer visualization is used to examine the development and morphodynamic significance of the lee-side separation vortex
  • Links between vegetation and morphodynamics of high-mountain slopes in the Tatra Mountains
  • for each of the 5 types of morphodynamic unit identified.
  • Swash bar morphodynamics in the Danish Wadden Sea : sand bed oscillations and suspended sediment flux during an accretionary phase of the foreshore cycle
  • resuspension and transport and its contribution to this morphodynamic behaviour is also explored.
  • Mono- and polygenetic wind ripple types - microforms indicating the morphodynamics of desert sand dunes
  • Pediments in the Gongola Basin, NE-Nigeria, development and recents morphodynamics