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Morphodynamics of the stagnating Zwin inlet, the Netherlands
Bowman, D. (1993). Morphodynamics of the stagnating Zwin inlet, the Netherlands. Sediment. Geol. 84(1-4): 219-239. https://dx.doi.org/10.1016/0037-0738(93)90057-C
In: Sedimentary Geology. Elsevier: Tokyo; Oxford; New York; London; Amsterdam. ISSN 0037-0738; e-ISSN 1879-0968, more
Peer reviewed article  

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Keywords
    Belgium, Het Zwin natuurreservaat
    Physics > Mechanics > Dynamics
    Zwin [Marine Regions]
    Marine/Coastal; Brackish water

Author  Top 
  • Bowman, D.

Abstract
    This study investigates the morphodynamical characteristics of the Zwin inlet, Zeeland, southwest Netherlands. Data is based on field measurements of currents and their flow pattern recognition and on study of the intertidal bedform fields. Long-term bathymetric data and coastal monitoring by air photo interpretation were further applied for revealing the main morphological response in the inlet and along its adjacent beaches.Within the spatial segregation of flood- and ebb-dominated flows, seven bedform fields were defined with characteristic spatial organization and clear textural trends. The overall picture demonstrates a stagnating inlet with sand starvation along the Dutch coast and widening of the Belgian beach updrift. The Zwin inlet functions as a sedimentary trap, with its typical ebb-delta features displaced shorewards.

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