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This study is based on a detailed mapping of a sector of the proximal part of the Atlantic continental shelf located to the south of Cap Spartel Morocco , by using a side-scan sonar SSS , complemented by sedimentological data from bibliographic sources. The SSS images show a complex mosaic of bedrocks and diverse submarine bedforms which are transverse and longitudinal to the dominant current flows. The morphological analysis suggests that tidal currents are the main active hydrodynamic agent controlling the development of the small-scale features.
Citations 2. References The NW termination of the Western Rif shelf also exhibits giant submarine dunes stacked at the entrance of the Strait of Gibraltar at water depths between and m Trentesaux et al. By using side-scan sonar, a recent study by Geawhari et al. Between Rabat and Essaouira, the continental shelf is 40 km wide, gently dipping 0.
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Full-text available. Nov Chapter 10 Recent sedimentation in the NW African shelf. Oct Mem Geol Soc Lond. A review of the data gathered over the last five decades on the NW African continental shelf within numerous research programmes shows that the sedimentary processes along the shelf are driven by long-term factors such as Quaternary glacial—interglacial periods and shelf morphology, and by short-term factors such as fluvial and aeolian sediment supply, local climate temperature, rainfall and wind and hydrodynamic conditions tides, swell, longshore current, the Canary Current and upwelling.
Based on the sedimentary characteristics, the margin has been subdivided into four segments: In this chapter, we present a synopsis of the state of knowledge on the NW African shelf sediments and processes based on various published and unpublished documents. Dec Oceanol Acta.
Influence of storms on tidal dune mobility in the Strait of Dover. The present paper deals with dune dynamics in a zone of the Strait of Dover located in the sea lane running into the North Sea. Single- and multibeam bathymetric data, coupled with seismic data, allow us to follow dune displacements over different time scales. A net bedload parting zone has been displayed and divides the area into two parts, SE and NW. However, according to the considered time-scale, dune movements present variations in intensity and direction. Over a long-term period decades , sedimentary dynamics fit the regional scheme of the residual tidal currents that induce transport toward the SW and the NE in the respective SE and NW parts of the studied area.