Abstract
The Agadir Canyon is the largest submarine canyon on the Moroccan continental margin, and is a major conduit for turbidity currents transporting sediments from the Morocco Shelf to the Canary Basin (Wynn et al. 2000). The Agadir Canyon is about 200 km long, and extends from the shelf edge at 150m to the lower rise at 4,250 m (Fig. 1). Open image in new window Fig. 1. Location map of the study area on the Moroccan margin. Bathymetric contours in kilometres. The locations of the areas shown in Figs. 2 and 4 are indicated. Canyons shown as solid black lines
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