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Morphology of the Ebro fan valleys from SeaMARC and sea beam profiles

B. Alonso·K.A. Kastens·A. Maldonado·A. Malinverno·C.H. Nelson·S. O'Connell·A. Palanques·William B. F. Ryan
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Abstract

The northern continental slope off the Ebro Delta has a badland topography indicating major slope erosion and mass movement of material that deposits sediment into a ponded lobe. The southern slope has a low degree of mass movement activity and slope valleys feed channel levee-complexes on a steep continental rise. The last active fan valley is V-shaped with little meandering and its thalweg merges downstream with the Valencia Valley. The older and larger inactive channel-levee complex is smoother, U-shaped, and meanders more than the active fan valley. ?? 1985 Springer-Verlag New York Inc.

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B. Alonso, K.A. Kastens, A. Maldonado, A. Malinverno, C.H. Nelson, S. O'Connell, A. Palanques, William B. F. Ryan. 1985. Morphology of the Ebro fan valleys from SeaMARC and sea beam profiles. https://doi.org/10.1007/bf02281631

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