Morphology of the Ebro fan valleys from SeaMARC and sea beam profiles
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.
Citation Information
Publication Year | 1985 |
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Title | Morphology of the Ebro fan valleys from SeaMARC and sea beam profiles |
DOI | 10.1007/BF02281631 |
Authors | B. Alonso, K.A. Kastens, A. Maldonado, A. Malinverno, C.H. Nelson, S. O'Connell, A. Palanques, William B. F. Ryan |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Geo-Marine Letters |
Index ID | 70013038 |
Record Source | USGS Publications Warehouse |