Abstract
A field of sediment waves on the Llobregat River prodelta, Catalonia, Spain, is examined using high-resolution multibeam bathymetry and seismic reflection profiles. The sediment waves develop on the prodelta front on slope gradients between 3° and 0.2°, within the Late-Holocene highstand mud wedge. Their characteristics and the most likely process at the origin of these structures are evaluated.
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CITATION STYLE
Urgeles, R., De Mol, B., De Batist, M., & Hughes-Clarke, J. E. (2017). Holocene Muddy Bedforms on the Llobregat River Prodelta Wedge. In Atlas of Bedforms in the Western Mediterranean (pp. 101–106). Springer International Publishing. https://doi.org/10.1007/978-3-319-33940-5_17
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