Ibiza and Formentera, also known as the Pitiusas Islands, are the westernmost islands of the Balearic archipelago in the western Mediterranean Sea. Around them, typical temperate-water carbonate shelves occur. Particular sedimentary processes take place on these shelves, where the lack of a significant terrigenous sediment supply and a microtidal regime reinforces the importance of seagrass meadows and wind-driven coastal currents in the sediment dynamics. The dome dune field described here is placed just downslope of a centuries-old Posidonia oceanica meadow close to a shallow passage between two islands where wind-driven currents are particularly important.
CITATION STYLE
Rivera, J., Pomar, L., Hermida, N., Mateu, G., & Acosta, J. (2017). Dome Dunes on the Inner to Middle Shelf Transition on a Temperate-Water Carbonate Sediment Shelf. Pitiusas Islands. In Atlas of Bedforms in the Western Mediterranean (pp. 159–165). Springer International Publishing. https://doi.org/10.1007/978-3-319-33940-5_25
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