Skip to Main Content

The present study describes the coastal land and seafloor morphology of the Sinis Peninsula (West Sardinia, Italy). Based on the analysis of the wave motion hydrodynamic, the 7500 yr B.P. shoreline is outlined. The potential causes of the transportation of deposits, which have been reworked from aplitic dykes from the Mal di Ventre Islet to the central-southern coast of the peninsula, are investigated on the basis of 7500 yr B.P. seafloor wave motion transformations and relative field of velocity analysis.

You do not currently have access to this chapter.

Figures & Tables

Contents

References

Related

Citing Books via

Close Modal
This Feature Is Available To Subscribers Only

Sign In or Create an Account

Close Modal
Close Modal