Abstract
A first study of the relative valves of the sea level in Provence over the last 5000 years, is based on the archeological facts and on new isotopic dates. On the eastern extremity of the Rhône Delta, the endogenous deformations (tectonic, tassements) play an important rôle. But the comparaison with the most stable sites of the War's seaboard shows equally the probable intervention of eustatic variations (protohistoric and antic regression ?). The study of a semi closed inlandsea (Etang de Berre) helps us to understand the history of the local climate.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
