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- W2316667047 abstract "Abstract. - On the calcareous Syrian coast, for the most part rocky but low, three different processes alternated several times during the Holocene : heavy sedimentation with prograding beaches ; mechanical erosion with receding coast and beach-rock formation ; organogenetic constructions (Vermetids) and biocorrosion. No less than three main aggradation phases occured (during the IVth millenium BC, lid millenium BC and medieval period) ; each of them can be correlated with an important alluvial discharge from the Lebanese and Syrian Wadis and rivers, removed by the South-North coastal drift and built into huge beaches. When the alluvial discharge diminished, former beach deposits were eroded by waves and currents, the coast receded and beach- rocks formed. Then biological and biochemical processes developed on the bed-rock and beach-rocks : Vermetid settled down and corrosion platforms developed. So, during the Holocene, the succession of several geomorphic processes occured, mainly linked to climatic oscillations, but probably also to anthropic factors. According to numerous 14C datings, the duration of each phase is about a millenium." @default.
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- W2316667047 date "1995-01-01" @default.
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- W2316667047 title "Rythmes et modalités de l'évolution du littoral syrien à l'Holocène (The evolution of Syrian coast in Holocene times : tempo and processes)" @default.
- W2316667047 doi "https://doi.org/10.3406/bagf.1995.1857" @default.
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