Abstract
Abstract. - For the mediterranean regions, the Middle Quaternary is a period of tectonic activity on all the landscape's scales. Large bulges and buckles involve a relief, emphasized by the deep valleys and the terraced landforms. On a local scale, tectonic faulting, accompanied or not by sismic processes and forms, oppose the evolution of occidental and oriental mediterranean basins. Then different dynamical processes fashion the relief. For the more unstable regions, the processus of the "rhexistasie" continue, unaffected by the climatological rhythm of this quaternary period.
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