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To show the response of fluvial and torrential morphodynamics to climatic variations and neotectonics in the semi-arid mountains, the authors present a preliminary geomorphological study of the main geosystem of the Alyhnayn area. This level is located in the upstream part of the intramountainous valley of N'fis river belonging to the northern side of High-Atlas. Its geomorphological analysis, based on the distribution of alluvial deposits and their characterization, reveals an alluvial-fans/terrace system. The latter is formed by a surface modeled on glacis and lacerated by more or less deep ravines. It is arbitrarily attributed to the middle Quatemary age. The geometric and the morpholithostratigraphic analysis of its deposits show a local control of a sedimentation of fluvialtorrential and gravitational types. A complex slop deposit is embedded within the fluvial sequences. It can be explained by a drop of the base level related to neotectonics. The sedimentation process is caused by the reactivation of a preexisting fault in relation with the High-Atlas elevation. The evolution of the Quatemary morphogenesis of the Alhnayn area has been influenced by uplift and climatic changes. Neotectonics controls fluvial and torrential dynamics by the local morphostructural framework. The fluvial and afluvial fans environments responded differently to recorder impacts.  Nous présentons la réponse des paléoenvironnements ayant régi le géosysteme principal d7Alhanayn correspondant 2 un cycle morphoclimatique élémentaire, inscrit dans un domaine intramontagneux en cours de surrection, aux rythmes de l'érosion et de la sédimentation en caractérisant la part aux controles climatique et tectonique. Ce niveau se localise dans un segment amont de la vallée méridienne nord-atlasique drainée par l'oued N'fis. Son analyse géomorphologique met en évidence qu'il s'agit d'un systeme de cones-terrase modelé en sa surface en glacis lacéré par des ravins plus ou moins profonds. 11 est attribué arbitrairement au Quaternaire moyen. L'analyse géométrique et morpholithostratigraphique de ses dép6ts mettent en évidence un controle local de la sédimentation de type fluvio-torrentiel et gravitaire lié 2 la réactivation d'une faille préexistante en relation avec la surrection haut-atlasique

estudios geológicos

Enregistrements sedimentaires et controle tectonique dans la genese des archives morphosedimentaires quaternaires de la coupe d'alhnayn (Vallee Meridienne Du N'fis, Maroc)