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Preliminary survey of the continental dunes in South‐Eastern Morocco (Tafilalt, Morocco) Volume 14, issue 3, JUILLET-AOÛT-SEPTEMBRE 2003

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Authors
Laboratoire des formations superficielles (LFS), Sciences du climat, de l‘environnement, de l‘eau et du patrimoine [SCEEP], BP 509 Boutalamine, Faculté des sciences et techniques, Errachidia, Maroc <kabirouhotmail.com> Association oasis Ferkla pour l‘environnement et le patrimoine (AOFEP), N° 430 Tighdouine, 52300 Tinjdad, Maroc Ministère de l‘Aménagement du Territoire, de l‘Urbanisme, de l‘Habitat et de l‘Environnement, 52 000 Errachidia, Maroc Office régional de mise en valeur agricole de Tafilalt (ORMVA\TF), 52 000 Errachidia, Maroc Association de lutte contre la désertification et protection de l‘environnement, Jorf, Errachidia, Maroc

Launched within the framework of the national research Programme [PROTARS: Support Thematic Project for Scientific Research (P2T3\ 13)], this survey aims at gaining a better insight of the processes and mechanisms of sand accumulation in the Jorf area in South‐East Morocco and more precisely in the locality of El Kraïr. From November 13, 2000, we started collecting a set of observations and measurements during one year in a trial perimeter installed in the above mentioned area. They confirm the predominance of the active southern‐westerly winds, already announced in 1964. The sandy load is more important with forty centimetres from the top of the soil while a 15‐meter migration of the barkhanes towards the North‐East is recorded. Finally, it appears that the origin of sandy materials is diversified (local and remote).