IDENTIFICATION, VALORISATION ET PROTECTION DES GÉOMORPHOSITES POUR LE DÉVELOPPEMENT DU GÉOTOURISME INTÉGRÉ DANS LA RÉGION D'ERRACHIDIA(MAROC)/Identification, valorization and protection of the geomorphosites for the developement of geo-eco-tourism integrated in the area of Errachidia (South-East) of Morocco

Tafilalet, circuit of the oases, are located at the South-East of Morocco corresponds to Wilaya of Draa-Tafilalet. It gathers the provinces : Midelt, Errachidia, Tinghir and Ouarzazate. The province of Errachidia, zone of study, contains in its administrative unit the following municipalities : Errachidia, Goulmima, Tinjdad, Erfoud, Errissani and Boudnib. The region of Errachidia, constitutes of the principal geomorphological entities of North to South : the carbonated Jurassic High-Atlas, the cretaceous bassin Boudnib-Ouarzazate with oases characteristic of this bioclimatic zone ressemblignthe « islands in the saharan desert » and the Anti-Atlasic chain dominated by a Précambrien basewich supports with its back a thick cover of the Paleozoic. In the tourist littérature of Morocco and many web sites nationals and internationals, refer to the gravitational landscapes in the Moroccan south among which geomorphosites ofthe province of Errachidia, considered by a very diversified geology, a very contrasted geomorphology offering superb landscapes carved by many meteoricerosive phases since the beginning of the Quaternary one strewn with serval endemicoases. Such is the primary reason of this research task from of point of view to promote geo-eco-tourism for the sustainable development of this area. Several tourist routes cross the zone of study. It presents two important routes such as the Amellagou-Tinjdad circuit and the Errachidia-Ettaous circuit. While liking it self of tourism of mountain of the High-Atlas of the rural communes of Amellagou and Aghbalou N'kerdous, we will review some summary aspects of natural sites of this presaharien field deserving guided tours in particular geomorphosites hydrogeologic and karstic, following the road curves of the Gheriswadi, appears on its side, a geomorphlogical landscape named « Asdram » of a distance from important observation offers a beautiful vision on the synclinorium infracenomanien. And while arrivingat the South of geomorphosites of the sedimentological type in particular the deposits of travertineuses layers meadows ofthe emergence ofthe sources. One proposess for this tourist way to make know a methodology of evaluation of the geosites recentlyused in the literature relating to the geological heritage in Switzerland, in Italy, in France and Romania following the many requests to share it with an aim of showing the wealth and the importance of the local geodiversity, methodology discusses the structure oft