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Studies of mass movements are very important for understanding the geomorphologic evolution and identifying morphodynamic risk areas . The Baturite massif presents itself as the most significant wet hill of Ceara . Its average altitude is around 800m , and may have ridges above 1,000 m . From the geomorphologic point of view , there is a wide variety of features such as reliefs dissected on the hillsides, interspersed rolling hills with the deposition plains and surfaces of erosion and deposition in the lower surrounding areas . The distribution and characteristics of mass movements vary according to the properties of each area. M ass movements have been identified only in the areas with the most significant slopes , which are essentially found in uphills and in the plateau . In general , it was observed the occurrence of rotational and translational landslides associated with mud flows and falls . Considering the need to develop mappings aimed at identifying areas of morphodynamic susceptibility, methodological criteria involving the triggering agents using techniques of maps algebra were established . As a result , we identified areas with high susceptibility , in the western and southern hillsides and part of the eastern areas, with average susceptibility in other sectors of the uphill and low susceptibility in the surrounding areas .

Suscetibilidade à Ocorrência de Movimentos de Massa no Maciço de Baturité - Ceará, Brasil