The coast of Anse de Forlani bay, located 2 km northwest of Saint-Florent, offers three-dimensional outcrops of the East Tenda Shear Zone (ETSZ) mylonites. These light-colored quartz-chlorite schists show parallel and tightly spaced foliation planes that are folded for the most part. These can be described as asymmetric tight macro-crenulation folds. The chlorite indicates medium-grade metamorphism (MP/MT) in the greenschist facies. The shear bands and fold asymmetry indicate a top-to-the-east shear sense during these metamorphic conditions. This observation is in line with the west-directed exhumation of the Tenda Massif by the East Tenda Shear Zone.