Field photographs showing (A) micaceous silty marl of the Flysch de Mixe Formation with interbedded fine-grained Bouma-type turbidites; (B) serpentinized mantle rocks of the Urdach Member; (C) typical fresh lherzolite tectonic breccia in the Urdach area; (D) ophicalcite breccia made up of variably serpentinized lherzolite clasts in a calcitic matrix; (E) polymictic lherzolite-marble breccia made up of various types of high-temperature Mesozoic marble; (F) conglomerate of the Erretzu Member made up of centimeter-sized pebbles and subangular clasts.