The Julian and Tuvalian lithologic column in the Oslica area starts with dolomitic breccias with limonitic groundmass and with a bauxite giving evidence of areal expose on the boundary between Cordevolian and Julian. Afterwards. precepitation of carbonate rocks followed. In the lithological interval where the limestone breccias predominate. https://www.spidertattooz.com/LOOK-Trail-Fusion-Pedals-Platform-9-16-Blue/