Visočica is a mountain range in central Bosnia and Herzegovina. Geologically, Visočica is part of the Dinaric Alps and formed largely of secondary and tertiary sedimentary rock, mostly limestone and dolomite. Due to subterranean non-porous geological layers, the typical karst characteristics of the nearby Herzegovina mountains are relatively absent in Visočica, resulting in enough water sources, even at heights around 1500-1700 m. Springtime lakes, though, tend to dry out soon towards the summer. Some smaller streams source from these mountains as tributaries to its bordering rivers: the Ljuta in the east, the Rakitnica on its northern and western slopes and the Neretva towards the south.