Continuing the line of summits in a Southeasterly direction, the Bolkar Mountains are bounded by the Goksu river to the West and the Pozanti river to the East. The Northern parts of the mountain lie in Nigde province while the Southern peaks rise in Mersin province.
These mountains exhibit interesting geological characteristics. Made of sedimentary material such as limestone and dolomites, the range reveals excellent examples of nappes, or folds in the layers of rocks. There are vast formations of karst as well as landscapes that reveal the effects of glacier and water erosion. Despite this erosion, no real water network has developed on the mountains. Because of the sedimentary nature of the rocks, water is absorbed creating large areas of karst, such as Pozanti and Sekerpinari.
The highest peaks of the Bolkar are: Medetsiz (3524 m), Kesifdagi (3475 m), Koyunasagi (3426 m), Tahtakaya (3372 m) and Egerkaya (3347 m).
The Northern flank receives the most exposure to snow and glacier formation; it is nevertheless the best route for an ascent to the highest summits of the Bolkar.