Third ridge of Crimean Mountains

This limestone ridge extends about 150 kilometers across southern Crimea, forming the outer section of three parallel mountain chains. The formation displays distinctive karst features including caves and sinkholes throughout its length.

This ridge formed through marine sediment deposits that accumulated from Jurassic times through to the Quaternary period. These layering processes created the limestone structures visible in the landscape today.

The passes through this ridge have served as crucial routes between coastal and inland regions for centuries. Local people and travelers still use these natural corridors to move between different parts of the territory.

Marked hiking trails cross the ridge and lead to viewpoints overlooking the Black Sea and northern steppes. The paths are generally accessible, though sturdy footwear is needed due to rocky terrain and uneven surfaces.

The limestone structure acts as a natural filtration system, channeling rainwater into underground lakes and water reservoirs. This geological feature makes the area notable for studying how water moves through karst landscapes.