Third ridge of Crimean Mountains, Limestone ridge in Crimean Mountains, Ukraine.
The Third Ridge of the Crimean Mountains is a limestone formation in southern Crimea, Ukraine, running as the outermost of three parallel chains. It displays classic karst features such as caves, sinkholes, and underground drainage that shape the surface of the rock throughout its length.
The ridge formed from layers of marine sediment deposited over a very long span of time starting in the Jurassic period. The gradual compression and uplift of these layers produced the limestone surface that now shapes the land.
The passes through this ridge still connect the coastal zone with the inland areas, and local roads follow routes that have been used for a very long time. In some villages at the foot of the ridge, the names of springs and paths reflect this long relationship between people and the terrain.
Marked hiking trails cross the ridge and lead to viewpoints over the Black Sea and the northern steppes. The terrain is rocky and uneven, so sturdy footwear is a practical necessity before heading out.
The limestone acts as a natural filter, drawing rainwater down through cracks and storing it in underground pools far below the surface. In some spots along the ridge, this water reappears as springs that feed streams lower down in the valley.
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