The rocky outcrop of the Upper Cretaceous

This chalk ridge consists of white limestone layers that rise up to 25 meters, with vertical walls carved into finger-like shapes and small cave openings throughout. The formation sits within a small area of open steppe landscape.

These chalk layers formed during the Upper Cretaceous period, roughly 70 to 100 million years ago, when this region was covered by a shallow sea. The site gained protected status in 1972 to preserve this geological record.

The site holds interest for those curious about how chalk deposits formed and what they reveal about ancient times. Visitors can observe the geological layers directly and understand the natural processes that shaped this landscape.

Visit during drier months when the steppe roads are most passable and the ground is firm. Wear sturdy shoes and bring plenty of water, as the area sits fully exposed with no shelter from sun or wind.

The eastern edge displays steeply inclined white-gray walls that resemble the ruins of an ancient fortress carved into the bedrock. These striking shapes result from millions of years of natural erosion by water and wind.

Location: Donetsk Oblast

Inception: 1972

GPS coordinates: 48.65944,37.68472

Latest update: December 12, 2025 09:08