Description
The uppermost (downstream of Samara) right-bank slope with typical landscape and geomorphological features of that riverine erosive ledge, which was named Kinelskikhyarov. The supporting section of the roof of the Upper Kazan deposits, among which red-colored mudstones and marls predominate. Their layers have melted and crumbled. Separate layers of red-colored sandstones, among them with a thickness of up to 1 m, already form the root outcrops. There are thin layers of whitish limestones. When driving on Bol. From top to bottom, this is the first (upper) point with significant geological information. Higher up the Bol. To Kinel, his right-bank pits are mostly all blackened.
The object is a natural monument of regional significance in the Orenburg region, which has a special protection regime. Information about prohibitions and restrictions can be found here.