The Romadanovsky Ravine

Natural deposits of sands and white clays with some concretions of ferrous sandstone embedded into them come out to the day surface on the slopes and at the bottom of the ravine. In these concretions there are well-preserved prints of leaves from trees that grew in the Oligocene Period of the Cenozoic Age. The given finding made it possible for scientists to give more precise characteristics to the process of development of the earth crust in the region.
Address: Romadanovka Settlement, Meleuzovsky Region, Bashkortostan.