Like the Bozzhira tract, the Airakta Mountains were covered by the Tethys Ocean in ancient times. This is why the Mangyshlak peninsula is interesting, which was formed 25 million years ago as a result of a layer of the earth's crust that rose due to an earthquake. After that, the formation began to deviate to the west. Over time, the erosion of the Cretaceous rocks led to the formation of canyons, outliers, caves, and winds and precipitation completed this process. To this day, the landscape is changing. Presumably, after 5-7 thousand years, weathering will lead to the disappearance of the remnant mountains altogether, since their height decreases every year.