Geography and Environment: It was formed within the Jura Lower Cretaceous limestones. As the limestones are not very thick; there is a shallow karstic surface in the region. It is a fossil cave which had been hydrologically abandoned. The ceiling is up to 1-8 m. It is adorned with stalactites; columns; stalagmites and wall dripstones; of which growths' were completely halted. At the bottom; there are debris and big blocks. It is a fossil cave; halted its geological development; and it is dry in all seasons. |