Denizli Province, 18 km from Acıpayam District. 3 km. of the Dodurgalar District to the east. It is on the eastern slope of the Mallı Mountain in the west. There are many stalagmites, stalactites and columns in the cave. The cave, which developed within the Jurassic-Crtaceous limestones, which is extremely suitable for karst due to the abundant cracked structure of the cave, has an indented structure as it is divided into many interlocking islets with many dripstone columns.