The Kaplan Divlite cones formed during the latter phase of Kula volcanism.
The Kula Divlit Volcanic Park is located in the Kula-Salihli Geopark, northeast of the Kula district.
The Fairy chimneys in the Kula-Salihli Geopark have been formed by a combination of surface water erosion, splash erosion, and tunneling erosion (piping) in the soft layers.
Kula şehri, Türkiye'deki 18. yüzyıl Osmanlı kent mimarisinin en iyi korunan örneklerinden biridir.
This cone is one of the 80 volcanic cones in the area and one of the most spectacular parts of the volcanic landscape formed during the 4th phase of Kula volcanism around 25 thousand years ago.
The Adala volcanic canyon known also as “Hermos Canyon” extends for 5km between the Demirköprü Dam and the Adala municipality of Salihli Town.
Rocks from the Menderes Massif that have undergone metamorphism can be found in the area of Evciler Village.