Mount Artos (Turkish: Çadır Dağı, lit.

Mount Artos rises to an elevation of 3,550 meters (11,647 feet) and is recognized as an extinct volcano.

The mountain's foundation consists of crystalline schists from the Paleozoic era, approximately 570-225 million years old.

Its geological composition includes schist and limestone, formed between the end of the Tertiary period and the Quaternary period around 2.5 million years ago.

The mountain's formation was accompanied by the development of surrounding valleys.