Lesser Caucasus
The Talysh Mountains are considered as a continuation of the Lesser Caucasus and followed by Paleogene and Neogene volcanic deposits. Furthermore, the southeastern part of the mountains composed of the Late Cretaceous deposits. Compared with the Greater and Lesser Caucasus glacial landforms are not particular in Talysh Mountains. The prominent ridges in Talysh Mountains are Talysh, Peshtasar, Dizgoni, and Burovar Ridges. The highest point is Kemyurkei Mountain with 2493 meters situated in Talysh Ridge. Northwest section composed of the middle and upper Miocene deposits.