 The Kur-Araz lowland joins to the Lankaran lowland by the Mughan and Salyan plains in the south.Several elevations such as, “gobu”, topographic shapes “chala” as well as river-formed lakes called “akhmaz” are typical for the lowland.The Talysh Mountains are considered as a continuation of the Lesser Caucasus and followed by Paleogene and Neogene volcanic deposits.