 The Lesser Caucasus Mountain is less high and has a folded-boulder structure caused by the presence of abyssal fractures of transversal and longitudinal striking.The prominent elevations are Murguz, Murovdagh, Shakhdagh, Garabagh, Eastern Goycha and Mykhtekyan.Shakhdagh ridge consists of volcanic rocks and Upper Cretaceous, Eocene carbonate, and consistent to the same-name syncline.