The region in the south-west of Lesser Caucasus includes the areas of Jabrayil, Fizuli, Khojavend, Aghdam, Khojaly, Tartar, Shusha, Khankendi. The relief is mainly mountaineous. The north part of Nagorno Karabakh economic- geographical region is north-east bottoms of the Karabakh range, south slopes of Murovdagh range ( the highest peak of Caucasus Gamish mountain (3724 m), the central, west ,and south parts are eastern slopes of Karabakh range (Gizgala mountain (2843 m), Girkhgiz (2827 m), Boyuk Kirs Mountain (2725 m), northern- east and east parts are west edges of Karabakh and Mil plains. It borders on Iran Islam Republic in the south and south-east. The Murovdagh and Karabakh ranges are divided into some side branches lowering towards Karabakh and Mil plains. In the result of break of ranges and their side branches with rivers there appeared deep and steep slopes. In the middle upland, in the areas, where river valleys expand, there are intermountain lowlands. The forests in the area are 187,7 thousan hectares. The relief of the area of Aghdam is mainly flat, partly mountainous. The maximal altitude is about 1365m. Jabrayil region is basically located on the sloping plain (Injechol, Geyan field). The climate of Jabrayil region is temperate semi-desert with dry summer and dry steppe climate in the south part, moderate hot with dry summer in the north. Mountain chestnut, chestnut and brown mountain forest soils are spread. The relief of Fizuli region is mostly sloping plain descending towards the Araz, it consists of low mountains in the west, gray and gray meadow, chestnut and light chestnut, mountain chestnut, mountain gray brown soils. The landscape of Tartar region, which is located on the west of Kura-Araz lowland, is flat inclined from west to east with a climate of temperate semi-desert, with dry winter and dry steppe climate. Mostly chestnut, gray , and gray meadow soils are spread here. In geological structure collateral tectonic elements of Caucasus Murovdagh, Karabakh, Aghdam antycliniorums and separating Toraghaychay and Khojavand synclinoriums take the main place. The arch of antyclinoriums consists of volcanic rocks of Middle Jurassic, remote wings of the arch, and the synclinal structures complicating them contains limestone of Upper Jurassic, volcanogenic and sedimentary rocks of Chalk. They are cut with intrusions at times. In the lower parts of plains and river valleys anthropogenic sediments are spread. In January, the average temperature is 2-0.50 C in plains and foothills, –4; -130 C in high mountains, in July correspondingly 25-260 C and 15-140 C. In high mountains annual rainfall is more than 800-900 mm. The peaks of Murovdagh range are snowy topped all year round from time to time. The main rivers are The Kura- its tributaries Tartar, Khachin, Gargar, and the Araz, its tributaries Kondelenchay, Guruchay, Gozluchay and others. At the same time, in these areas 4 types of mammals, 8 types of birds, 1 type of fish, 3 types of amphibians and reptiles, 8 types of insects, 27 types of plants, which are included in “The Red Book of Azerbaijan”, were protected.