number of employees is Shaki-Ipek OJSC. Shaki is part of the Shaki-Zaqatala Economic Region. The Shaki region, one of the largest agricultural and industrial districts of the Republic, has a total area of 2.43 thousand km2 and a population of 184,172. At present 29 industrial enterprises operate in the region, of which 21 are small enterprises. Population Alternative according to the data of Lezgins ~ 40,000. Climate The annual sum of sunny hours is 2350 hours. Approximately 40 percent of sunny hours are observed in summer. The climate in Shaki is influenced by various air masses, cyclones and anticyclones, and local winds. The Arctic and mild air masses enter Shaki with causing the temperature rise in the winter. Mountain winds form local winds in Sheki in the summer. It is because of a contrast in pressure between the mountain and the valley. The cold winds are moderated by the Great Caucasus from the north. Thus, the temperature in Sheki is 0.5 C in January. The average annual temperature is 12 C in Sheki. The average temperature ranges from 20 to 25 C in June and August. In Sheki solid winds (over 15m / s) are hardly ever seen, with as 10–12 days a solid wind. Less than 1 meter per second the speed of the wind in Sheki is often observed. The average sum of rainfall is 730 mm. 50% of it falls in May, June, September and October. In Kish village the least precipitation is in August (35 mm), January (29 mm) and February (36 mm), 775 mm, over 1000 mm rainfall in Khan Lowland. Floods, storm, and hail are characteristic of the mountain and the fields encompassing Sheki and its urban places. The flood event is observed frequently. The Kish Waterway basin is located in the western portion of the city and it is considered one of the most powerful flood areas in the world. In the place called Guruchay were collected sand, stone, and mud from the mountains for a long time and its middle part is higher than the city Dodo settlement. The atmosphere events such as the storm and the hail have a great deal of effect here. High relief, strong heat in the summer and high evaporation are the essential reasons for hail in Shaki. The elevation of 500–850 m above sea level, the mountain woodlands encompassing it prevents the city from overheating. The