Abstract
It was determined during the research that the relief of the zone is complex, very fragmented and the potential riskiness of erosion is higher. It was defined on the map that a main part of the Gobustan zone, i.e, 68,1% concentrated at an altitude of 500-800 meters. The areas of which surface inclination is more than 10 are 71, 3%. The potential riskiness of the erosion in the zone is very high. It was found that the depth of the local erosion basis is deeper than 50 meters and the most depth is 600-800 meters. It was determined that the south-east end of the Great Caucasus and the Gobustan zones are the most fragmented regions. Here the density of the ravine-gorge network is mainly more than 0,5 km at one kilometre.
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