Analyze of hydro-geoneurons of Ghezelozan basin

Geo-neurons analysis of Ghezel Ozan basin at the north west part of Iran by using the climatic statistics and information and Arc GIS, Surfer and excel soft wares has change to hydro-geo-neurotic analysis. In this article, for studying the neurotic system of drainage network, the hydrologic relations and climatic data were used. Whole of Ghezel Ozan basin, by considering its main tributaries , is divided into 56 sub basins. Topo-geo- neuron, immemorial geo-neuron and virtual geo-neurons, were identified in accordance with the structures of basin pattern and attrition surfaces. The results showed that about 3792 square kilometers, the solid precipitation in Quaternary glaciers blocked and in some other way have played a role in the transformation of heights. The dominant landforms of such a situation has been in form of glacier circus. At the downstream of such landforms, despite of appropriate slope, linear probing surface water has changed into glacier surface process and has created U-shaped glacial valleys and sometimes glacial act as the form of ice sheet and as general forms landforms that is named as virtual geo-neuron. The neurons of Yanki Kand and Qalah Chay has acted as isolated topo-geo-neuron by the climatic change of the region in Quaternary and melting of ice surfaces in middle of Ghezel Ozan basin. Zanjan Rood downstream, middle and along the Ghazal Ozan, of Bijar until Miyaneh is degenerative and amount of water they receive is much less than the water that comes out of them and if there exists no rivers such as Anguran Chay, Qalah Chay, Qranqon Chay, Ghezel Ozan were not , the river becomes dry completely