The geomorphologic development of Chahnimes

There are some unique geomorphic phenomenon in Iran that Clutes and Chahnimes can be considered among them. There are two theories published in books and articles about the development Chahnimes in Sistan-Baluchistan province, one of which relates its development to tectonic activities and the other attributes it to the process of water and wind. And there is still a lack of documented studies regarding accurate assessment of its development and they only suffice to general terms. Given the numerous uncertainties that exist in this area, a plan was designed to investigate how the development of this geomorphic phenomenon was performed. This plan limits the scope of this phenomenon by autopsy in Iran and Afghanistan and by relying on the analysis of form and process and utilizing remote sensing techniques and come to other findings, the result of which can be summarized as follows:The phenomenon of Chanimeh has 5 different models of developmental phenomenon out of which only one model is affected by flysch differential erosion of Zahedan and that happens to be on the developed heights and the rest of the water is in the aqueous medium and East Africa.
This rare phenomenon defines the general strategy for water supply in the region and is considered the only alternative storage of surface water and groundwater in the Hamoon area.