geomorphic study of saryghamesh river basin emphasis coincidence of drainage network with earth structure

sarygamesh basin one of the bulhary chay tributary take place in moghan plain, northeastern azarbyjan area in iran and south edge of kora- araz zone. aims of this research are study specificities and geomorphic evolution of sarygamesh basin, survey rivers work on structure and geologic formation, and corresponding hydrographic with earth structure. toward above aim is used to litologic, structural data, and water network data. the research method in this study are observer, filed, descriptive and library method. data and information of this research was assemblage by 1- topographic maps in order to primary identification and topographic analysis,2- geology maps for recognition of rocks and formations and geologic structure, 3-aerial photograph and satellite image for identify geomorphologic landforms. arc view and arc gis software used for drawing maps. this basin was belonging to three different structural zones in the names of crumpled allah yarlo-havai zone, volcanic plateau and moghan sedimentary basin. internal processes are created anticlines and synclines with eastern- western trend. process of external dynamic was impressed structural landforms and was created landform and different geomorphic phenomena. in some of area difference resistance of rocks was created reverse roughness in the basin for example hanging syncline. misadjusting of river network with earth structure is chiefly antecedence and crate cluse. erosion in the different forms was changing mountain landscape and changing forms of initial structural landforms. in the resent years atrophic erosion has justify important role in alteration of area landscape