Hamedan-Sosangerd region, west Iran is a quaternary tectonically active region with 755 Km length. There are many geologic structures that they have formed by the collision of the Arabian and Eurasian plates. This area has extended from central Iranto the south of Zagros mountain. The study area is Karkheh river basin and it has divided to 35 Sub-basin for calculation of 6 geomorphic indices.Finally, this region were classified in 4 relative tectonic activity classes. Keywords: Hamedan, Sosangerd geomorphology, basin, class, Tectonic
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