Tectonic Geomorphology of Atrak River, NE Iran

Elahe Javadi Mosavi, Mehran Arian^*

Department of Geology, Science and Research Branch, Islamic Azad University, Tehran, Iran.

DOI: 10.4236/ojg.2015.53010                

Abstract

Atrak River region, northeast Iran is a quaternary tectonically active region. There are many geologic structures that they are formed by the collision of the Arabian and Eurasian plates. This area has extended from north east Iran to the of kope dagh zone. The study area is Atrak river basin and it has been divided to 56 Sub-basin for calculation of 6 geomorphic indices. Finally, this region was classified in 4 relative tectonic activity classes.

Keywords

Atrak, Kope Dagh, Geomorphology, River, Basin, Iran

Conflicts of Interest

The authors declare no conflicts of interest.

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