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Information Journal Paper

Title

THE GEOMORPHOLOGY STUDY OF BINALOUD BASIN

Pages

  258-265

Abstract

 Binaloud basin is located in the center of Khorasan-e Razavi province, namely between BINALOUD to the north and Central Iran geological zones to the south. It is influenced by tectonical and erosional factors. The controlling major and minor faults trend mainly NW- SE.  Due to rock type and tectonic activity, the studied area is a plain.  The existence of OPHIOLITE units caused that the main rivers are of subsequent type. Also due to lithological properties, the most drainage patterns are of dendritic type.  Binaloud basin includes two large subbasins, namely BAZ-E-HOUR and KAL-E-SIAH, each one consisting of various geomorphological phenomena. Those phenomena that have been identified in BAZ-E-HOUR and its subbasins (Qareh-Cheh) are landslide, badland, talus, rills and gullies. The last two features are responsible for transporting the most sediment into the basins, whereas in KAL-E-SIAH basin, mass movement and slumping are the main sediments. The geomorphic studies could help detailed identification of the sediment supply areas, and their transportation ways.

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  • Cite

    APA: Copy

    POURSOLTANI, M.R., MOUSAVI, S.M.J., & ALAMI, S.A.. (2010). THE GEOMORPHOLOGY STUDY OF BINALOUD BASIN. JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), 5(4), 258-265. SID. https://sid.ir/paper/127183/en

    Vancouver: Copy

    POURSOLTANI M.R., MOUSAVI S.M.J., ALAMI S.A.. THE GEOMORPHOLOGY STUDY OF BINALOUD BASIN. JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY)[Internet]. 2010;5(4):258-265. Available from: https://sid.ir/paper/127183/en

    IEEE: Copy

    M.R. POURSOLTANI, S.M.J. MOUSAVI, and S.A. ALAMI, “THE GEOMORPHOLOGY STUDY OF BINALOUD BASIN,” JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), vol. 5, no. 4, pp. 258–265, 2010, [Online]. Available: https://sid.ir/paper/127183/en

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