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Information Journal Paper

Title

THE FORM AND EVOLUTION GORGES OF THE MAKUAREA

Pages

  1-1

Abstract

 Maku area which is located in north west or Iran generally it is mountainous region. In this mountains currents of water flow ln N-S directions and continously the erosive activity change the land form during in ten million years. At the end of Eocene part or west is emerged, finally western mountains or Iran are shaped in the boundry line. In the late of Cenozoic period MAKU.area are effected by the most movement of organic at last the main physical features are founded. As result of this movement the central mountains gradually emerged, N-W to S-E respectively the Hawing this water eroded in these places as a result the GORGEs are appeared. These GORGE N-W to S-E are as follow: - The GORGE of Qara-su flows to the Bazergan plain. - The GORGE of ZANG-E-MAR enters in to Qateh-jog plain. - The S-W Fechal GORGE connected to the east part of MAKU. Sary-su GORGE in the DANALU and MAKU.em style="font-style:inherit;color:#ff0078"> GORGE in thc MAKU.city are created. In the northern mountain the QURISKAK and ADAGAN river break Hasun and Idali mountain, the GORGE of QURISKAK and ADAGAN are Shaped.

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  • Cite

    APA: Copy

    SAMADZADEH, R.. (2000). THE FORM AND EVOLUTION GORGES OF THE MAKUAREA. GEOGRAPHICAL RESEARCH QUARTERLY, 32(38), 1-1. SID. https://sid.ir/paper/5602/en

    Vancouver: Copy

    SAMADZADEH R.. THE FORM AND EVOLUTION GORGES OF THE MAKUAREA. GEOGRAPHICAL RESEARCH QUARTERLY[Internet]. 2000;32(38):1-1. Available from: https://sid.ir/paper/5602/en

    IEEE: Copy

    R. SAMADZADEH, “THE FORM AND EVOLUTION GORGES OF THE MAKUAREA,” GEOGRAPHICAL RESEARCH QUARTERLY, vol. 32, no. 38, pp. 1–1, 2000, [Online]. Available: https://sid.ir/paper/5602/en

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