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Information Journal Paper

Title

GEOMORPHOLOGY OF LATE PLEISTOCENE MOUNTAIN GLACIERS IN SHAH ALBORZ MOUNTAIN- WESTERN ALBORZ

Author(s)

KHOSHRAFTAR REZA | FARID MOJTAHEDI NIMA | ASADI OSKOEI EBRAHIM | NOROOZPOUR SHAHRE BIJARI KAMBIZ | Issue Writer Certificate 

Pages

  155-165

Abstract

 1-Intrudaction: One of the evidences of the Quaternary CLIMATE CHANGEs in Iran, are glacial topography in mountainous areas. Understanding glacier forms such as CIRQUES, as the accumulation of snow and ice sites and mountain glaciers supply, is very important in glacial geomorphology.

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  • Cite

    APA: Copy

    KHOSHRAFTAR, REZA, FARID MOJTAHEDI, NIMA, ASADI OSKOEI, EBRAHIM, & NOROOZPOUR SHAHRE BIJARI, KAMBIZ. (2016). GEOMORPHOLOGY OF LATE PLEISTOCENE MOUNTAIN GLACIERS IN SHAH ALBORZ MOUNTAIN- WESTERN ALBORZ. QUATERNARY JOURNAL OF IRAN, 2(2), 155-165. SID. https://sid.ir/paper/255906/en

    Vancouver: Copy

    KHOSHRAFTAR REZA, FARID MOJTAHEDI NIMA, ASADI OSKOEI EBRAHIM, NOROOZPOUR SHAHRE BIJARI KAMBIZ. GEOMORPHOLOGY OF LATE PLEISTOCENE MOUNTAIN GLACIERS IN SHAH ALBORZ MOUNTAIN- WESTERN ALBORZ. QUATERNARY JOURNAL OF IRAN[Internet]. 2016;2(2):155-165. Available from: https://sid.ir/paper/255906/en

    IEEE: Copy

    REZA KHOSHRAFTAR, NIMA FARID MOJTAHEDI, EBRAHIM ASADI OSKOEI, and KAMBIZ NOROOZPOUR SHAHRE BIJARI, “GEOMORPHOLOGY OF LATE PLEISTOCENE MOUNTAIN GLACIERS IN SHAH ALBORZ MOUNTAIN- WESTERN ALBORZ,” QUATERNARY JOURNAL OF IRAN, vol. 2, no. 2, pp. 155–165, 2016, [Online]. Available: https://sid.ir/paper/255906/en

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