مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

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مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

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Information Journal Paper

Title

ORIGIN OF SABALAN ROCK GLACIERS CASE STUDY OF ROCK GLACIER AT NORTH SLOPE OF HARAM SUMMIT

Pages

  12-17

Abstract

 Surface and internal characteristics of tongue-shaped GLACIER/fa?page=1&sort=1&ftyp=all&fgrp=all&fyrs=all" target="_blank">ROCK GLACIER have been studied at the north slope of Haram summit on interior SABALAN Mountain. The formation of surface depressions indicates the existence of a solid ice core, and its origin also is determined by using RILA concept. It is probable that a normal GLACIER has been buried beneath a cover debris. The vertical section of this GLACIER/fa?page=1&sort=1&ftyp=all&fgrp=all&fyrs=all" target="_blank">ROCK GLACIER shows three layers from bottom to top, and based on the dynamic criterion, the GLACIER/fa?page=1&sort=1&ftyp=all&fgrp=all&fyrs=all" target="_blank">ROCK GLACIER is an active one.

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    APA: Copy

    DALAL OUGHLI, A.. (2004). ORIGIN OF SABALAN ROCK GLACIERS CASE STUDY OF ROCK GLACIER AT NORTH SLOPE OF HARAM SUMMIT. GEOSCIENCES, 11(51-52), 12-17. SID. https://sid.ir/paper/31963/en

    Vancouver: Copy

    DALAL OUGHLI A.. ORIGIN OF SABALAN ROCK GLACIERS CASE STUDY OF ROCK GLACIER AT NORTH SLOPE OF HARAM SUMMIT. GEOSCIENCES[Internet]. 2004;11(51-52):12-17. Available from: https://sid.ir/paper/31963/en

    IEEE: Copy

    A. DALAL OUGHLI, “ORIGIN OF SABALAN ROCK GLACIERS CASE STUDY OF ROCK GLACIER AT NORTH SLOPE OF HARAM SUMMIT,” GEOSCIENCES, vol. 11, no. 51-52, pp. 12–17, 2004, [Online]. Available: https://sid.ir/paper/31963/en

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