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Information Journal Paper

Title

ANALYSIS OF THE INTENSITY OF ALLUVIAL FANS HAZARDS IN SOUTH BINALUD BASED ON ACCEPTABILITY OF MORPHOTECTONIC INDICES

Pages

  24-25

Abstract

 Introduction: Alluvial fans are depositional landforms developed on a confined channel emerged from a drainage basin, i.e. between a mountain range and a plain. An alluvial fan is a fan- or cone-shaped deposit of sediments crossed and built up by streams. If a fan is built up by debris flows, it is properly called a debris cone or colluvial fan. These flows come from a single point source at the apex of the fan. They move to occupy the positions on the fan surface over time. The fans are typically found where a canyon draining mountainous terrain enter out onto a flatter plain, and especially along fault-bounded mountain fronts.

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    Cite

    APA: Copy

    SEPEHR, ADEL, & ABDOLLAHZADEH, ZAHRA. (2015). ANALYSIS OF THE INTENSITY OF ALLUVIAL FANS HAZARDS IN SOUTH BINALUD BASED ON ACCEPTABILITY OF MORPHOTECTONIC INDICES. PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, 47(1), 24-25. SID. https://sid.ir/paper/395245/en

    Vancouver: Copy

    SEPEHR ADEL, ABDOLLAHZADEH ZAHRA. ANALYSIS OF THE INTENSITY OF ALLUVIAL FANS HAZARDS IN SOUTH BINALUD BASED ON ACCEPTABILITY OF MORPHOTECTONIC INDICES. PHYSICAL GEOGRAPHY RESEARCH QUARTERLY[Internet]. 2015;47(1):24-25. Available from: https://sid.ir/paper/395245/en

    IEEE: Copy

    ADEL SEPEHR, and ZAHRA ABDOLLAHZADEH, “ANALYSIS OF THE INTENSITY OF ALLUVIAL FANS HAZARDS IN SOUTH BINALUD BASED ON ACCEPTABILITY OF MORPHOTECTONIC INDICES,” PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, vol. 47, no. 1, pp. 24–25, 2015, [Online]. Available: https://sid.ir/paper/395245/en

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