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

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SEPEHR ADEL; ABDOLLAHZADEH ZAHRA

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Journal: Physical Geography Research Year:2015 | Volume:47 | Issue:1 Page(s): 24-25

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Title

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

Author(s)

SEPEHR ADEL | ABDOLLAHZADEH ZAHRA | Issue Writer Certificate

Keywords

ACCEPTABILITY INDEXQ1

CENTRAL WEIGHT VECTORQ2

MORPHOTECTONICQ2

VULNERABILITYQ2

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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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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