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Information Journal Paper

Title

LAND SLIDE HAZARD ZONATION IN THE NORTH OF TEHRAN BY USE OF GEOGRAPHIC INFORMATION SYSTEM (GIS)

Pages

  75-87

Abstract

LANDSLIDE in this study was surveyed by dividing the area into several equal regions which later were classified in terms of real risk resulted of sliding of strata. Such procedure which is accompanied with simplifying the effects and evaluation of instability agents led to providing the LANDSLIDE risk map of the area. In order to prepare this map, first data was gathered and effective parameters on instability were identified. Then this parameters including lithology of study area, slop of area, aspect of the slop, average annual rainfall, distance from faults and earthquake acceleration were processed in Arc GIS9.2 software and the quality parameters were quantified with each data layer divided into smaller classes. In the next stage, specific weights were assigned to each class and risk value of each parameter was determined. Finally, they were presented as a LANDSLIDE hazard map.

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    Cite

    APA: Copy

    SHARIF, MAHSA, OUROMEIHY, ALI, & ZARE, MEHDI. (2011). LAND SLIDE HAZARD ZONATION IN THE NORTH OF TEHRAN BY USE OF GEOGRAPHIC INFORMATION SYSTEM (GIS). JOURNAL OF THE EARTH, 6(21), 75-87. SID. https://sid.ir/paper/193052/en

    Vancouver: Copy

    SHARIF MAHSA, OUROMEIHY ALI, ZARE MEHDI. LAND SLIDE HAZARD ZONATION IN THE NORTH OF TEHRAN BY USE OF GEOGRAPHIC INFORMATION SYSTEM (GIS). JOURNAL OF THE EARTH[Internet]. 2011;6(21):75-87. Available from: https://sid.ir/paper/193052/en

    IEEE: Copy

    MAHSA SHARIF, ALI OUROMEIHY, and MEHDI ZARE, “LAND SLIDE HAZARD ZONATION IN THE NORTH OF TEHRAN BY USE OF GEOGRAPHIC INFORMATION SYSTEM (GIS),” JOURNAL OF THE EARTH, vol. 6, no. 21, pp. 75–87, 2011, [Online]. Available: https://sid.ir/paper/193052/en

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