Landslide Hazard Assessment in the Onarchay Watershed of Meshkinshahr Using the (MABAC) Model

Document Type : Original Article

Authors

1 . Associate Professor, Department of Geography, Mohaghegh Ardabili University, Ardabil. Iran

2 Associate Professor, Department of Geography. , Mohaghegh Ardabili University, Ardabil Iran

3 Ph.D student in Geomorphology, Faculty of Social Sciences, University of Mohaghegh Ardabili,

Abstract

One of the most important forms of geomorphological processes on the Earth's surface is landslides. Landslides are dynamic processes that play a role in the change and evolution of slopes (Guzzetti et al., 2005:274). This phenomenon occurs due to the displacement of constituent materials on slopes; the result is the movement of a large mass of materials down the slopes (Maddi, 2009:77). The displacement of soil and rock masses on slopes originates from two external and internal factors.However, this phenomenon causes the formation and evolution of slopes in mountainous areas (Roering et al., 2005:655). But they cause damage or death to humans and also significant financial losses to mountainous areas, agricultural lands and facilities in that area such as communication roads and development sectors (Mohammadnia et al., 2018:115). In this context: (Maddadi et al., 2019), conducted a comparative evaluation of MABAC and CODAS multi-criteria decision-making in landslide risk zoning in Kausar County. (Yalcin, 2008), evaluated landslide areas in the Ardsin region of Turkey using the analytic hierarchy process and statistical index and weighting factor. Therefore, considering that no research has been conducted on landslides in the Onarchay region so far. Therefore, the purpose of this study is to investigate the various factors affecting the occurrence of landslides in the Onar Chay watershed of Meshkinshahr and to zoning the landslide risk using the (MABAC) model.

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Main Subjects

References

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History

  • Receive Date: 24 February 2025
  • Revise Date: 30 April 2025
  • Accept Date: 03 May 2025

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