EGU22-3853
https://doi.org/10.5194/egusphere-egu22-3853
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Landslide susceptibility mapping of Chitral, northwestern Pakistan using GIS

Said Mukhtar Ahmad
Said Mukhtar Ahmad
  • Quiad i Azam University Islamabad Pakistan, Department of Earth Sciences, Geology, Islamabad, Pakistan (mukhtargeo44@gmail.com)

Landslide susceptibility mapping of Chitral, northwestern Pakistan using GIS

Mukhtar S. Ahmad1, *, Mona Lisa1, Saad Khan2 Munawar Shah3

1Department of Earth Sciences, Quaid-I-Azam University, Islamabad 45320, Pakistan

2Bacha Khan University Charsadda, Pakistan

3Department of Space Science, Institute of Space Technology, 44000 Islamabad, Pakistan

1mukhtargeo44@gmail.com

1lisa_qau@yahoo.com

2saadkhan@bkuc.edu.pk

3shahmunawar1@gmail.com

*Corresponding author: mukhtargeo44@gmail.com

Abstract

Landslides are the most frequently occurring geohazard in rugged Himalayan mountainous terrains. They often cause significant loss to life and property, and therefore landslide susceptibility mapping (LSM) has become increasingly urgent and important. In this study, LSM is carried out in the Chitral district of the Hindukush region in northwestern Pakistan. Several Geographic Information System (GIS) based models (such as Analytical Hierarchy Process (AHP), weighted overlay) has been used to build landslide inventory and susceptibility maps. The study incorporated nine main factors (including human-induced parameters, such as distance from road; topographical parameters, such as slope, aspect, and landcover; geological parameters, such as lithology, distance to fault, seismicity; hydrological parameters, such as rainfall and distance to stream) to generate LSM, further classified in five classes, very high susceptibility zone, high, moderate, low, and very low susceptible zone. It is concluded that most of the landslides in the study area are the result of steep slopes of mountains, followed by precipitation and earthquake. Landslide in the form of rockfall is mostly due to the active seismicity of the Hindukush region. The predicted susceptible zones of landslide in the study area are in good agreement with the past landslide localities, which is an indication of the susceptibility mapping of landslides in the region.

How to cite: Ahmad, S. M.: Landslide susceptibility mapping of Chitral, northwestern Pakistan using GIS, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-3853, https://doi.org/10.5194/egusphere-egu22-3853, 2022.