GIS-based landslide susceptibility mapping for the 2005 Kashmir earthquake region

• Published in: Geomorphology (Amsterdam, Netherlands) Vol. 101; no. 4; pp. 631 - 642
• Main Authors: Kamp, Ulrich, Growley, Benjamin J., Khattak, Ghazanfar A., Owen, Lewis A.
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 01.11.2008; Elsevier
• Subjects: Aster; Earth sciences; Earth, ocean, space; Earthquake; Engineering and environment geology. Geothermics; Exact sciences and technology; Geomorphology, landform evolution; GIS; Hazard; Himalaya; Landslides; Marine and continental quaternary; Natural hazards: prediction, damages, etc; Surficial geology; Susceptibility; Pakistan; Asia; Kashmir; Indian Peninsula; Himalayas; Jammu and Kashmir; Lesser Himalayas; India; Pakistan, Himalayas; Pakistan, Kashmir; GIS; Landslides; Earthquake; Susceptibility; Hazard; Himalaya; carbonate rocks; geographic information systems; slopes; earthquakes; faults; limestone; imagery; data bases; land cover; clastic rocks; rivers; shale; slates; roads; cartography; clastic sediments; carbonates; metamorphic rocks; forests; deforestation; sedimentary rocks; landslides; dolomite; landform evolution
• ISSN: 0169-555X; 1872-695X
• DOI: 10.1016/j.geomorph.2008.03.003

The M w 7.6 October 8, 2005 Kashmir earthquake triggered several thousand landslides throughout the Himalaya of northern Pakistan and India. These were concentrated in six different geomorphic–geologic–anthropogenic settings. A spatial database, which included 2252 landslides, was developed and analyzed using ASTER satellite imagery and geographical information system (GIS) technology. A multi-criterion evaluation was applied to determine the significance of event-controlling parameters in triggering the landslides. The parameters included lithology, faults, slope gradient, slope aspect, elevation, land cover, rivers and roads. The results showed four classes of landslide susceptibility. Furthermore, they indicated that lithology had the strongest influence on landsliding, particularly when the rock is highly fractured, such as in shale, slate, clastic sediments, and limestone and dolomite. Moreover, the proximity of the landslides to faults, rivers, and roads was also an important factor in helping to initiate failures. In addition, landslides occurred particularly in moderate elevations on south facing slopes. Shrub land, grassland, and also agricultural land were highly susceptible to failures, while forested slopes had few landslides. One-third of the study area was highly or very highly susceptible to future landsliding and requires immediate mitigation action. The rest of the region had a low or moderate susceptibility to landsliding and remains relatively stable. This study supports the view that (1) earthquake-triggered landslides are concentrated in specific zones associated with event-controlling parameters; and (2) in the western Himalaya deforestation and road construction contributed significantly to landsliding during and shortly after earthquakes.