Geotechnical investigation and landslide susceptibility assessment along the Neelum road: a case study from Lesser Himalayas, Pakistan
Arabian Journal of Geosciences, 2021
Globally, and in Pakistan, among natural hazards, landslides are considered one of the most dange... more Globally, and in Pakistan, among natural hazards, landslides are considered one of the most dangerous and frequently occurring events having devastating impacts on society and economy. The present study deals with the susceptibility mapping and detailed geological and geotechnical investigations on two large-scale landslides named Shahkot and Sandok, Lesser Himalayas, Pakistan. Inventory of 74 landslides was developed by SPOT-5 images and further classified in the field. The goodness of developed landslide susceptibility map was assessed by success rate curve (SRC) and prediction rate curve (PRC) which were 83.1% and 79.2%, respectively. Geotechnical investigations of selected landslides were carried out to identify the causative factors and landslide triggering mechanism. The Shahkot landslide is classified as complex (debris slide and slump failure), whereas the Sandok landslide is classified as rockslide. Laboratory testing, i.e., sieve analysis, Atterberg limits, specific gravity, and X-Ray Diffraction (XRD) analysis of the disturbed soil samples, reveal that the soils of Shahkot landslide are silty sand to clayey silty sand with plasticity index (PI) ranging from 2.05 to 14.96%. Petrographic studies showed that the schist and granite of the Shahkot and Sandok landslides contain quartz and feldspar with fair amounts of flaky minerals like chlorite, biotite, and muscovite. The XRD analysis showed mineral composition of quartz, muscovite, kaolinite, goethite, aragonite, hematite, plagioclase, siderite, montmorillonite, calcite, gypsum, orthoclase, dolomite, and illite. Intense jointing and fracturing in granite due to close proximity to faults imparts low unconfined compressive strength (UCS) values which holds the major cause of Sandok landslide beside other geomorphological and geological causes. The study depicts that drainage network, anthropogenic activities along steep slopes, fragile geology, active faults, freeze, and thaw action are influential parameters which significantly contribute to the landslide events.
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