Abstract

The Himalayan region and hilly areas face severe challenges due to landslide occurrences during the rainy seasons in India, and the study area, i.e., the Rudraprayag district, is no exception. However, the landslide related database and research are still inadequate in these landslide-prone areas. The main purpose of this study is: (1) to prepare the multi-temporal landslide inventory map using geospatial platforms in the data-scarce environment; (2) to evaluate the landslide susceptibility map using weights of evidence (WoE) method in the Geographical Information System (GIS) environment at the district level; and (3) to provide a comprehensive understanding of recent developments, gaps, and future directions related to landslide inventory, susceptibility mapping, and risk assessment in the Indian context. Firstly, 293 landslides polygon were manually digitized using the BHUVAN (Indian earth observation visualization) and Google Earth® from 2011 to 2013. Secondly, a total of 14 landslide causative factors viz. geology, geomorphology, soil type, soil depth, slope angle, slope aspect, relative relief, distance to faults, distance to thrusts, distance to lineaments, distance to streams, distance to roads, land use/cover, and altitude zones were selected based on the previous study. Then, the WoE method was applied to assign the weights for each class of causative factors to obtain a landslide susceptibility map. Afterward, the final landslide susceptibility map was divided into five susceptibility classes (very high, high, medium, low, and very low classes). Later, the validation of the landslide susceptibility map was checked against randomly selected landslides using IDRISI SELVA 17.0 software. Our study results show that medium to very high landslide susceptibilities had occurred in the non-forest areas, mainly scrubland, pastureland, and barren land. The results show that medium to very high landslide susceptibilities areas are in the upper catchment areas of the Mandakini river and adjacent to the National Highways (107 and 07). The results also show that landslide susceptibility is high in high relative relief areas and shallow soil, near thrusts and faults, and on southeast, south, and west-facing steep slopes. The WoE method achieved a prediction accuracy of 85.7%, indicating good accuracy of the model. Thus, this landslide susceptibility map could help the local governments in landslide hazard mitigation, land use planning, and landscape protection.

Highlights

  • Landslides are among the most dangerous and frequently occurring natural hazards in many hilly or mountainous terrains, which often occur without warning and cause the loss of life and property

  • This study demonstrated the significant combined use of BHUVAN and Google Earth® to prepare multi-temporal landslides inventory to access landslide susceptibility map in the data-scarce environment in the Rudraprayag district

  • The weights of evidence (WoE) method achieved a prediction accuracy of 85.7%, indicating good accuracy of the model

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Summary

Introduction

Landslides are among the most dangerous and frequently occurring natural hazards in many hilly or mountainous terrains, which often occur without warning and cause the loss of life and property. The frequency and magnitude of landslides are further increasing due to climatic extremes in fragile hilly or mountainous areas. Despite this fact, many countries worldwide are facing large-scale human tragedies, material damages, and economic losses by landslide events [11,12,13]. It is essential to recognize that the spatial distribution, frequency, magnitude, and volume of landslides negatively impact the natural landscape. To mitigate the risk of landslide occurrences in unstable slopes and evaluate the short and long-term adverse effects of landslides on the natural landscape, an interdisciplinary approach is needed

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