Landslide Susceptibility Mapping of Tehri Reservoir Region Using Geospatial Approach

dc.contributor.authorTripathi, Gaurav
dc.contributor.authorShakya, Achala
dc.contributor.authorUpadhyay, Ritambhara Kumari
dc.contributor.authorSingh, Suraj Kumar
dc.contributor.authorKanga, Shruti
dc.contributor.authorPandey, Sandeep Kumar
dc.date.accessioned2024-01-21T10:51:53Z
dc.date.accessioned2024-08-14T06:47:34Z
dc.date.available2024-01-21T10:51:53Z
dc.date.available2024-08-14T06:47:34Z
dc.date.issued2023-03-10T00:00:00
dc.description.abstractUttarakhand is one of the most landslide-susceptible states because of its geographical setting, which consists of 86% of the Himalayan terrain. However, in recent years, landslides have increased dramatically due to the large number of settlements, farms, road buildings, and a wide variety of hydroelectric projects. Therefore, this is a need to study the landslides scrupulously at a regional scale to rein the future developmental planning models. In the current work, a comprehensive study has been undertaken for the assessment of landslide susceptibility zones using the weight of evidence (WOE) and risk assessment for the Tehri region, specifically around the Tehri reservoir. Landslides are derived through remotesensing techniques and other sources such as slope, geology, aspect, geomorphology, land use/land cover, drainage, lineaments, and more. After that, the WOE method is applied to integrate causative factors for the mapping of susceptible landslide zones, where the weights have been assigned to each layer according to available literatures. Subsequently, vulnerability is prepared for the area by integrating layers through the weighted sum technique. Finally, a risk map was prepared by integrating a susceptibility and vulnerability map. All three maps, namely, vulnerability, landslide susceptibility, and risk maps, were classified into five zones: very low, low, moderate, high, and very high. The results obtained from final maps and plots indicate that approximately 8% of the area is in a high susceptible zone, 50% is in a moderate susceptible zone, 54% is in a very low-risk zone, 23% is in a moderaterisk zone, and 14% is in a very high-risk zone. This study identified and illustrated the causative factors, combined into a GIS environment to identify landslide-prone locations. Then, depending upon the potency of an element, suitable and effective preventive measures may be taken to reduce the impact of the disaster. The concerned government agencies can use the same map while mapping disaster management, developing future strategies, implementing rehabilitation programs, and environmental planning. � The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerland AG 2023.en_US
dc.identifier.doi10.1007/978-3-031-24659-3_7
dc.identifier.isbn9783031246593
dc.identifier.isbn9783031246586
dc.identifier.urihttps://kr.cup.edu.in/handle/32116/4100
dc.identifier.urlhttps://link.springer.com/10.1007/978-3-031-24659-3_7
dc.language.isoen_USen_US
dc.publisherSpringer International Publishingen_US
dc.subjectGISen_US
dc.subjectLandslide Hazard Zonationen_US
dc.subjectRemote Sensingen_US
dc.subjectTehri Reservoiren_US
dc.subjectWeightsen_US
dc.titleLandslide Susceptibility Mapping of Tehri Reservoir Region Using Geospatial Approachen_US
dc.title.journalClimate Change Adaptation, Risk Management and Sustainable Practices in the Himalayaen_US
dc.typeBook chapteren_US
dc.type.accesstypeClosed Accessen_US

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