2013
DOI: 10.12691/aees-1-2-1
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Using Geographic Information System and Analytical Hierarchy Process in Landslide Hazard Zonation

Abstract: Nepal frequently suffers from various types of water induced disasters like soil erosion, landslide, debris flow, flood etc. To mitigate the problem related to Landslides & Debris flow, Landslide Hazard zonation is important to quick and safe mitigation measures and make strategic planning for the future by identifying the most vulnerable areas and channelizing most of the protective measures and techniques to a more focused area. This study was carried out in Rupa watershed area of kaski district with the mai… Show more

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Cited by 27 publications
(15 citation statements)
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“…Thulibesi phant in Armala, where 117 sinkhole spots were observed, is exposed to severe sinkhole hazards [55]. Sarangakot and Kaskikot within the Phewa watershed [56] and the Rupakot area of the Rupa watershed [57] are prone to landslide hazards. The Phewa Lake catchment area in Pokhara witnessed a shallow seated landslide due to extreme rainfall in 2007 [51].…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…Thulibesi phant in Armala, where 117 sinkhole spots were observed, is exposed to severe sinkhole hazards [55]. Sarangakot and Kaskikot within the Phewa watershed [56] and the Rupakot area of the Rupa watershed [57] are prone to landslide hazards. The Phewa Lake catchment area in Pokhara witnessed a shallow seated landslide due to extreme rainfall in 2007 [51].…”
Section: Introductionmentioning
confidence: 99%
“…A detailed geographical study of Pokhara, Kaski was carried out by Gurung in 1965 [66]. Yet, there are few studies have assessed the hazard risk scenario [54][55][56][57][58] and urbanization trends [67,68] of Pokhara City and the Seti watershed [8]. However, long-term time-series studies of urbanization and the hazard risk of the entire Kaski District is lacking.…”
Section: Introductionmentioning
confidence: 99%
“…Figure 5 represents the landslide inventory map of Panchase laid over the local MP/RMP. In past researches of landslide hazard zonation, the landslide density was found to be 0.44 per km 2 (Basnet et al, 2006) in the Phewa watershed and 0.571 per km 2 (Bhatt et al, 2013) in the Rupa watershed. These landslide densities were lower than that was found in the entire Panchase region.…”
Section: Landslide Inventory and Distributionmentioning
confidence: 97%
“…Most studies have concentrated on the detailed analysis of a single potentially destructive natural phenomenon: floods [ [12] , [13] , [14] ], landslides [ 15 , 16 ], and earthquakes [ 17 , 18 ]. However, a region is affected not only by a specific natural hazard but also by a series of geo-hazards.…”
Section: Introductionmentioning
confidence: 99%