The slide is a shallow translational debris slide which has been triggered due to rainfall coupled with extensive slope cut. The affected slope is predominantly composed of in-situ soil intermixed with parent rockmass, dissection of slope by drainages, o
Nair,V,Athira., Jamir, I., 2022, Remote Sensing based Macro-scale (1:50,000) landslide susceptibility mapping in Toposheets82L/16, 82P/1,2,3,4,5,6 ; 83I/13,14 & 83M/01 covering  parts of West Siang East Siang, Upper Siang, Dibang Valley and Lower Dibang
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Pasighat-Yingkiong road Slide 18
NH-513
ii. Construction of retaining wall for toe support
Slope material is predominantly composed of rockmass overlain by thin column of in-situ soil ,Illplanned modification of slope