A shallow translational debris slide occurred due to the adverse condition of SFM. Saturation of overburden and increase in pore pressure and loss of cohesion during rainfall causes material to slide No remedial measures can be suggested as no element at
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
NA
Pasighat-Yingkiong road Slide 13
NH-513
No element at risk where the landslide is located therefore no remedial measures can be suggested.More over the landslide location is inaccessible thus the data recorded are from a far and limited.
1.Adverse condition of rock mass consists of jointed and fractured parent rock mass along with splintery shale.2. Steep slope gradient.3.Drainage dissection on the affected slope.4.Toe erosion by Nala.