Rainfall led to increase in saturation of slope material resting on steep slope with natural drainages, which eventually resulted in slope failure. Since the landslide is located far from any settlement and infrastructure, at present there is less to wor
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
The landslide is located on a slope with no elements at risk in the vicinity, therefore no remedial measures are suggested. Moreover, the landslide location is inaccessible, thus the data recorded are from afar and limited.
Likabali-Aalo road Slide 4
Likabali-Aalo road
No remedial measures are suggested since there are no elements at risk
. Steep slope gradient ii. Slope forming material is composed of fragile sandstone (weathered and fractured) intermixed with soil.