The study area comprises of insitu soil and fragmented sandstonesiltclay rocks. Cutting of slope for house construction on natural slopes and due to over saturation of weak overburden material during incessant rainfall are the main causative factors for
Kiso, E. and Tariq, Q. A. (2018); MacroScale (1:50,000) Landslide Susceptibility Mapping in Toposheet nos. 83G/5 and 83G/9 in Karbi Anglong, Dima Hasao and NGaon districts in Asam and Kohima District in  NGaland . GSI report of FS 201718.
The house is abandoned.
Dilaiji
DilaijiMon Terang road
1. Slope easing in the crown area. 2. Train/channelize the draiNGe away from the affected area. 3. Proper hillside drains may be adopted.
1. Poor slope forming material comprising of weathered ferruginous sandstonesiltstone (W4) and insitu soil. 2. Percolation of rain water/natural draiNGe within the weak material causing increase in pore water pressure.