Gully erosion leading to shallow translational slide. High rainfall in the area leads to percolation of water, with development of local pore water pressure and loose cohesion. Excavation and toe cutting of moderate steep slope destabilized the natural s
Neethusree, K. J. and Suma, C. S, 2020. Macro-Scale (1:50,000) Landslide susceptibility mapping in Toposheet no. 83 C/12 and in parts of Toposheets nos. 83 D/5, 9, 13 & 14 in Dima Hasao, Cachar and Hailakandi districts of Assam, East Jaintia Hills distri
Wide openings/ cracks are present on the road and slope face due to gully erosion; it created worse situation of road structure. Hence immediate protections are to be taken in this particular area.
Narainchara grant slide
Narainchara grant
1. Tapping and channelling of springs or water source on upslope portion, and diversion of surface runoff away from the affected slope face. 2. Construction and timely maintenance of lined lined hillside drains 3.Toe support for the affected slope throug
This failure has occurred as a result of combined effect of several factors such as: 1. The affected slope comprises highly friable sandstone 2. Lose of toe support due to Extensive cut slope 3. Gully erosion 5.Toe erosion due to absence of proper concre