Megotsohe Chasie et al., 2016. Preparation of GIS-based landslide susceptibility Maps for mountainous region. Unpub. GSI report of FS 2014-2016.
Initially shallow translational to rotational, subsequently developed into debris flow on account of surcharge.
Approx. 255m ESE of Viswema
The flow of debris and its subsequent accumulation at the lower basal slopes has led to temporary blockage/damming of the stream course. This has in turn partially diverted the channel/nala flow and initiated debris slides on the right bank of the stream
Site specific studies may be required to ascertain the exact failure mechanisms for formulation of appropriate remedial measures. However, generic remedial measures may include: Provision of a contour drain at the crown and suitably diverting to a safer