The landslide was basically a debris slide triggered by high anomalous rainfall, which got surcharged with run-off water and progressed into a debris flow. The flow of the debris was solely responsible for the destruction, damage and loss of lives and pr
Chasie M. &  Theophilus P.K., 2017: Updation of existing landslide inventory of North Eastern region based on the new incidences as and when occurs during the period, Unpubl. GSI progress report for FS 2016-24
Landslide occurred on 31st August 2016
Khasiapunji slide
Khasiapunji village
Remedial measures suggested at landslide site:
a. The loose debris material along the nalla course from crown to foot and into the run-out path must be cleared to restore the natural course of the stream. It is also suggested that run-out path is not put
From the field studies, a combination of factors has been interpreted to be involved in the
initiation and triggering of the landslide, which are:
a. 2-5m thick overburden resting on the slope got saturated during continuous, heavy rainfall and loses its