The slide is a shallow translational rock cum debris slide and retrogressive in nature caused due to extensive slope cut, day lighting of the weak slope forming material and development of local pore pressure due to incessant rainfall in highly jointed r
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 2016-52
The slide is basically a cut-slope failure. Numerous minor slides of this size have occurred along this road section creating inconvenience to the commuters. Landslide initiated on 22/05/2016
Jatinga-2
Jatinga, Haflong
1. Toe support for the day-lighted bedrock through construction of strong concrete retaining walls with provision of drain pipes. 
2. Construction of lined hill side drain.
3. Moderation of upslope angle.
1. Development of local pore pressure due to incessant rainfall in highly jointed rock along the discontinuity planes.
2. Extensive slope cut for construction of road, exposing the discontinuity planes in day-lighted condition which failed along the weak