Landslide occurred at Kalikhola village of Kangpokpi District, Manipur during July, 2018 resulted damage of village foot track and blocked a nala (Kali Lok) at downslope with water logging forming a dam. The area is represented by NS trending alternate s
The entire Kalikhola is prone to landslide mainly because of inherent geological, topographical and landuse pattern. Thus, an appropriate watershed management and landuse management is urgently required.
Kalikhola Slide I (New Landslide)
Kalikhola village
Immediate  removal  of  debris  material  which  blocked  the  stream course for free flow of water. The newly developed nala (running along the middle part of the slide) be made functional clearing the debris material. Plantation  of  fast  growing,  la
Presence of topographic break in slope, the steeper upslope part is represented by harder rocks and thick forest while the gentler lower part is represented by sparse vegetation and thin layer of debris underlain by impermeable clayey layer; Rain water a