Landslide at Kalikhola village of Kangpokpi District, Manipur reactivated during early part of July, 2018 resulting damage of village foot track and blocked a nala (Kali Lok) resulting temporary dam structure creating a small lake. The area is represente
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 II (Old 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,  l
Presence of topographic break in slope, the steeper upslope part is represented by hard rock (Barails) and thick forest while the gentler lower part is represented by sparse vegetation and thin layer  of debris underlain by impermeable clayey layer. Rain