 Within the soil profile developed in the old slide body pine trees were showing creeping which is indicative that the paleo slide was active. During heavy rainfall the overburden material got saturated and toe of the slide was cut by the nala which ulti
An Interim Report on Preliminary  Geological  Slope Stability Assessment of the Recent Disaster Affected Areas in Parts of Chamoli District, Uttarakhand by Bhupendra Singh, Bhupender Singh, Ajay Kumar and Arindam Roy, Senior Geologists, M-IV, NR GSI Dehr
UK_CHA_NH_ 036
Dhungwali (Near Karanparyag)
Boulder crate walls with deflection spurs, diversion of surface run off, breast wall with weep holes, retaining wall, proper filling and compaction of road.
Heavy rainfall in the area caused saturation of thick slope wash material and old slide debris, bank erosion caused by nala resulted in sinking of road.