The heavy rainfall triggered the landslide by forming rills and gully and detaching and moving the calcrete blocks downslope. The slide material is spread on the road and calcrete block have rolled down upto the river bed.
Interim report on Preliminary Slope Stability Assessment of Recent Disaster Affected Areas of Bageshwar District, Uttarakhand by Manoj Kumar Kaistha, Sr. Geologist; Ravi Negi & Sebabrata Das, Geologists and P.V.S. Rawat, Superintending Geologist, M-IV, N
Calcrete rock blocks upto 3m dimension and debris
UK_BAG_PMGSY_93
Stone masonry breast wall of 2 m height with weep holes along the road in the landslide affected area.
Gully erosion.