The heavy precipitation event during 2012 initiated the formation of slide and got reactivated  during the monsoon rains of the 2013 too. A nala flows along the d/s margin of the slide and swerves along its toe and ultimately flows down in the Saryu rive
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
UK_BAG_PMGSY_65
Harsila on right bank of the Saryu River
Gabion wall all along the slope, lining of nala all along the slide zone
Saturation of the shallow debris material