A massive landslide measuring about 450-500 m (length) along a major hillslope drainage/ nala occurred on a slope predominantly composed of clay and pebble-cobble beds with minor occurrence of ferruginous sandstone. The recurrent landslide first occurred
Kikon, A., and Jamir, I., 2021: Remote sensing based macro-scale (1:50,000) landslide susceptibility mapping in Toposheets 78M/9, M/10, M/11, M/13, M/14, M/15, 83A/2, A/3, A/4, A/7, A/8, A/11, A/12, 83B/1, B/5 & B/9 covering  parts of Tawang, West Kameng
A recurrent landslide since 2015, .implementation of adequate mitigative measures is suggested.
Tippi Slide
NH 13/ Tippi
Systematic channeling of hillslope drainage for proper disposal of surface water runoff through construction of culvert.
1. SFM: slope material is predominantly composed of clay and pebble-cobble beds with minor occurrence of ferruginous sandstone. 2. Hillslope dissected by a major drainage. 3. Slope failure along the drainage during incessant and heavy rainfall.
