The shallow rotational debris slide occurred due to steep slope angle with thick slope forming material led to slope instability and subsequently, slope failure due to oversaturation during heavy rainfall.
Ramesh Guguloth, Neethu Alpho Joseph, 2022, Remote Sensing based Macro-scale (1:50,000) landslide susceptibility mapping in Toposheets 83M/4, 8,12,15,16; 83N/01, 2, 5, 6, 9,13; 92A/03, 4, 6, 7, 11,14,15,16; 92E/02, 3 & 4 covering  parts of Tirap, Changan
NIL
1.5 km SE of Sanliam
Khonsa-Lazu road
1.Removal of debris material 2. Slope moderation.
Steep slope angle with thick slope forming material has led to slope instability and subsequently, slope failure due to oversaturation during heavy rainfall.