On 14th  June 2018, a debris flow occurred on the northern flank of Karinchola mala. The landslide initiated as deep rotational failure at the contact between rock and overburden in the form of debris slide and then transformed in to debris flow along tw
The slope forming material present near the crown area is soil and debris with a thickness of 0 to 0.5m and towards the downslope area it changes to soil, lithomarge and weathered rock with the thickness of the column increases up to 6m. The distressed m
Kalvari Landslide
Kattipara  Chamal road
Precarious boulders present in the debris flown path may be safely removed. Natural drainage path has to be maintained for avoiding water logged situation.
Landslide initiated as deep rotational failure at the contact between rock and overburden in the form of debris slide and then transformed in to debris flow along two runout chutes. Excessive rainfall is the triggering factor which resulted in the reduct