On 14th June 2018 a debris flow was occurred at Kurumpoyil. This landslide initiated as planar failure at the contact between rock and overburden in the form of debris slide and then transformed in to debris flow. Excessive rainfall is the triggering fac
Kurumpoyil Landslide
Kurumpoyil  Vayalada road
Unscientific hill slope modification has to avoided
Landslide initiated as planar failure at the contact between rock and overburden in the form of debris slide and then transformed in to debris flow. Excessive rainfall is the triggering factor which resulted in the reduction of strength on saturation and