A  successive  landslide  occurred  on  14th    June  2018  at Pulipparakunnu. The landslide initiated 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
Adjacent  to  this  landslide  another  landslide  with  similar properties was observed.
Pulipparakunnu Landslide
Mananthavady ΓÇô Niravilpuzha  road
Precarious boulders along the debris flow path have to be removed. The natural flow of water should not be blocked along the nala.
Landslide initiated 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 increase in pore