Formation of thick laterite horizon and in between occurrence of saprolite layer. The saprolite layer is the main reason for the slide. Slide initiated since 2006 and reactivated 2019.
Reghu, R. and Senthilkumar, K., 2020. Macro-scale (1:50,000) Landslide susceptibility mapping in parts of Toposheet nos.Toposheets nos. 48O01, 48O05 and 48N08, Shimoga and Chikmagalur district, Karnataka. Unpublished GSI report.
Easing of the slope and construction of channel wall are recommended.
Mutturu-1
Mutturu-1
Easing of the slope and construction of channel wall are recommended.
Thick overburden material saturated and toe cut by the nala.