Geoelectric sections shows talus deposit on top of clayey soil resting on volcanic substratum with shallow water table.

The cause of landslide in the study area could be the rainfall triggered down slope movement of the top talus deposits.

Lateral discontinuities such as cracks/fissures serve as secondary permeability and facilitates water seepage.

VES survey has given adequate insight into failure mechanisms and influencing factors of the landslide in the study area.