Streams or gullies which form along the slope should be channelized to avoid further seepage along the undisturbed slope. Several small failures are observed in the locality, therefore slope stability studies may be carried out to understand the causativ
Birchandrapara landslide
Subolsingh, Hezamara R.D. Block
Removal of the slide material from the scarp as well as the advancing material; Removal of load such as tall trees with penetrative roots and overhanging materials;  Diversion of surface runoff away from the affected slope by construction of hillside dra
The area shows a thick volume of highly weathered, loose and unconsolidated ferruginous sandstone with small clay pocket where modification of natural slope for construction of the house have been made without sufficient slope support. The incessant rain