The shallow translational debris slide formed due to intense weathering and erosion. Over long periods, daily temperature variations and extreme heat along with water flowing through fractures decomposes the bedrock. In addition, heavy downpour resulted
Neethusree, K. J. and Suma, C. S, 2020. Macro-Scale (1:50,000) Landslide susceptibility mapping in Toposheet no. 83 C/12 and in parts of Toposheets nos. 83 D/5, 9, 13 & 14 in Dima Hasao, Cachar and Hailakandi districts of Assam, East Jaintia Hills distri
One family is residing very close to the affected location. Evacuate and relocate the residents from the downslope area. (Mainly to be taken up by the respective state department.)
Bishnupur Puniyar Slide
Bishnupur Puniyar
1. Slope modification with benches supported by gabion wall/ 2.Covering the vulnerable slope by geosynthetic/ geotextile 3.Removal of debris and tress from the slope face 4. Natural flow should be channelized by construction of a chute drain.
1. Slope forming material comprising mainly of highly weathered sandstone and siltstone 2. Intense weathering and erosion has resulted the development of fractures on the slope face 4. Over long period, daylighting and water seepage condition through fra