Landsliding in sedimentary terrains

Landsliding in sedimentary terrains


Marketed By :  LAP LAMBERT Academic Publishing   Sold By :  Kamal Books International  
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  • Product Description

Sedimentary terrains of the Sub-Himalayas (Siwaliks) were built up in the foothills by thrusting and uplifting of the foreland sediments. The Siwaliks are geologically young of Neogene Period. Several north-south flowing subsequent rivers have incised the foothills consequently removing lateral support of the river valley slopes, and contributing for landsliding. The Siwalik rocks are typically characterized by high contrast in stiffness between interbedded sandstone and mudstone or between well cemented conglomerate and mudstone. Differential weathering in sedimentary layers, and erosion of mudstone, and potential structural discontinuities in sandstones further aggravate landsliding in the sedimentary terrains. Thrusting along major tectonic lines and tilting of sedimentary layers are also important causes.

Product Specifications
SKU :COC41036
Country of ManufactureIndia
Product BrandLAP LAMBERT Academic Publishing
Product Packaging InfoBox
In The Box1 Piece
Product First Available On ClickOnCare.com2015-03-08
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