Titlebook: Quaternary Geomorphology in India; Case Studies from th Balai Chandra Das,Sandipan Ghosh,Aznarul Islam Book 2019 Springer International Pub

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EWER

Geophysical Control on the Channel Pattern Adjustment in the Kunur River Basin of Western Part of Lines make prominent deformation in longitudinal profile, planform index, channel geometry and other fluvial forms of Kunur River. High Transverse Topographic Symmetry Factor (TTSF) values (>0.40) around the fault lines and high Drainage Basin Asymmetry (AF-index) values (64.40) also positively reveal the neotectonic sensitivity over the basin.

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Cardiac-Output

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POLYP

Modes of Formation, Palaeogene to Early Quaternary Palaeogenesis and Geochronology of Laterites in acterization of various ferricretes, fossil records and OSL dating have emphasized on the primary and secondary origin of laterites in West Bengal. The primary laterites (Palaeogene to Neogene) are genetically related to parent rocks, viz., Rajmahal basalt and Gondwana sandstones, but the secondary

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,Microstructural Evidence of Palaeo-Coastal Landform from Westernmost Fringe of Lower Ganga–Brahmapuitic micro-features are also continuing through the changes of various hydro-meteorological components. The present chapter concentrates on the studies of deposited microstructure features in one of the lateritic pockets of Paschim Medinipur district, West Bengal. Few soil samples from Palaeo-coasta

Adrenaline

Imprints of Neo-tectonism in the Evolutionary Record Along the Course of Khari River in Damodar Fan, and meander form index (upper: −0.02, middle: −0.17 and lower: −0.13). We found this kind of meander behaviour to be correlated with the negative Bouguer anomaly (−45 to −30 m Gal) in the middle reach. Similarly, based on SRTM DEM (30 m), we detected a break in the long profile at the middle reach

ASTER

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