Titlebook: Himalayan Neotectonics and Channel Evolution; Harendra Nath Bhattacharya,Soma Bhattacharya,Aznar Book 2022 The Editor(s) (if applicable) a

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Pillory

frozen-shoulder

Culmination

Role of Active Tectonism and Geomorphic Drivers on Channel Oscillation of the Raidak-I River in thek migration in association with erosion–deposition changes along the river Raidak-I using DSAS models. The present work intends to evaluate the relationship between the riverbank erosion–deposition and geomorphological and tectonic adjustment. For the study, earth observatory data like MSS, TM, ETM+

構(gòu)想

Morphotectonics of the Chel River Basin, Eastern Himalaya, India: Insights from Shuttle Radar Topogices to investigate the effects of neotectonics on channel characteristics and landform development. The individual and cumulative analysis of geomorphic indices such as Relief Ratio (Rh), Drainage basin asymmetry (Af), Stream length gradient index, Mountain front sinuosity, Basin Shape, Valley floo

情愛(ài)

,Influence of Neotectonics on Channel Evolution of Kameng River, North–East Himalaya,ware and derived information on the basin’s asymmetry factor, bearing of lineaments and streamlines and hypsometric variables. Information gathered from images and other secondary sources were processed using basin’s asymmetry factor (AF) and revised asymmetry factor (RAF), variance (R.) for bearing

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獨(dú)特性

GEAR

Flavouring

,Influence of Neotectonics on Channel Evolution of Kameng River, North–East Himalaya, of channel lines explained by bearing of tectonic lineaments, and hypsometric integral (HI) methods. We conclude that neotectonics caused the Kameng basin and its sub-basins tilted and channel links of the Kameng system are evolved following the fault, crack, and joint lines.