Decadal scale geomorphic changes and tributary confluences within the Ganga River valley in Varanasi region, Ganga Plain, India

Allahabad to Buxar, the Ganga River shows distorted menders, huge meander cut-offs, ox-bow lakes, scroll bars and abandoned linear channel belts, all suggesting to a fault system-related tectonic control on the river. The confluence dynamics of northern tributaries Gomati and Varuna Rivers which have shifted progressively from north to south, and confluences of southern tributary Jirgo which shifted from south to north, further corroborate the view and also suggest that the presence of a NE-SW trending dextral strike slip fault having a gravity component.