Big rivers dominate the world's continental surface, yet we are still learning about how they
operate and whether they are explicably different, not only from each other, but also from …

River channel confluences are widely acknowledged as important geomorphological nodes
that control the downstream routing of water and sediment, and which are locations for the …

In an earlier book, The Geology of Fluvial Deposits (1996), I set out in detail modern
methods of facies and architectural analysis of fluvial deposits, and used numerous case …

Depositional models of braided rivers are necessary for rational interpretation of ancient
deposits, and to aid in the characterization of subsurface deposits (eg aquifers, hydrocarbon …

Ground penetrating radar (GPR) surveys of unit and compound braid bars in the sandy
South Saskatchewan River, Canada, are used to test the influential facies model for sandy …

Mid‐channel bars and their associated confluences are key morphodynamic nodes within
braided rivers, with past studies having investigated the morphodynamics of small natural …

Erosion of banks and channel migrations are usually common phenomenon and recurring
geo-hazardous problem in the Brahmaputra-Jamuna river system of Bangladesh. The …

River channel confluences are sites of significant hydraulic and morphological change
within fluvial networks (Richards, 1980; Rhoads, 1987; Ferguson et al., 2006; Biron and …

Bangladesh is dominated by three great rivers–the Brahmaputra-Jamuna, Ganga and
Meghna–that combine to feed sediment into one of the World's largest deltas in the Bay of …

Understanding the morphological erraticism for large braided river systems is still a
challenging issue in the present era of fluvial geomorphology. The present paper reports …