“…Numerous geospatial technology-based studies have been conducted across the world, including in the United States on the four rivers of Olympic National park (East et al, 2017) , Taiwan on the Zhuoshui River and the Gaoping River (Kuo et al, 2017), Italy on the Scrivia river (Mandarino et al, 2020), Germany on the Old Rhine downstream (Arnaud et al, 2015), China on the lower yellow river (Kong et al, 2020;Guo et al, 2021) and the lower jingjiang reach (Yang et al, 2013), India on the Koshi river (Sinha et al, 2014), the Sharda river (Midha and Mathur, 2014), the Dwarkeswar river (Ghosh and Mukhopadhyay, 2021), the middle lower part of ganga , and the Ramganga river basin (Agnihotri et al, 2020), and Bangladesh on the lower padma river (Rashid, 2020; Nawfee et al, 2018;Halder et al, 2021), the rivers in southern estuarine Region (Islam et al, 2018), the Lower Meghna river (Mahmud et al, 2020), Madhumati river (Biswas et al, 2021), the lower Teesta river (Akhter et al, 2019), and the Brahmaputra river (Rashid et al, 2021). Lower sections of rivers regularly change course as a result of tectonic tilting, hydrological variability, and sedimentological readjustments (Agnihotri et al, 2020;Talukdar and Pal, 2017, Talukdar and Pal, 2018, Saha and Pal, 2019, Nawfee et al, 2018, Dewan et al, 2017 and the junction of the Ganga and Jamuna rivers is no exception (Rashid, 2020;Mahmud et al, 2020;Dewan et al, 2017). Any alterations, either natural or anthropogenic, might cause a shift away from dynamic equilibrium (Sinha et al, 2014;Dewan et al, 2017;Rashid et al, 2021;Mahmud et al, 2021).…”