River bank erosion along the Ganges in Malda and Murshidabad districts was 2.86 km. If Ganga/Padma actually merges with Bhagirathi due to the natural tendency, it will lead to flood and catastrophe in the entire Bhagirathi basin. Bhagirathi water remains at a higher elevation than the river Ganga/Padma during lean season and if they merge the water of the feeder canal will flow through Padma to Bangladesh defeating the very purpose of the Farakka Project." River bank erosion along the Ganges in Malda and Murshidabad districts River bank erosion along the Ganges in Malda and Murshidabad districts focusses on river bank erosion along the main channel of the Ganges in Malda
Adi Ganga Adi Ganga Adi Ganga, also known as Gobindapur Creek, Surman’s Nullah and Tolly’s Nullah, was the main flow of the Hooghly River from the 15th to 17th century but has subsequently virtually dried up. The earlier course of the lower Ganges as it flowed through the Bhagirathi channel was somewhat different from what its flow at the beginning of the 21st century. At Tribeni, near Bandel, it branched into three streams. The Saraswati flowed in a south-westerly direction, past Saptagram. The Jamuna (not the same river as in north India or many streams of that name in eastern Bengal) flowed