was built by Sir Arthur Cotton in 1852. It got damaged in 1987 floods, and rebuilt as a barrage cum roadway soon after and named after him. The roadway connects Rajahmundry in East Godavari and Vijjeswaram in West Godavari. The irrigation canals of this barrage also form part of National Waterway 4. Hydro power stations The Godavari river in Maharashtra is one of the rivers whose water energy is least harnessed for generating hydro electricity. The 600 MW capacity Upper Indravati hydro power station is the biggest hydro power station which diverts Godavari River water to the Mahanadi River basin. The following is the list of hydro electric power stations excluding small and medium installations. Unutilized water Nearly 2490 tmcft of water has gone waste to the sea on average in a water year from 1 June 2003 to 31 May 2022 (19 years). The yearly water unutilized is given below Geology and sediment transfer in the Godavari Drainage Basin The primary and initial catchment of the Godavari drainage basin is largely represented by the basalt of the Deccan Volcanic Province (~50% of the total basin area). This is followed by the Precambrian granites and gneisses of the eastern Dharwar Craton, sandstones, shales and limestones of the Gondwana Supergroup, various sedimentary units of Cuddapah and Vindhyan basins, charnockites and khondalites of the Proterozoic Eastern Ghats Mobile Belt and the sandstones of the Rajahmundry Formation. The Godavari River carries the largest sediment load among the peninsular rivers and the majority of the mass transfer in Godavari occurs during the monsoon. Mineral magnetic studies of the Godavari River sediments suggest that the floodplains in the entire stretch of the river are characterized by a Deccan basalt source. The bed loads on the other hand are of sourced from local bedrock. Influx of Deccan source in the Godavari River up to the delta regions and possibly in the Bay of Bengal off the Godavari, therefore, can be related to the intensive chemical weathering in the Deccan basalts. Abrupt increase in δ13C values and decrease in TOC content accompanied with a significant increase in ferrimagnetic mineral concentration in Bay of Bengal sediments from ~3.2 to 3.1 cal. ka BP reflected a shift of organic carbon and sediment source and a severe decline in vegetation coverage. Such phenomena indicate intensified deforestation and soil/rock erosion in the Deccan Plateau producing higher ferrimagnetic mineral inputs, which is