The Manych () is a river in the Black Sea–Caspian Steppe of Southern Russia. It flows through the western and central part of the Kuma–Manych Depression. In ancient times, it was known as the Lik. A tributary of the Don, it is long, with its current source at the mouth of the Kalaus in the southwestern part of the Republic of Kalmykia. It flows through the town of Proletarsk and joins the Don in Manychskaya, east of the city of Rostov-on-Don. Along the Manych, going downstream, there are: Dam at at the mouth of the Kalaus River blocking flow eastward to East Manych Lysyy Liman Reservoir (Dam at ) in between these two dams A section that is almost dry Lake Manych-Gudilo Proletarsk (Proletarskoye) Reservoir (Пролетарское водохранилище) (Dam at , near the town of Proletarsk) Vesyolovskoye Reservoir (Весёловское водохранилище) (Dam at , near Vesyoly). Ust-Manych Reservoir near the river mouth (Усть-Манычское водохранилище) (Dam at ) The Proletarsk Dam is sufficiently high to raise the water level in Lake Manych-Gudilo upstream from it, so in fact the lake has become part of the Proletarsk Reservoir. The three reservoirs (and Lake Manych-Gudilo) form an almost continuous chain, the original course of the river being almost entirely flooded by them. According to the calculations of the Russian geographer Alexander Bazelyuk, between Manych-Gudilo and the river mouth, merely of the length of the West Manych river remains in its original "river" (rather than reservoir) form: from the Vesyolovsk Dam to the upper reaches of the Ust-Manych Reservoir, and from the Ust-Manych Dam to where the river joins the Don. Unusual drainage system Formerly, at least in periods of high water, the Manych River would flow in two directions. The river Kalaus, when reaching the Kuma–Manych Depression at , would split. About 30% of the water would become the West Manych and flow northwest to, or toward, the Don River. The remaining water became the East Manych and flowed roughly southeast and dried up on the steppe before reaching the Caspian Sea. Sometime around 1970 a low dam was built which prevented any water from flowing into the East Manych. The East Manych is now fed by irrigation canals coming from the Kuma and Terek Rivers. Canals Historically (prior to the construction of the dams and irrigation channels, i.e. until 1932–1940 for the West Manych, and until 1969 for the East Manych), both rivers were