The population density was 266.7 inhabitants per square mile (103.0/km 2). Demographics 2010 censusĪs of the census of 2010, there were 208 people, 90 households, and 60 families living in the city. Other main branches of the Volga delta are the Bakhtemir, Kamyzyak, Staraya (Old) Volga, and Bolda.Volga is located at 42☄8′9″N 91☃2′26″W (42.802583, -91.540562) on the Volga River.Īccording to the United States Census Bureau, the city has a total area of 0.78 square miles (2.02 km 2), all land. Above Astrakhan a second distributary, the Buzan, marks the beginning of the Volga delta, which, with an area of more than 7,330 square miles, is the largest in Russia. A floodplain, characterized by numerous interconnecting channels and old cutoff courses and loops, lies between the Volga and the Akhtuba. (Between the Samara Bend and Volgograd it receives only the relatively small left-bank tributaries of the Samara, Bolshoy Irgiz, and Yeruslan.) Above Volgograd the Volga’s main distributary, the Akhtuba, branches southeastward to the Caspian Sea, running parallel to the main course of the river, which also turns southeast. From this point the Volga becomes a mighty river, which, save for a sharp loop at the Samara Bend, flows southwestward along the foot of the Volga Hills in the direction of Volgograd. At Kazan the river turns south into the reservoir at Samara, where it is joined from the left by its major tributary, the Kama. (Within this stretch the Kostroma, Unzha, and Oka rivers enter the Volga.) On its east-southeastward course from the confluence of the Oka to Kazan, the Volga doubles in size, receiving waters from the Sura and Sviyaga on its right bank and the Kerzhenets and Vetluga on its left. From the reservoir the river proceeds southeastward through a narrow, tree-lined valley between the Uglich Highlands to the south and the Danilov Upland and the Galich-Chukhlom Lowland to the north, continuing its course along the Unzha and the Balakhna lowlands to Nizhny Novgorod. Past the town of Rzhev, the Volga turns northeastward, is swelled by the inflow of the Vazuza and Tvertsa rivers at Tver (formerly Kalinin), and then continues to flow northeastward through the Rybinsk Reservoir, into which other rivers, such as the Mologa and the Sheksna, flow. It then passes through a chain of small lakes, receives the waters of the Selizharovka River, and then flows southeast through a terraced trench. The Volga is a small stream in its upper course through the Valdai Hills, becoming a true river only after the entrance of several of its tributaries. The course of the Volga is divided into three parts: the upper Volga (from its source to the confluence of the Oka), the middle Volga (from the confluence of the Oka to that of the Kama), and the lower Volga (from the confluence of the Kama to the mouth of the Volga itself).
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