Volga Delta
The Volga Delta is the largest river delta in Europe and occurs where Europe's largest river system, the Volga River, drains into the Caspian Sea in Russia's Astrakhan Oblast, north-east of the republic of Kalmykia. The delta is located in the Caspian Depression—the far eastern part of the delta lies in Kazakhstan. The delta drains into the Caspian approximately downstream from the city of Astrakhan.
The Volga delta has grown significantly in the 20th century because of changes in the level of the Caspian Sea. In 1880, the delta had an area of. Today the Volga Delta covers an area of and is approximately across. It has a classical "delta pattern". The delta lies in the arid climate zone, characterized by very little rainfall. The region receives less than one inch of rainfall in January and July in normal years. Strong winds often sweep across the delta and form linear dunes. Along the front of the delta, one will find muddy sand shoals, mudflats, and coquina banks.
Three zones
The changing level of the Caspian Sea has resulted in three distinct zones in the delta.The higher areas of the first zone are known as "Baer's mounds," named after researcher Karl Ernst von Baer who worked in this region. These mounds are linear ridges of clayey sands, ranging from in height, and averaging about. They are between in length. Between the Baer's mounds are depressions that fill with water and become either fresh or saline bays; the height from the bottom of a depression to the peak of its neighboring mound ranges from. These depressions, called "", used to form part of the early, very deep river delta but gradually became separated from it. Because of their isolation from the fresh waters of the Volga, they are becoming increasingly saline. Together they form a "vast and extremely diverse area of western substeppe " which, because of the varying degrees of wetness and salinization, house a wealth of flora and fauna. The origin of these mounds and is still debated: the early suggestion that they were formed by aeolian action is now discredited, and now they are thought to have arisen either underwater or through river flow.
The second zone, in the delta proper, generally has very little relief, and is the site of active and abandoned water channels, small dunes and algal flats.
The third zone is composed of a broad platform extending up to offshore, and is the submarine part of the delta.