The Tura (near the source also — Dolgaya) is a river in the Sverdlovsk and Tyumen Oblasts of Russia, a left tributary of the Tobol (basin of the Irtysh). It flows across the Tura Plain.

In 18th-century sources, G. F. Müller explained the origin of the hydronym from the Tatar tura — "city", referring to its location on the river of Chimgi-Tura. Modern hypotheses link the hydronym to the Ural-Altaic root "tur" — "watercourse, body of water", which passed into several Ugric and Turkic languages.

The length of the river is 1,030 kilometres (640 mi), and the drainage basin area is 80,400 square kilometres (31,000 sq mi). It is navigable for 635 km from its mouth. The elevation of the mouth is 42.2 m above sea level. The average annual discharge 184 km from the mouth is 202.7 cubic metres per second (7,160 cu ft/s).

It begins at an elevation of 370 m above sea level from the confluence of several streams 4 km southwest of the Khrebet-Uralsky railway station. Forest cover of the drainage basin is 51%; in its upper part, crystalline mountain rocks predominate, while in the lower reaches, sedimentary rocks are present.

In the upper reaches, the river valley is narrow with steep slopes, and the riverbed is rocky. In the lower reaches, the flow is smooth. The flow velocity is 2.0—2.5 m/s in the upper reaches and no more than 1.5 m/s in the lower reaches.

The Tura freezes in November and thaws mainly in the first half of April. In some years, ice break-up is accompanied by ice jams. The feeding is predominantly snow and rain. The flood period is prolonged (2.5 months) with a sharp rise in levels and a protracted decline. The range of water level fluctuations during the year is from 4 to 6.6 m.

As with many other rivers in the region, four phases are clearly distinguished in the river's water regime throughout the year:

Average monthly discharge (m³/s) of the Tura River at Tyumen (184 km from the mouth) from 1896 to 1998