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Akbulak river.

Rivers of the Tashkent region.

“Beauty is a manifestation of secret natural laws, which otherwise would have been hidden from us forever”

Johann Wolfgang von Goethe.

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Akbulak - the left inflow of the Chatkal River. In translation Akbulak - "A white spring". The source of the river Akbulak is in the Namangan region. The most part of the course is located in Bostanlyksky district of the Tashkent region of the Republic of Uzbekistan.
The river Akbulak begins in mountainous in the spurs of the Chatkal Range which are in the natural boundary Akbulak. Two lakes in sources have a drain in the summer, water from two others filters through surrounding lakes deposits and taluses.
Akbulak's valley was formed as a result of a tectonic break in a zone of development of Kumbelsky breaks of meridional pro-deleting. The river valley has the treelike drawing. In the lower current the valley of the river is twisting, with sharp excesses.
The right part of the valley is limited to the ridge Sargardon. In 1986 geologists described Akbulakskaya the lower carbon fabrics, a turneysky tier covering the left inflows of the Chatkal River. In Akbulak's upper courses (mid-mountain sites of the closed valleys, are closed from streams of damp air density of river valleys is low.
On average and the lower current Akbulak accepts a large number of water currents. The largest inflows are Tereklisay Serkelisay (the left inflow), Sargardonsay (the right inflow), Karaarchasay (the left inflow).