| Taldymanaka | |
| Other Name: | Талдыманақа |
| Source1: | Aktau Kazakh Uplands |
| Source1 Coordinates: | 47.8367°N 71.6778°W |
| Source1 Elevation: | ca 1100m (3,600feet) |
| Mouth: | Sarysu |
| Mouth Location: | near Mount Tokti |
| Mouth Coordinates: | 48.5139°N 70.9833°W |
| Mouth Elevation: | 434m (1,424feet) |
| Progression: | Sarysu→Telikol→Shieli-Telikol Canal→Syr Darya→Aral Sea |
| Subdivision Type1: | Country |
| Subdivision Name1: | Kazakhstan |
| Length: | 158km (98miles) |
| Discharge1 Avg: | 0.25m3/s |
| Basin Size: | 3950km2 |
| Pushpin Map: | Kazakhstan |
| Pushpin Map Caption: | Mouth location in Kazakhstan |
The Taldymanaka (Kazakh: Талдыманақа; Russian: Талдыманака) or Taldy-Manaka[1] is a river in Zhanaarka District, Ulytau Region, Kazakhstan.[2] [3] It has a length of and a drainage basin of 3950km2.[4]
This river is one of the most important tributaries of the Sarysu. The city of Zhanaarka is located 50km (30miles) to the ENE of the mouth of the Taldymanaka.[2] The water of the river is fresh upstream from the big bend. It is used for drinking purposes and watering livestock.
The Taldymanaka originates in springs of the southern slopes pf the Aktau massif of the Kazakh Uplands.[2] It heads northwards in its upper course as a mountain river within a 300m (1,000feet) to 400m (1,300feet) wide valley bound by steep cliffs. After it leaves the mountain area it flows within a floodplain among agricultural fields where a reservoir has been built recently. Further north it makes a wide bend northwestwards, westwards and southwestwards, heading then roughly westwards all along its lower course. In its last stretch the Taldymanaka flows again within a floodplain, where there are a number of salt lakes, especially to the south. Finally it joins the left bank of the Sarysu a little further upriver from the mouth of the Atasu.[4] [3] [5]
River Taldymanaka is fed mainly by snow and rainwater. Its highest level is usually in the spring with the melting of the snow in the steppe. By the summer it stops flowing, splitting into separate pools. Its main tributaries are the Zaimka, Uzen, Sulumanaka and Kokpekti.[5]
