Aqsu (Buchtarma)
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Aqsu Ақсу |
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| Data | ||
| location | Audany Katonqaraghai in East Kazakhstan ( Kazakhstan ) | |
| River system | If | |
| Drain over | Buchtarma → Irtysh → Ob → Arctic Ocean | |
| source | on the southern slope of the Qysylqaraghai 49 ° 30 '35 " N , 86 ° 8' 26" E |
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| Source height | approx. 1900 m | |
| muzzle |
Buchtarma coordinates: 49 ° 16 ′ 58 " N , 85 ° 17 ′ 45" E 49 ° 16 ′ 58 " N , 85 ° 17 ′ 45" E |
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| Mouth height | 664 m | |
| Height difference | approx. 1236 m | |
| Bottom slope | approx. 17 ‰ | |
| length | 71 km | |
| Catchment area | 1130 km² | |
| Discharge at the Aqsu A Eo gauge : 945 km² Location: 15 km above the mouth |
MQ 1954/1987 Mq 1954/1987 |
16.77 m³ / s 17.7 l / (s km²) |
| Flowing lakes | Maraly | |
| Communities | Aqsu | |
The Aqsu ( Kazakh Ақсу ; Russian Белая Belaja - "White River") is a right tributary of the Buchtarma in East Kazakhstan in the central Altai .
The Aqsu rises on the southern slope of the Qysylqaraghai (Russian Listwjaga ). In the upper and middle reaches it flows mainly in a westerly direction through the mountains. In the lower reaches it turns to the southwest and flows through the settlement of the same name Aqsu (until 2009 Белое Beloje ). Then it flows another 15 km to its confluence with the Buchtarma. The Aqsu has a length of 71 km. It drains an area of 1130 km². The mean discharge is 16.77 m³ / s. The river is mainly fed by the snowmelt . The mean discharge in the months with the highest discharge, May and June, is 42.68 m³ / s and 42.68 m³ / s, respectively.
Web links
Individual evidence
- ↑ a b Aqsu at the Aqsu gauge - hydrographic data at R-ArcticNET