Sileti
| Sileti | ||
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| Data | ||
| location | Aqmola , Pavlodar ( Kazakhstan ) | |
| River system | Schiderti | |
| Headwaters | central area of the Kazakh threshold 51 ° 16 ′ 42 ″ N , 71 ° 46 ′ 37 ″ E |
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| muzzle | in the lake Siletitengis coordinates: 53 ° 4 '28 " N , 73 ° 24' 15" O 53 ° 4 '28 " N , 73 ° 24' 15" O
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| length | 407 km | |
| Catchment area | 18,500 km² | |
| Discharge at the Prirechnoye gauge ( ⊙ ) A Eo : 343 km² Location: 1670 km above the mouth |
MQ Mq |
2.3 m³ / s 6.7 l / (s km²) |
| Discharge at the Ilinka gauge ( ⊙ ) A Eo : 238 km² Location: 12,400 km above the mouth |
MQ Mq |
11.54 m³ / s 48.5 l / (s km²) |
| Discharge at the Izobilny gauge ( ⊙ ) A Eo : 134 km² Location: 14,600 km above the mouth |
MQ Mq |
4.68 m³ / s 34.9 l / (s km²) |
The Sileti ( Kazakh Сілеті ; Russian Селеты Selety ) is an endorheic river in Kazakhstan .
The river has its source east of Nur-Sultan (until 2019 Astana) in the central area of the Kazakh threshold . From there it flows in a northerly direction through the West Siberian lowlands . The river finally reaches the marshland around the outflowless lake Siletitengis . During the spring floods (95% of the annual runoff) the river water flows into the lake. The Sileti has a length of 407 km. Its catchment area covers 18,500 km². In summer, parts of the river run dry. The average discharge at the level Ilyinskoye is 5.8 m³ / s. The river freezes between late October and mid-November. At the end of March / beginning of April it is ice-free again. In some winters the river freezes to the bottom. The river water is used for irrigation and drinking water supply.
Individual evidence
- ↑ a b c d e f g Article Sileti in the Great Soviet Encyclopedia (BSE) , 3rd edition 1969–1978 (Russian)
- ↑ Sileti at the Prirechnoye gauge - hydrographic data from R-ArcticNET
- ↑ Sileti at the Ilinka gauge - hydrographic data from R-ArcticNET
- ↑ Sileti at the Izobilny gauge - hydrographic data from R-ArcticNET