Kshtut
Kshtut | ||
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Data | ||
location | Tajikistan | |
River system | Zerafshan | |
Drain over | Zerafshan → Karaköl | |
Headwaters |
Hissar Mountains / Serafschankette 39 ° 7 ′ 52 ″ N , 68 ° 9 ′ 36 ″ E |
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muzzle |
Zerafshan coordinates: 39 ° 27 '19 " N , 68 ° 3' 5" E 39 ° 27 '19 " N , 68 ° 3' 5" E
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length | approx. 60 km | |
Catchment area | approx. 800 km² | |
Discharge at the Zerikhisor gauge ( ⊙ ) A Eo : 792 km²
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MQ 1936/1985 Mq 1936/1985 |
7.33 m³ / s 9.3 l / (s km²) |
The Kshtut ( Tajik Киштӯд ) is a left tributary of the Serafshan in Tajikistan .
The Kshtut rises in the north of the Hissar Mountains at the transition to the Serafschankette . It is fed by the local glaciers . The Kstut initially flows in a westerly direction, later it turns north and cuts through the Serafschan chain. The Kshtut finally ends above Dasthizkazy , 40 km east of panjakent , in the flowing west Zeravshan. The Kshtut has a length of about 60 km. Its catchment area covers approx. 800 km². The mean discharge at the Zerikhisor gauge , about 10 km above the mouth, is 7.33 m³ / s. June and July are the months with the most flow.
In the catchment area of the Kshtut, below the Tschimtarga , the highest peak of the Serafshan chain, lie the Kulikalon lakes .
Individual evidence
- ↑ a b UNESCO: Kshtut at Zerikhisor (discharge data 1936–1985) ( Memento of the original from August 8, 2014 in the Internet Archive ) Info: The archive link was inserted automatically and has not yet been checked. Please check the original and archive link according to the instructions and then remove this notice.