The Zarafshon is a river in Tajikistan and Uzbekistan in Central Asia. Its name, "spreader of gold" in Persian language, refers to the presence of gold-bearing sands in the upper reaches of the river. To the ancient Greeks it was known as the Polytimetus. It was also formerly known as Sughd River. The river is long and has a basin area of .[ Зеравшан (река в Ср. Азии), Great Soviet Encyclopedia]
Geographic position
It rises at the Zeravshan Glacier, close to where the
Turkestan Range and the
Zeravshan Range of the
Pamir-Alay mountains meet, in
Tajikistan. In its upper course, upstream from its confluence with the
Fan Darya, it is also called
Matcha.
It flows due west for some , passing
Panjakent before entering
Uzbekistan at , where it turns west-to-north-west, flowing past the legendary city of
Samarkand, where it feeds the
Dargom Canal, which is entirely dependent on the
oasis thus created, until it bends left again to the west north of
Navoiy and further to the south-west, passing
Bukhara before it is lost in the desert beyond the city of Qorakoʻl (Karakul), not quite reaching the
Amu Darya, of which it was formerly a tributary.
See also
Notes
Further reading
-
Vasily Bartold "К Истории Орошения в Туркестане" (Collected Works, Vol.3) (Москва) 1965
-
V.V. Barthold "Turkestan Down to the Mongol Invasion" (London) 1968
-
Robert Lewis "Early Irrigation in West Turkestan" Annals of the Association of American Geographers Vol.56 No..3 (Sept. 1966) pp467–491
-
Edgar Knobloch "Beyond the Oxus" (London) 1972