TheCeyhan River (historicallyPyramos orPyramus (Greek:Πύραμος),Leucosyrus (Greek:Λευκόσυρος)[1] orJihun)[2] is a river inAnatolia in the south ofTurkey.
The Ceyhan River (Pyramus) has its source (known asSöğütlü Dere) at a location calledPınarbaşı 3 km (1.9 mi) on theNurhak Mountains of the EasternTaurus Mountains range, southeast of the town ofElbistan in theKahramanmaraş province of Turkey. According to classical references its source is atCataonia near the town ofArabissus.[3] Its main tributaries are called Harman, Göksun, Mağara Gözü, Fırnız, Tekir, Körsulu, Aksu (which joins Ceyhan at the outskirts of Kahramanmaraş), Çakur, Susas, and Çeperce. Its total length is 509 kilometres (316 mi).
In classical times for a time it passed under ground, but then came forward again as a navigable river, and forced its way through a glen ofMount Taurus, which in some parts was so narrow that Strabo claims a dog or hare could leap across it.[4] Its course, which to this point had been south, then turned to the southwest, and reached the sea. The river was deep and rapid;[5] its average breadth was 1 stadium.[6]
At present, because of the narrow deep valleys that used to exist, the Ceyhan River has been dammed for hydroelectric generation, for flood control and for providing irrigation to the fertile Çukurova region. The main hydroelectric generating dams are atMenzelet,Kılavuzlu,Aslantaş,Sır andBerke. Of the deep valleys, only the one calledKısıklı Canyon exists in its natural form, south of the location the Menzelet Dam.
The quantity of water flow on the Ceyhan River changes greatly season by season. During August and September the river is at its lowest flow. During November and December the autumn rains temporarily raise the water flow rate from 50 to 380 cubic metres per second (1,800 to 13,400 cu ft/s). In January the flow rate decreases until mid-February. As the snows melt in the Taurus Mountains during spring and early summer months, the flow increases and, periodically caused flooding prior to its damming. During the last quarter of the 20th century, during the floods, the two rivers of the Çukurova plain, the Ceyhan River and theSeyhan River, joined at least 6 times.[7]
In classical times the Ceyhan River reached the Mediterranean Sea atMallus. Currently this location is inland a few miles from the Mediterranean coast on an elevation in the Karataş Peninsula,Adana Province, Turkey, a few miles from the town ofKarataş. In classical times it carried with it such a quantity of mud, that, according to an ancient oracle, its deposits would one day reach the island ofCyprus, and thus unite it with the mainland.[8] The delta formed at the mouth of the Ceyhan River is a refuge for wetlands birds and some years their numbers reach a few million. The sand bank in front is famed for nesting ground for sea turtles.
(Comp.Scylax, p. 40;Ptol. v.8.4;Plin. v.22;Mela, i.13;Curtius iii.7;Arrian,Anab. ii.5.8.)
This article incorporates text from a publication now in thepublic domain: Smith, William, ed. (1854–1857). "Pyramus".Dictionary of Greek and Roman Geography. London: John Murray.
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