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The Issyk River is a vital high-altitude waterway located within the Trans-Ili Alatau mountains of southeastern Kazakhstan. Originating from glacial meltwater high in the northern Tien Shan range, the river flows northward through the deep, narrow Issyk Gorge, characterized by steep granite cliffs and dense forests of Schrenk's Spruce. Its most significant geographical feature is Lake Issyk, an alpine body of water situated at an elevation of 1,760 meters, which was originally formed 8,000 years ago by a massive natural rockslide dam. The river's hydrology is defined by its cold, turquoise glacial water and its status as a tributary to the broader Ili River basin. However, the river is also geologically noted for its high susceptibility to debris flows; most notably in 1963, a catastrophic glacial lake outburst flood traveled down the river's course, breaching the lake's natural dam and permanently reshaping the valley's topography.