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The Tuyuksu Glacier (Kazakh: Tūiyqsu, Тұйықсу — stagnant water, tr. tuyiq'su) is a central, valley glacier in Kazakhstan, located on the northern slope of the Zailiyskiy Alatau ridge, in the upper reaches of the Malaya Almatinka River, located from south to north at the foot of the eponymous mountain pass, in the center of a group of glaciers which form a horseshoe-shaped circus.[1]