The sole remaining interglacial remnant of the glaciation will be the sixty one km very long South Inylschek glacier. The outlet glacier tongues of the plateau glacier flowed northward right down to Lake Issyk Kul, calving With this a hundred and sixty km long lake.
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The Tian Shan in its rapid geological earlier was stored from glaciation mainly because of the "preserving" warm influence of the Indian Ocean monsoon climate. This defined its ecological functions which could maintain its exclusive ecosphere.
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