The sole remaining interglacial remnant of this glaciation would be the sixty one km lengthy South Inylschek glacier. The outlet glacier tongues of your plateau glacier flowed northward down to Lake Issyk Kul, calving With this a hundred and sixty km very long lake.

This may be a result of dust storm exercise in central Asia. The order of big ionic concentrations in the snow packs was determined to get Ca2+ > SO4 2??> NH4 + > NO3 ??> Cl?? Na+ > Mg2+ > K+. Ca2+ was the dominant cation; SO4 2??was the dominant anion. We find, except NO3 ?? which the variabilities of ionic concentrations are remarkably correlated. Results exhibit the glacier area was drastically influenced by dust activity and anthropogenic source. The major ions, Specifically Na+, originate from dust sources of central Asia and from the Ocean, transported by the westerly winds.

In the same way, potent glaciation was current inside the large mountain region in the Kungey Alatau, which stretches for 230 km north of Issyk Kul and connects for the mountain foreland close to Alma Ata.

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The Tian Shan in its fast geological earlier was saved from glaciation due to the "shielding" heat impact from the Indian Ocean monsoon local weather. This outlined its ecological options which could maintain its distinct ecosphere.

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