The article examines the geological origin, geomorphological evolution, and spatial characteristics of the lower Syr Darya basin. It analyzes the river's hydrological course from the Fergana Valley to the Aral Sea region, along with the historical-geographical significance of its ancient channels — Eski Daryaliq, Inkordarya, Jonadarya, and Quvondarya. Based on scholarly sources, Cenozoic tectonic processes, the delta's role in sustaining ancient human populations, and its contribution to the Aral Sea formation are substantiated.
| Mualliflar | Yuldasheva , Nilufar, Юлдашева , Нилуфар, Yuldasheva , Nilufar |
|---|---|
| Jurnal | Тамаддун нури |
| Nashr sanasi | 2026-07-30 |
| Jild | 7 |
| Betlar | 178-180 |
| Til | O‘zbek |
| DOI | 10.69691/yhjygg29 |
DOI: 10.69691/yhjygg29 · Maqolaning asl sahifasi
Syr Darya, Aral Sea region, lower basin, geomorphology, Turan lowland, Cenozoic, Neogene, Pleistocene, Holocene, paleochannels, delta, alluvial deposits., Сырдарья, Приаралье, нижний бассейн, геоморфология, Туранская низменность, кайнозой, неоген, плейстоцен, голоцен, палеорусла, дельта, аллювий., Sirdaryo, Orolbo‘yi, quyi havza, yer yuzasi shakllari, Turon tekisligi, kaynozoy, neogen, pleystotsen, golotsen, qadimgi o‘zanlar, delta, daryo yotqiziqlari.
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