ГЕОМОРФОЛОГИЯ ТУРГАЙСКОЙ ЛОЖБИНЫ В СВЯЗИ С ПРОБЛЕМОЙ ПЕРЕБРОСКИ ЗАПАДНОСИБИРСКИХ ВОД В СРЕДНЮЮ АЗИЮ

Geomorphological levels (terraces) are described of the Middle and Late Pleistocene ages developed in the Turgai Hollow and correlative to the four geomorphological levels of the Irtysh valley. Of the four levels of the Hollow only one level (100 in) is through. The presence of this level, with a re... View More