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"Eastern transfer" as the main argument in favor of the water origin of the ridge relief of the South of Western Siberia

New data were obtained in favor of “Eastern transfer” – the transfer of material from the North-East to the South-West during the formation of the ridge system in Late Pleistocene. They consist in two positions: first, they are longitudinal furrows in the axial part of the ridges, which are fan-shaped split at their South-Western ends; second, the inextricable genetic link of the ridge relief with the spillways is confirmed. The Eastern transfer is interpreted as convincing evidence of the water origin of the ridge relief.