From springs in Gobi flow along Yenisei then dammed by northern glaciers trough West Siberian Glacial Lake flowed about 10000 km; Mangerud, J. et al.
Flow along Yenisei trough West Siberian Glacial Lake flowed about 10000 km; Mangerud, J. et al. This was from springs in Gobi. This Yenisei was then dammed by northern glaciers.