Структура и особенности развития рельефа гравийно-галечных и валунных русел

Аннотация

Investigations of the bed relief structure revealed principal types of channel landforms which form hierarchic sequence of gravel formations on Lena, Aldan, Kirenga and Dniester rivers. Linear parameters of bed ridges appeared to depend on the river's order. The development of the channel macroforms is shown to result from the bed load transport.