MORPHOLOGY AND DYNAMICS OF THE LARGE RIVER COASTS IN THE FROST GROUND ZONE (MIDDLE LENA NEAR YAKUTSK AS AN EXAMPLE)
https://doi.org/10.15356/0435-4281-2014-1-81-91
Abstract
Major features of bank erosion within the middle course of the Lena River are related to the hydrological conditions of flowing water contact with different floodplain levels, and variations in floodplain lithology. Formative discharges of the spring freshet correspond to the frozen sandy strata of the high floodplain banks, thus promoting thermal erosion of the latter. Effectiveness of the thermal erosion increases with the increase in bank height and is highest for high floodplain and terrace levels. Morphology of the banks depends not on the rate of their washing out, but on the influx of the sediments at their base. Volume of eroded bank material exceeds the annual bedload runoff due to the large extent of the eroded bank within the studied Lena River reach.
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Review
For citations:
Tananayev N.I. MORPHOLOGY AND DYNAMICS OF THE LARGE RIVER COASTS IN THE FROST GROUND ZONE (MIDDLE LENA NEAR YAKUTSK AS AN EXAMPLE). Geomorfologiya. 2014;(1):81-91. (In Russ.) https://doi.org/10.15356/0435-4281-2014-1-81-91