Bank erosion, as an integral part of the lateral river channel migrations, is a multi-factorial phenomenon. Empirical evidence suggests that the riverbank erosion depends on the size of the river, the morphology of the bends, water flow; however, a big role plays erosion resistance of …
2021-8-8 · editor Acad. G. G. Matishov. Rostov-on-Don: SSC RAS Publishing, 2008. 264 р. Several localities of Late Pliocene mammal remains from the territory of north-east Azov region (East Europe, Russia) are considered. Th eir geological and taphonomicalare given
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