geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2671Research ArticleНаучные сообщенияShort communicationsИзменение морфологии русла и руслоформирующих наносов от истока до устья (на примере р. Терека). Changes of channel morphology and bed load from the source towards mouth (case study of the Terek River)ЛодинаР. В.LodinaR. V.РашутинД. В.RashutinD. V.СидорчукА. Ю.SidorchukA. Yu.ЧаловР. С.ChalovR. S.Московский государственный университет имени М.В.Ломоносова, географический факультетРоссия19871411202201Геоморфология8694Copyright © Лодина Р.В., Рашутин Д.В., Сидорчук А.Ю., Чалов Р.С., 20222022Лодина Р.В., Рашутин Д.В., Сидорчук А.Ю., Чалов Р.С.Lodina R.V., Rashutin D.V., Sidorchuk A.Y., Chalov R.S.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/2671

Morphological types of the Terek River channel are considered and their succession from the source towards the river mouth is discussed, the latter being preconditioned with the valley geological and geomorphic features. The longitudinal profile transformation is considered in details as well as special features of the bed load granulometric differentiation along the valley.

Morphological types of the Terek River channel are considered and their succession from the source towards the river mouth is discussed, the latter being preconditioned with the valley geological and geomorphic features. The longitudinal profile transformation is considered in details as well as special features of the bed load granulometric differentiation along the valley.

References

The authors declare that there are no conflicts of interest present.