geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2828Research ArticleНаучные сообщенияShort communicationsСвязь руслоформирующей деятельности рек Приморского Края с геолого-геоморфологическими условиямиGeologic and geomorphic control over the channel-forming activity of the Maritime territory riversСахарюкН. П.SakharyukN. P.КарасевМ. С.KarasevM. S.Дальневосточный научно-исследовательский институт гидротехники н мелиорацииRussian Federation19890912202202Геоморфология8492Copyright © Сахарюк Н.П., Карасев М.С., 20222022Сахарюк Н.П., Карасев М.С.Sakharyuk N.P., Karasev M.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/2828

Geologic and topographic features of the Maritime territory control the loose material volume which comes from slopes to valleys floor as well as conditions of channel deformations development and floodplain-forming processes. Three types and eleven sub-types of curves of the channel-forming discharges are distinguished according to geologic and geomorphic conditions of the drainage basins and order of streams. The data obtained permit to approach prognosis of changes in rivers channel-forming activity by way of model ling of changes in conditions of channel deformations and floodplain-forming processes while the drainage basins topography assumed to be invariable.

Geologic and topographic features of the Maritime territory control the loose material volume which comes from slopes to valleys floor as well as conditions of channel deformations development and floodplain-forming processes. Three types and eleven sub-types of curves of the channel-forming discharges are distinguished according to geologic and geomorphic conditions of the drainage basins and order of streams. The data obtained permit to approach prognosis of changes in rivers channel-forming activity by way of model ling of changes in conditions of channel deformations and floodplain-forming processes while the drainage basins topography assumed to be invariable.

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