geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3024Research ArticleНаучные сообщенияShort communicationsК истории развития речных долин на юге Срединного хребта КамчаткиOn the valleys history in the Southern Sredinny Range of the Kamchatka PeninsulaЕжовБ. В.EzhovB. V.Тихоокеанский институт географии ДВО РАНРоссия19933101202301Геоморфология9296Copyright © Ежов Б.В., 20232023Ежов Б.В.Ezhov B.V.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/3024

The paper describes terrace alluvium in valleys in the Southern Sredinny Range of Kamchatka, the region featuring denudational-tectonic topography. The fluvial sequence in the terrace series reveals an alteration of cold and warm periods in the alluviation, which permits to correlate the Quaternary climatic fluctuations on Kamchatka with those in West Siberia. Not less than 8 period of river down cutting are distinguished in the evolution of mountain topography, with periods of glacial erosion and glacio-fluvial sedimentation between them.

The paper describes terrace alluvium in valleys in the Southern Sredinny Range of Kamchatka, the region featuring denudational-tectonic topography. The fluvial sequence in the terrace series reveals an alteration of cold and warm periods in the alluviation, which permits to correlate the Quaternary climatic fluctuations on Kamchatka with those in West Siberia. Not less than 8 period of river down cutting are distinguished in the evolution of mountain topography, with periods of glacial erosion and glacio-fluvial sedimentation between them.

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