geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-179710.31857/S043542812205008Xgeomorf-3125Research ArticleФлювиальная геоморфологияProblems of Fluvial GeomorphologyВлияние газогидротермальной деятельности на формирование рельефа речных долин геотермальных зонGas-hydrothermal activities impact on the relief formation of geothermal zones’ river valleysЛебедеваЕ. В.LebedevaE. V.Ekaterina.lebedeva@gmail.comИнститут географии РАН, МоскваРоссияInstitute of Geography RAS, MoscowRussian Federation202213022023535116126Copyright © Лебедева Е.В., 20232023Лебедева Е.В.Lebedeva E.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/3125

Выходы сольфатарных газов, грязевулканические проявления, минерализованные термальные воды способствуют формированию разнообразных, иногда весьма специфических форм рельефа в днищах и на бортах речных долин территорий современного вулканизма. Проведена типизация денудационных и аккумулятивных форм преимущественно микро- и мезорельефа в речных долинах геотермальных зон в условиях проявлений газогидротермальной активности. Рассмотрены особенности влияния газогидротерм на характер геоморфологических процессов в пределах речных долин, проанализированы причины интенсификации склоновых процессов и эрозии. Основные выявленные закономерности типичны для большинства долин с газогидротермальными проявлениями, что подтверждают наблюдения в долинах рек, дренирующих склоны вулканов Тихоокеанского огненного кольца (в том числе Курильских островов, Камчатки, Новой Зеландии, Северной и Южной Америки), а также Исландии. 

Solfataric gases outputs, mud volcanic manifestations and mineralized thermal waters contribute to the formation of various, sometimes very specific landforms on the slopes and the bottoms of river valleys in the modern volcanism territories. It has been carried out the typification of denudation and accumulative forms of predominantly micro- and mesorelief in river valleys of geothermal zones under the conditions of gas-hydrothermal activity manifestations. The features of gas hydrotherms influence on the nature of geomorphological processes within river valleys are considered, and analysed the reasons for intensification of the slope processes and erosion. The main patterns revealed are typical for the most valleys with gas-hydrothermal manifestations, which is confirmed by observations in the river valleys, draining the slopes of volcanoes of the Pacific Ring of Fire (including the Kuril Islands, Kamchatka, New Zealand, North and South America), as well as of Iceland. 

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