geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2439Research ArticleНаучные сообщенияShort communicationsМатематическое моделирование тектонических деформаций речных террасMathematical models of river terraces deformations due to tectonicsКленовВ. И.KlenovV. I.Московский государственный университет имени М.В.Ломоносова, Географический факультетРоссия19832909202204Геоморфология8386Copyright © Кленов В.И., 20222022Кленов В.И.Klenov V.I.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/2439

Computer modeling permits to study river terraces response on different types of tectonic movements. If the .rate of uplift increases upstream, the resulting terraces are of chord type, altitudes of synchronous terraces fluctuate due to self-oscillattion. The river's response to differentiated uplifts is pronounced not only within the raised area, but in the adjacent parts of the valley as well. Besides, all the responses of the valley and its terraces to the tectonics have prolonged aftereffects. Deformations of terrace series bring about destruction of most of earlier levels.

Computer modeling permits to study river terraces response on different types of tectonic movements. If the .rate of uplift increases upstream, the resulting terraces are of chord type, altitudes of synchronous terraces fluctuate due to self-oscillattion. The river's response to differentiated uplifts is pronounced not only within the raised area, but in the adjacent parts of the valley as well. Besides, all the responses of the valley and its terraces to the tectonics have prolonged aftereffects. Deformations of terrace series bring about destruction of most of earlier levels.

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