geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3527Research ArticleНаучные сообщенияShort communicationsГеолого-геоморфологическое строение и голоценовая история развития Берестовой балки (Ростовская область)Geologic-geomorphologic structure and development of Berestovaya ravine (Rostov region) during HoloceneПанинА. В.PaninA. V.МалаеваЕ. М.MalayevaE. M.ГолосовВ. Н.GolosovV. N.ИвановаН. Н.IvanovaN. N.МаркеловМ. В.MarkelovM. V.Московский государственный университет имени М.В.Ломоносова, географический факультетРоссия199826122023047085Copyright © Панин А.В., Малаева Е.М., Голосов В.Н., Иванова Н.Н., Маркелов М.В., 20232023Панин А.В., Малаева Е.М., Голосов В.Н., Иванова Н.Н., Маркелов М.В.Panin A.V., Malayeva E.M., Golosov V.N., Ivanova N.N., Markelov M.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/3527

The ravine was thoroughly investigated by means of geologic and topographic-geodetic methods. Three episodes of filling of the ravine by slope deposits during Boreal and Early Atlantic periods of the Holocene were revealed. Two latest were correlated with linear erosion animation as the result of fires. Active secondary bottom erosion occurs during only few last centuries b.p. The longitudinal profile of the ravine was reconstructed, volumes of accumulated material and eroded one were calculated. On this account the conclusion was made that accumulation in Holocene overbalanced bottom erosion.

The ravine was thoroughly investigated by means of geologic and topographic-geodetic methods. Three episodes of filling of the ravine by slope deposits during Boreal and Early Atlantic periods of the Holocene were revealed. Two latest were correlated with linear erosion animation as the result of fires. Active secondary bottom erosion occurs during only few last centuries b.p. The longitudinal profile of the ravine was reconstructed, volumes of accumulated material and eroded one were calculated. On this account the conclusion was made that accumulation in Holocene overbalanced bottom erosion.

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