geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2421Research ArticleНаучные сообщенияShort communicationsПсевдокарст в лёссовых породахPseudokarst in loessКригерН. И.KrigerN. I.БотниковВ. И.BotnikovV. I.ЛаврусевичС. А.LavrusevichS. A.МиронюкС. Г.MironyukS. G.ПетровА. Г.PetrovA. G.ПНИИИС Госстроя СССРRussian Federation19832909202203Геоморфология7984Copyright © Кригер Н.И., Ботников В.И., Лаврусевич С.А., Миронюк С.Г., Петров А.Г., 20222022Кригер Н.И., Ботников В.И., Лаврусевич С.А., Миронюк С.Г., Петров А.Г.Kriger N.I., Botnikov V.I., Lavrusevich S.A., Mironyuk S.G., Petrov A.G.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/2421

Various forms of surficial and underground cavities in loess are described. Processes giving rise to such cavities are discussed as well as environmental and loess properties which are lavourable to pseudokarst development. Importance of man-induced (technogenous) factors is evaluated.

Various forms of surficial and underground cavities in loess are described. Processes giving rise to such cavities are discussed as well as environmental and loess properties which are lavourable to pseudokarst development. Importance of man-induced (technogenous) factors is evaluated.

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