geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-1931Research ArticleДискуссииDiscussionsРазногласия в методике специализированного геоморфологического картированияDifferent views on methods of special geomorphological mappingФилатовВ. Ф.FilatovV. F.ЛоскутовЮ. И.LoskutovYu. I.КузнецоваГ. Ф.KuznetsovaF. G.СНИИГГИМСRussian Federation19781506202203Геоморфология107111Copyright © Филатов В.Ф., Лоскутов Ю.И., Кузнецова Г.Ф., 20222022Филатов В.Ф., Лоскутов Ю.И., Кузнецова Г.Ф.Filatov V.F., Loskutov Y.I., Kuznetsova F.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/1931

The authors object to most of the critical comments of Yu. P. Seliverstov on the paper «Principles and some methodical questions of compilation of special geomorphological maps intended for bauxite searches» («Geomorphology», n. 4, 1975). Main difference in their views results from the authors opinion (on the contrary to Seliverstov's one) that weathering crusts are not synchronous to planation surfaces formation, they think that once pediplain is uplifted and dissected the pediment slopes stop parallel retreat.

The authors object to most of the critical comments of Yu. P. Seliverstov on the paper «Principles and some methodical questions of compilation of special geomorphological maps intended for bauxite searches» («Geomorphology», n. 4, 1975). Main difference in their views results from the authors opinion (on the contrary to Seliverstov's one) that weathering crusts are not synchronous to planation surfaces formation, they think that once pediplain is uplifted and dissected the pediment slopes stop parallel retreat.

References

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