geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-1775Research ArticleНаучные сообщенияShort communicationsОценка денудационного среза Малого КавказаEvaluation of the degradation sheet on Lesser CaucasusХалиловГ. А.HalilovG. A.Институт географии АН АзербайджанаАзербайджан20022605202201Геоморфология9097Copyright © Халилов Г.А., 20152015Халилов Г.А.Halilov G.A.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/1775

Some general and particular problems of the degradation sheet of Lesser Caucasus are discussed. Its value and rate of denudation are determined by stratigraphic methods. Due to significant complexity of geodynamic and paleogeomorphologic conditions of Lesser Caucasus evolution the denudation rate differs strongly from place to place and depends on morphostructures. The degradation sheet was consequently evaluated for each morphostructure particularly. It varies from 85 to 1650 m and the denudation rate - from 0.01 to 0.08 mm/y.

Some general and particular problems of the degradation sheet of Lesser Caucasus are discussed. Its value and rate of denudation are determined by stratigraphic methods. Due to significant complexity of geodynamic and paleogeomorphologic conditions of Lesser Caucasus evolution the denudation rate differs strongly from place to place and depends on morphostructures. The degradation sheet was consequently evaluated for each morphostructure particularly. It varies from 85 to 1650 m and the denudation rate - from 0.01 to 0.08 mm/y.

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