geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-1750Research ArticleНаучные сообщенияShort communicationsЭтапы формирования Пицундского полуостроваStages of the Pitsunda Peninsula formationХоситашвилиГ. Р.KhositashviliG. R.КупцовВ. М.KuptsovV. M.ТолстыхТ. Н.TolstykhT. N.ВСЕГИНГЕОРоссия19761905202203Геоморфология100105Copyright © Хоситашвили Г.Р., Купцов В.М., Толстых Т.Н., 20222022Хоситашвили Г.Р., Купцов В.М., Толстых Т.Н.Khositashvili G.R., Kuptsov V.M., Tolstykh T.N.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/1750

The Pitsunda Peninsula is considered to be an aggregation form typical for the Caucasian coast. Its complex structure is determined not only by high variety of the rock facies but by their lateral changes as well. Time model of the Pitsunda mass has been constructed on the base of sediments absolute dating, which was used as a main criterion for estimation of the formation regime.

The Pitsunda Peninsula is considered to be an aggregation form typical for the Caucasian coast. Its complex structure is determined not only by high variety of the rock facies but by their lateral changes as well. Time model of the Pitsunda mass has been constructed on the base of sediments absolute dating, which was used as a main criterion for estimation of the formation regime.

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