Section of the “Albatross” Quaternary Sediments
- Authors: Komarov V.N1, Vaitieva Y.A1, Goryachev I.A1, Dumnova A.A1
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Affiliations:
- Sergo Ordzhonikidze Russian State Geological Prospecting University
- Issue: No 3 (2023)
- Pages: 64-68
- Section: Articles
- URL: https://journals.eco-vector.com/0032-874X/article/view/631028
- DOI: https://doi.org/10.7868/S0032874X23030079
- ID: 631028
Cite item
Abstract
The outcrop of quaternary sediments located on the coast of the Kazantip Bay, in the vicinity of the village of Novootradnoye, 300 m south-southeast from the guest house “Albatross” has been studied. The studied continental rocks are probably of eluvial origin. However, a significant amount of sand in their composition may indicate the participation of the deluvial process in their formation — temporary flow associated erosion of bedrock on the uplands located to the south, as well as strong aeolian activity, traces of which are manifested in the form of dusty high-carbonate loess-like loams. The formation of sediments, apparently, occurred during the middle subboreal warming (4800–3400 years ago) and coincides with the period of increasing climate aridization.
About the authors
V. N Komarov
Sergo Ordzhonikidze Russian State Geological Prospecting University
Email: komarovmgri@mail.ru
Moscow, Russia
Yu. A Vaitieva
Sergo Ordzhonikidze Russian State Geological Prospecting UniversityMoscow, Russia
I. A Goryachev
Sergo Ordzhonikidze Russian State Geological Prospecting UniversityMoscow, Russia
A. A Dumnova
Sergo Ordzhonikidze Russian State Geological Prospecting UniversityMoscow, Russia
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