Dynamics of landscapes of the spit Dolgaya

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Abstract


This paper is devoted to the analysis of the landscape dynamics of the Dolgaya Spit, Taganrog Bay of the Sea of Azov. The analysis of the dynamics of the lithological composition, topography, soil, vegetation, anthropogenic impact. The formation of new shafts of beach-forming material from sand and shell occurs continuously on the western side of the spit. The maximum height is reached by the newly formed ramparts on the western part of the spit, as the height of the shafts decreases to the east.


About the authors

Anna Mikhaylovna Aleinikova

Peoples’ Friendship University of Russia (RUDN University)

Author for correspondence.
Email: aleinikova_am@rudn.university
8 Podolskoe Shosse, bldg. 5, Moscow, 113093, Russian Federation

Candidate of Geographical Sciences, Associate Professor, Associate Professor of the Department of Geoecology, Ecological Faculty, Peoples’ Friendship University of Russia (RUDN University).

V V Krylenko

P.P. Shirshov Institute of Oceanology of the Russian Academy of Sciences (The Southern branch)

Email: krylenko@mail.ru
1G Prostornaya St., Gelendzhik, Krasnodar region, 353467, Russian Federation

References

  1. Geologiya Azovskogo moray [Geology of the Azov Sea]. Kiev: Naukova Dumka Publ.; 1974. 246 p.
  2. Kosyan RD, Krylenko VV. Sovremennoe sostoyanie morskih akkumulyativnyh beregov Krasnodarskogo kraya i ih ispolzovanie [The current state of the marine accumulative shores of the Krasnodar territory and their use]. Krasnodar: Nauchnyi mir Publ.; 2014. 256 p.
  3. Krylenko VV, Аleinikov АА, Boiko ЕS, Krylenko MV. Оsenka dinamiki beregovoi linii коsy Dоlgaya pri pomoshi sputnikovyh snimkov [Assessment of the dynamics of the coastline of the Dolgaya Spit using satellite images]. Geographicheskie issledovaniea Krasnodarskogo kraya: sb. nauch. trudov [Geographical research of the Krasnodar territory: coll. scientific proceedings]. Кrasnodar: Кubanskii gos. un-т Publ.; 2016;(10): 253—260.

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Copyright (c) 2018 Aleinikova A.M., Krylenko V.V.

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