Dynamics of landscapes of the spit Dolgaya

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...

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Main Authors: Anna Mikhaylovna Aleinikova, V V Krylenko
Format: Article
Language:English
Published: Peoples’ Friendship University of Russia (RUDN University) 2018-12-01
Series:RUDN Journal of Ecology and Life Safety
Subjects:
Online Access:https://journals.rudn.ru/ecology/article/viewFile/20882/16839
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author Anna Mikhaylovna Aleinikova
V V Krylenko
author_facet Anna Mikhaylovna Aleinikova
V V Krylenko
author_sort Anna Mikhaylovna Aleinikova
collection DOAJ
description 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.
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spelling doaj.art-b5e4c7cbe0ec43bab8f72295701e2d112022-12-22T00:20:13ZengPeoples’ Friendship University of Russia (RUDN University)RUDN Journal of Ecology and Life Safety2313-23102408-89192018-12-0126337938510.22363/2313-2310-2018-26-3-379-38517499Dynamics of landscapes of the spit DolgayaAnna Mikhaylovna Aleinikova0V V Krylenko1Peoples&rsquoP.P. Shirshov Institute of Oceanology of the Russian Academy of Sciences (The Southern branch)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.https://journals.rudn.ru/ecology/article/viewFile/20882/16839landscape dynamicsspit relief
spellingShingle Anna Mikhaylovna Aleinikova
V V Krylenko
Dynamics of landscapes of the spit Dolgaya
RUDN Journal of Ecology and Life Safety
landscape dynamics
spit relief
title Dynamics of landscapes of the spit Dolgaya
title_full Dynamics of landscapes of the spit Dolgaya
title_fullStr Dynamics of landscapes of the spit Dolgaya
title_full_unstemmed Dynamics of landscapes of the spit Dolgaya
title_short Dynamics of landscapes of the spit Dolgaya
title_sort dynamics of landscapes of the spit dolgaya
topic landscape dynamics
spit relief
url https://journals.rudn.ru/ecology/article/viewFile/20882/16839
work_keys_str_mv AT annamikhaylovnaaleinikova dynamicsoflandscapesofthespitdolgaya
AT vvkrylenko dynamicsoflandscapesofthespitdolgaya