The evolution of Sf. Gheorghe (Danube) asymmetric deltaic lobe

<p>The wave asymmetric Sf. Gheorghe lobe is the only active in the Danube delta where river mouth bar (and the associated barrier islands and spits) continuously deployed a cyclic development for almost two millennia. During first stage, the Sf. Gheorghe distributary had a small discharge (wit...

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Main Authors: Alfred VESPREMEANU-STROE, Luminiţa PREOTEASA, Florin TĂTUI, Alida TIMAR-GABOR, Ionela CÂRDAN
Format: Article
Language:English
Published: „Ștefan cel Mare” University Press 2014-11-01
Series:GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series
Subjects:
Online Access:http://georeview.ro/ojs/index.php/revista/article/view/245
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spelling doaj-391ba3651ce44642b673dba561d22e8f2021-06-02T09:31:23Zeng„Ștefan cel Mare” University PressGEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series1583-14692014-11-01242172173287The evolution of Sf. Gheorghe (Danube) asymmetric deltaic lobeAlfred VESPREMEANU-STROELuminiţa PREOTEASAFlorin TĂTUIAlida TIMAR-GABORIonela CÂRDAN<p>The wave asymmetric Sf. Gheorghe lobe is the only active in the Danube delta where river mouth bar (and the associated barrier islands and spits) continuously deployed a cyclic development for almost two millennia. During first stage, the Sf. Gheorghe distributary had a small discharge (with an order of magnitude lower than present) which after that experienced a rapid increase in consequence of the successive avulsions of Împuţita (southern distributary of Sulina arm) and Dunavăţ distributaries. Our morphological analyses together with the newly obtained chronology, revealed the multiple ridgesets structure of Sf. Gheorghe deltaic lobe. In fact, all ridgesets (10) follow a common morphodynamic pattern characterized by the cyclic succession of three stages: i) subaqueous mouth bar development, ii) barrier island emergence, iii) barrier spit phase with several secondary spits derived from an updrift trunk ridge. The size of each ridgeset increased exponentially with every new cycle due to the constant lengthening of the coastline as the downdrift side of the lobe advances seaward through a series of progressively larger similar quadrilaterals, yielding to a constant enlargment of the delta front size. </p>http://georeview.ro/ojs/index.php/revista/article/view/245danube delta evolution
collection DOAJ
language English
format Article
sources DOAJ
author Alfred VESPREMEANU-STROE
Luminiţa PREOTEASA
Florin TĂTUI
Alida TIMAR-GABOR
Ionela CÂRDAN
spellingShingle Alfred VESPREMEANU-STROE
Luminiţa PREOTEASA
Florin TĂTUI
Alida TIMAR-GABOR
Ionela CÂRDAN
The evolution of Sf. Gheorghe (Danube) asymmetric deltaic lobe
GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series
danube delta evolution
author_facet Alfred VESPREMEANU-STROE
Luminiţa PREOTEASA
Florin TĂTUI
Alida TIMAR-GABOR
Ionela CÂRDAN
author_sort Alfred VESPREMEANU-STROE
title The evolution of Sf. Gheorghe (Danube) asymmetric deltaic lobe
title_short The evolution of Sf. Gheorghe (Danube) asymmetric deltaic lobe
title_full The evolution of Sf. Gheorghe (Danube) asymmetric deltaic lobe
title_fullStr The evolution of Sf. Gheorghe (Danube) asymmetric deltaic lobe
title_full_unstemmed The evolution of Sf. Gheorghe (Danube) asymmetric deltaic lobe
title_sort evolution of sf. gheorghe (danube) asymmetric deltaic lobe
publisher „Ștefan cel Mare” University Press
series GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series
issn 1583-1469
publishDate 2014-11-01
description <p>The wave asymmetric Sf. Gheorghe lobe is the only active in the Danube delta where river mouth bar (and the associated barrier islands and spits) continuously deployed a cyclic development for almost two millennia. During first stage, the Sf. Gheorghe distributary had a small discharge (with an order of magnitude lower than present) which after that experienced a rapid increase in consequence of the successive avulsions of Împuţita (southern distributary of Sulina arm) and Dunavăţ distributaries. Our morphological analyses together with the newly obtained chronology, revealed the multiple ridgesets structure of Sf. Gheorghe deltaic lobe. In fact, all ridgesets (10) follow a common morphodynamic pattern characterized by the cyclic succession of three stages: i) subaqueous mouth bar development, ii) barrier island emergence, iii) barrier spit phase with several secondary spits derived from an updrift trunk ridge. The size of each ridgeset increased exponentially with every new cycle due to the constant lengthening of the coastline as the downdrift side of the lobe advances seaward through a series of progressively larger similar quadrilaterals, yielding to a constant enlargment of the delta front size. </p>
topic danube delta evolution
url http://georeview.ro/ojs/index.php/revista/article/view/245
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