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        <title type="main" level="a">Impact of cliff erosion on marine sediment composition - indication of local coastline evolution (Vrgada Island, Croatia)</title>
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          <persName n="1" ref="https://orcid.org/0000-0001-8789-8068" type="ORCID">
            <forename>Kristina</forename>
            <surname>Pikelj</surname>
            <placeName type="affiliation">University of Zagreb, Croatia</placeName>
          </persName>
          <persName n="2">
            <forename>Nina</forename>
            <surname>Furčić</surname>
            <placeName type="affiliation">University of Zagreb, Croatia</placeName>
          </persName>
        </author>
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          <resp>This is a section of <title>Eighth International Symposium “Monitoring of Mediterranean Coastal Areas. Problems and Measurement Techniques”</title>(DOI: <idno type="DOI">10.36253/978-88-5518-147-1</idno>) by </resp>
          <name>Donatella Carboni, Laura Bonora, Matteo De Vincenzi</name>
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      <publicationStmt>
        <publisher>Firenze University Press</publisher>
        <pubPlace>Firenze</pubPlace>
        <date when="2020">2020</date>
        <idno type="DOI">https://doi.org/10.36253/978-88-5518-147-1.46</idno>
        <availability>
          <p>Available for academic research purposes</p>
          <p>Open Access</p>
          <p>Copyright Author(s)</p>
          <licence source="text" target="https://creativecommons.org/licenses/by/4.0/legalcode">
            <p>Content licence CC BY 4.0</p>
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      <abstract xml:lang="en">
        <p>Erosive coastal cliffs formed in soft-rocks sediments along the generally carbonaceous Eastern Adriatic are a rare feature. The one from the Vrgada Island gave rise to the idea that local seabed surface sediment may reflect the composition of the cliff sediment. First results of sedimentological analyses showed that sediment samples collected on both sides of the cliff contain material eroded mostly from the eastern side of the cliff. Subsequent longshore drift caused by dominant waves likely sort fallen material, transporting its finer fractions to the northern side and further into the sea.</p>
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      <textClass>
        <keywords>
          <list>
            <item>Coastal cliff</item>
            <item>Surface sediment</item>
            <item>Coastal erosion</item>
            <item>Vrgada Island</item>
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      <p>It is available online at https://doi.org/10.36253/978-88-5518-147-1.46<ref target="https://doi.org/10.36253/978-88-5518-147-1.46" /></p>
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          <head>References</head>
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            <bibl>Pikelj, K., Juračić, M. - Eastern Adriatic Coast (EAC): geomorphology and coastal vulnerability of a Karstic Coast. J. Coastal Res. (2013) 29 (4), 944–957.</bibl>
            <idno type="DOI">10.2112/JCOASTRES-D-12-00136.1</idno>
          </bibl>
          <bibl n="15804">Pikelj, K. - Composition and origin of seabed sediments of the eastern part of the Adriatic Sea (in Croatian). (2010) Unpublished Ph.D. Thesis, University of Zagreb, p. 239.</bibl>
          <bibl n="15805">Pikelj, K., Jakšić, L., Aščić, Š., Juračić, M. - Characterization of the fine-grained fraction in the surface sediment of the eastern Adriatic channel areas. Acta Adriat. (2016) 57, 195–208.</bibl>
          <bibl n="15806">Banak, A., Pikelj, K., Lužar-Oberiter B., Kordić, B. - Sedimentary record of Pleistocene aeolian - alluvial deposits on Vrgada island (eastern Adriatic coast, Croatia). Submitted (2020)</bibl>
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          <bibl n="15808">Mamužić, P. - Basic Geological Map of SFRY: Sheet Šibenik, scale 1:100 000 (K33-8). Institut za geološka istraživanja (1962-1965); Savezni geološki zavod, Beograd, 1 sheet.</bibl>
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