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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">geomorf</journal-id><journal-title-group><journal-title xml:lang="ru">Геоморфология и палеогеография</journal-title><trans-title-group xml:lang="en"><trans-title>Geomorfologiya i Paleogeografiya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2949-1789</issn><issn pub-type="epub">2949-1797</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">geomorf-1773</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>Научные сообщения</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Short communications</subject></subj-group></article-categories><title-group><article-title>Особенности развития пересыпей восточной Чукотки в условиях повышения уровня моря</article-title><trans-title-group xml:lang="en"><trans-title>Recent development of gravel barriers on the coast of Eastern Chukotka: implications to present and possible future sea-level rise</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Каплин</surname><given-names>П. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Kaplin</surname><given-names>P. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Поротов</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Porotov</surname><given-names>A. V.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Московский государственный университет имени М.В.Ломоносова, Географический факультет</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2002</year></pub-date><pub-date pub-type="epub"><day>26</day><month>05</month><year>2022</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>74</fpage><lpage>82</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Каплин П.А., Поротов А.В., 2015</copyright-statement><copyright-year>2015</copyright-year><copyright-holder xml:lang="ru">Каплин П.А., Поротов А.В.</copyright-holder><copyright-holder xml:lang="en">Kaplin P.A., Porotov A.V.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://geomorphology.igras.ru/jour/article/view/1773">https://geomorphology.igras.ru/jour/article/view/1773</self-uri><abstract><p>Recent morphodynamic of some types of coarse elastic-deposit barriers are considered on the base of comparative study of natural features, historical and archaeological data. The evolution of such types of barriers during recent sea-level rise mostly depends on the type and coarseness of beach sediments. Some peculiarities of coast evolution in Late Holocene have been characterized.</p></abstract><trans-abstract xml:lang="en"><p>Recent morphodynamic of some types of coarse elastic-deposit barriers are considered on the base of comparative study of natural features, historical and archaeological data. The evolution of such types of barriers during recent sea-level rise mostly depends on the type and coarseness of beach sediments. Some peculiarities of coast evolution in Late Holocene have been characterized.</p></trans-abstract></article-meta></front><back><ref-list><title>References</title></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
