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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-2640</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>Основные типы и сезонные переформирования берегов малых и средних свободномеандрирующих рек Средней Прибалтики</article-title><trans-title-group xml:lang="en"><trans-title>Main types and seasonal transformations of banks of small and medium rivers with free meanders at the Middle Baltic region</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>Эберхардс</surname><given-names>Г. Я.</given-names></name><name name-style="western" xml:lang="en"><surname>Eberhards</surname><given-names>G. Ya.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Латвийский государственный университет им. П. Стучки</institution><country>Латвия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1986</year></pub-date><pub-date pub-type="epub"><day>10</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>3</issue><issue-title>Геоморфология</issue-title><fpage>85</fpage><lpage>90</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Эберхардс Г.Я., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Эберхардс Г.Я.</copyright-holder><copyright-holder xml:lang="en">Eberhards G.Y.</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/2640">https://geomorphology.igras.ru/jour/article/view/2640</self-uri><abstract><p>The paper summarizes the author's many years’ stationary observations on bank erosion at free-meandering rivers of the Middle Baltic region. Various types of the banks destruction are distinguished depending on the geology, elevation, vegetation cover on the floodplain (or terrace) surface, the erosion processes being described in details.</p></abstract><trans-abstract xml:lang="en"><p>The paper summarizes the author's many years’ stationary observations on bank erosion at free-meandering rivers of the Middle Baltic region. Various types of the banks destruction are distinguished depending on the geology, elevation, vegetation cover on the floodplain (or terrace) surface, the erosion processes being described in details.</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>
