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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-2215</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>Дискуссии</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Discussions</subject></subj-group></article-categories><title-group><article-title>Типология речных террас. Терминология типов речных террас.</article-title><trans-title-group xml:lang="en"><trans-title>Fluvial terraces typology</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>Розанов</surname><given-names>Л. Л.</given-names></name><name name-style="western" xml:lang="en"><surname>Rozanov</surname><given-names>L. L.</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>Институт географии АН СССР</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1980</year></pub-date><pub-date pub-type="epub"><day>30</day><month>08</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>94</fpage><lpage>104</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Розанов Л.Л., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Розанов Л.Л.</copyright-holder><copyright-holder xml:lang="en">Rozanov L.L.</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/2215">https://geomorphology.igras.ru/jour/article/view/2215</self-uri><abstract><p>The article revises the fluvial terraces' terminology and typology. A geomorphological classification is introduced, consisting of two classes, four types and eight sub-types of the terraces. Criteria of the classes and types identification are formulated in terms of dynamic phases of alluvium, load budget changes in the course of fluvial processes, structure and thickness of alluvium, morphological features of surfaces. A necessity is argued to unify the geomorphological content of various fluvial terraces types, including accumulative, equilibrium accumulative, erosional accumulative, erosional types.</p></abstract><trans-abstract xml:lang="en"><p>The article revises the fluvial terraces' terminology and typology. A geomorphological classification is introduced, consisting of two classes, four types and eight sub-types of the terraces. Criteria of the classes and types identification are formulated in terms of dynamic phases of alluvium, load budget changes in the course of fluvial processes, structure and thickness of alluvium, morphological features of surfaces. A necessity is argued to unify the geomorphological content of various fluvial terraces types, including accumulative, equilibrium accumulative, erosional accumulative, erosional types.</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>
