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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-2702</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>Врезание реки в плювиальные отложения на дне долины и харакерные типы руслового процесса</article-title><trans-title-group xml:lang="en"><trans-title>River's downcutting into the valley floor alluvium and characteristic types of the channel process</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>Зубков</surname><given-names>Н. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Zubkov</surname><given-names>N. S.</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>Государственный гидрологический институт, Ленинград</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1987</year></pub-date><pub-date pub-type="epub"><day>15</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>3</issue><issue-title>Геоморфология</issue-title><fpage>39</fpage><lpage>44</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Зубков Н.С., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Зубков Н.С.</copyright-holder><copyright-holder xml:lang="en">Zubkov N.S.</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/2702">https://geomorphology.igras.ru/jour/article/view/2702</self-uri><abstract><p>The paper deals with the mechanism of the recent river downcutting into alluvium which filled preglacial valleys during the glacial time. The channel process type may change from one stage of the background channel deformations to another, the fact should be taken into consideration while predicting long term channel transformations.</p></abstract><trans-abstract xml:lang="en"><p>The paper deals with the mechanism of the recent river downcutting into alluvium which filled preglacial valleys during the glacial time. The channel process type may change from one stage of the background channel deformations to another, the fact should be taken into consideration while predicting long term channel transformations.</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>
