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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-2083</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>Современный русловой аллювий р. Белой и влияние на него интенсивной антропогенной нагрузки</article-title><trans-title-group xml:lang="en"><trans-title>Contemporary channel alluvium of Belaya river and strong human impact on it</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>Злотина</surname><given-names>Л. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Zlotina</surname><given-names>L. V.</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>Московский государственный университет имени М.В.Ломоносова, Географический факультет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2001</year></pub-date><pub-date pub-type="epub"><day>15</day><month>07</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>61</fpage><lpage>65</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Злотина Л.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Злотина Л.В.</copyright-holder><copyright-holder xml:lang="en">Zlotina L.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/2083">https://geomorphology.igras.ru/jour/article/view/2083</self-uri><abstract><p>The exploration of the non-metallic pits in the channel of Belaya river during several decades has caused the significant enlargement of alluvium coarseness in the lower stream. The influence of the draggers is less marked.</p></abstract><trans-abstract xml:lang="en"><p>The exploration of the non-metallic pits in the channel of Belaya river during several decades has caused the significant enlargement of alluvium coarseness in the lower stream. The influence of the draggers is less marked.</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>
