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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-2599</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 формирования русел малых рек Вологодской области в связи с их хозяйственным использованием</article-title><trans-title-group xml:lang="en"><trans-title>Special features of small rivers channels formation in the Vologda region with view to their economic use</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>Джуха</surname><given-names>И. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Dzhukha</surname><given-names>I. G.</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>Кичигин</surname><given-names>А. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Kichigin</surname><given-names>A. N.</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>Вологодский политехнический институт</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1986</year></pub-date><pub-date pub-type="epub"><day>09</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>66</fpage><lpage>71</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Джуха И.Г., Кичигин А.Н., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Джуха И.Г., Кичигин А.Н.</copyright-holder><copyright-holder xml:lang="en">Dzhukha I.G., Kichigin A.N.</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/2599">https://geomorphology.igras.ru/jour/article/view/2599</self-uri><abstract><p>Channel processes at small rivers are considered for the Vologda region, channels morphology and deformations appeared to depend on geological and geomorphological conditions, the stream's size and its position within the drainage net structure as well as on economic factors. The region is subdivided into areal units according to conditions of the channel-forming discharge at small rivers. Some aspects of environmental protection are considered, measures are recommended to prevent the small rivers from silting and pollution resulting from the cultivation of the rivers valleys and water-sheds.</p></abstract><trans-abstract xml:lang="en"><p>Channel processes at small rivers are considered for the Vologda region, channels morphology and deformations appeared to depend on geological and geomorphological conditions, the stream's size and its position within the drainage net structure as well as on economic factors. The region is subdivided into areal units according to conditions of the channel-forming discharge at small rivers. Some aspects of environmental protection are considered, measures are recommended to prevent the small rivers from silting and pollution resulting from the cultivation of the rivers valleys and water-sheds.</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>
