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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-1793</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 овраг образования в разных природных условиях</article-title><trans-title-group xml:lang="en"><trans-title>Characteristics of gully formation at the different natural settings</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>Беляев</surname><given-names>В. Р.</given-names></name><name name-style="western" xml:lang="en"><surname>Beliaev</surname><given-names>V. R.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Московский государственный университет имени М.В.Ломоносова, Географический факультет</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2002</year></pub-date><pub-date pub-type="epub"><day>26</day><month>05</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>105</fpage><lpage>110</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Беляев В.Р., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Беляев В.Р.</copyright-holder><copyright-holder xml:lang="en">Beliaev V.R.</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/1793">https://geomorphology.igras.ru/jour/article/view/1793</self-uri><abstract><p>Field research data, including route and stationary data obtained by Research Institute of Soil Erosion and Channel Processes as well as published data were used to analyze the peculiar features of the gully formation under different natural conditions. Four test sites were taken: in the steppe zone, forest-steppe zone, the southern part of the mixed forest zone and tundra zone. The impact of melt-water and storm rainfall was shown, minimal catch basin area necessary for gullies rise was evaluated as in natural conditions and under strong human impact. Simultaneous action of zonal and local factors of gully formation was analyzed.</p></abstract><trans-abstract xml:lang="en"><p>Field research data, including route and stationary data obtained by Research Institute of Soil Erosion and Channel Processes as well as published data were used to analyze the peculiar features of the gully formation under different natural conditions. Four test sites were taken: in the steppe zone, forest-steppe zone, the southern part of the mixed forest zone and tundra zone. The impact of melt-water and storm rainfall was shown, minimal catch basin area necessary for gullies rise was evaluated as in natural conditions and under strong human impact. Simultaneous action of zonal and local factors of gully formation was analyzed.</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>
