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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-2139</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>О взаимосвязи овраг - балка – долина</article-title><trans-title-group xml:lang="en"><trans-title>About the interrelations between gulley, balks, and valley</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>Скоморохов</surname><given-names>А. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Skomorokhov</surname><given-names>A. I.</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>Пос. Геологов, Курская обл.</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2000</year></pub-date><pub-date pub-type="epub"><day>16</day><month>07</month><year>2022</year></pub-date><volume>0</volume><issue>3</issue><issue-title>Геоморфология</issue-title><fpage>25</fpage><lpage>34</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Скоморохов А.И., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Скоморохов А.И.</copyright-holder><copyright-holder xml:lang="en">Skomorokhov A.I.</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/2139">https://geomorphology.igras.ru/jour/article/view/2139</self-uri><abstract><p>Balka and rapid erosion forms are the concepts of different level. Erosion forms constantly change balkas as well as all other slopes, replacing each other in space and time. The formation of correlative deposits is another sequence of rapid erosion forms development.</p></abstract><trans-abstract xml:lang="en"><p>Balka and rapid erosion forms are the concepts of different level. Erosion forms constantly change balkas as well as all other slopes, replacing each other in space and time. The formation of correlative deposits is another sequence of rapid erosion forms development.</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>
