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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-2759</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>Геоморфологический аспект картографирования эрозионно-опасных земель Европейской части СССР</article-title><trans-title-group xml:lang="en"><trans-title>Geomorphic aspects of mapping lands endangered by erosion</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>Литвин</surname><given-names>Л. Ф.</given-names></name><name name-style="western" xml:lang="en"><surname>Litvin</surname><given-names>L. F.</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>Спиридонов</surname><given-names>А. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Spiridonov</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>Московский государственный университет имени М.В.Ломоносова, географический факультет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1988</year></pub-date><pub-date pub-type="epub"><day>19</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>85</fpage><lpage>92</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Литвин Л.Ф., Спиридонов А.И., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Литвин Л.Ф., Спиридонов А.И.</copyright-holder><copyright-holder xml:lang="en">Litvin L.F., Spiridonov 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/2759">https://geomorphology.igras.ru/jour/article/view/2759</self-uri><abstract><p>When mapping the erosion processes in small scale the topographic erosional potential (TEP) should be analysed on the basis of general geomorphological subdivision. In most of geomorphological regions the curves of areas distribution according to the TEP values are characterized by a left-hand asymmetry, most pronounced within flat lowlands. A selectivity of agricultural development of lands smooths down differences in TEP of arable lands between lowlands and eroded elevated regions.</p></abstract><trans-abstract xml:lang="en"><p>When mapping the erosion processes in small scale the topographic erosional potential (TEP) should be analysed on the basis of general geomorphological subdivision. In most of geomorphological regions the curves of areas distribution according to the TEP values are characterized by a left-hand asymmetry, most pronounced within flat lowlands. A selectivity of agricultural development of lands smooths down differences in TEP of arable lands between lowlands and eroded elevated regions.</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>
