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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-1929</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>Опыт определения объема и скорости общей денудации в условиях лесостепи Русской равнины</article-title><trans-title-group xml:lang="en"><trans-title>An attempt of denudational volume and rate estimation under forest-steppe at the Russian Plain</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>Тимофеев</surname><given-names>Д. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Timofeev</surname><given-names>D. A.</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>Фирсенкова</surname><given-names>В. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Firsenkova</surname><given-names>V. M.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Институт географии АН СССР</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>1978</year></pub-date><pub-date pub-type="epub"><day>15</day><month>06</month><year>2022</year></pub-date><volume>0</volume><issue>3</issue><issue-title>Геоморфология</issue-title><fpage>95</fpage><lpage>100</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Тимофеев Д.А., Фирсенкова В.М., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Тимофеев Д.А., Фирсенкова В.М.</copyright-holder><copyright-holder xml:lang="en">Timofeev D.A., Firsenkova V.M.</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/1929">https://geomorphology.igras.ru/jour/article/view/1929</self-uri><abstract><p>The total erosion at the Seim River basin (Middle Russian Elevation) has been estimated by calculation of the volume of concave erosional landforms. Coefficient of denudation, i. e. volume of eroded rocks to total volume of valley and interfluves ratio is equal to 0,54, which indicates the maturity of the relief under consideration. Erosion rate calculated for Neogene and Quaternary appeared to be 0,028 mm per year, the value being close to the contemporary solid discharge of the Seim River (0,026 mm per year).</p></abstract><trans-abstract xml:lang="en"><p>The total erosion at the Seim River basin (Middle Russian Elevation) has been estimated by calculation of the volume of concave erosional landforms. Coefficient of denudation, i. e. volume of eroded rocks to total volume of valley and interfluves ratio is equal to 0,54, which indicates the maturity of the relief under consideration. Erosion rate calculated for Neogene and Quaternary appeared to be 0,028 mm per year, the value being close to the contemporary solid discharge of the Seim River (0,026 mm per year).</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>
