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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-2660</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Article</subject></subj-group></article-categories><title-group><article-title>Карта усредненного рельефа Русской равнины</article-title><trans-title-group xml:lang="en"><trans-title>Map of averaged relief of 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>Бронгулеев</surname><given-names>В. Вад.</given-names></name><name name-style="western" xml:lang="en"><surname>Bronguleev</surname><given-names>V. Vad.</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>Бронгулеев</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Bronguleev</surname><given-names>V. V.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт географии АН СССР</institution><country>Россия</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>ВЗПИ</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1987</year></pub-date><pub-date pub-type="epub"><day>14</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>22</fpage><lpage>29</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Бронгулеев В.В., Бронгулеев В.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Бронгулеев В.В., Бронгулеев В.В.</copyright-holder><copyright-holder xml:lang="en">Bronguleev V.V., Bronguleev V.V.</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/2660">https://geomorphology.igras.ru/jour/article/view/2660</self-uri><abstract><p>The map of averaged relief of the Russian Plain gives simple and obvious presentation of the most important topographic features of the area. It emphasizes regional pattern of surface elevations and inclinations distribution and «takes away» small, mostly erosional landforms. An importance of oblique directions of orographic axes is manifested, together with longitudinal and latitudinal directions as well as arcuate connections. A hierarchic structure is clearly seen: landforms of one rank are united in consequtive order to form landforms of higher rank. The technique of the map compiling is described, its contents and some implications are considered.</p></abstract><trans-abstract xml:lang="en"><p>The map of averaged relief of the Russian Plain gives simple and obvious presentation of the most important topographic features of the area. It emphasizes regional pattern of surface elevations and inclinations distribution and «takes away» small, mostly erosional landforms. An importance of oblique directions of orographic axes is manifested, together with longitudinal and latitudinal directions as well as arcuate connections. A hierarchic structure is clearly seen: landforms of one rank are united in consequtive order to form landforms of higher rank. The technique of the map compiling is described, its contents and some implications are considered.</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>
