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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-2895</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>Принципы составления геоморфологической карты Европейской части СССР масштаба 1:2 000 000 для высшей школы</article-title><trans-title-group xml:lang="en"><trans-title>Principles of geomorphological map compilation aimed for higher School: map of the European USSR, scale 1:2 000 000</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>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 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>1991</year></pub-date><pub-date pub-type="epub"><day>22</day><month>12</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>87</fpage><lpage>92</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Спиридонов А.И., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Спиридонов А.И.</copyright-holder><copyright-holder xml:lang="en">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/2895">https://geomorphology.igras.ru/jour/article/view/2895</self-uri><abstract><p>As distinct from the Geomorphological map of the European USSR, scale 1: 2 500 000, published in 1966, the new geomorphological map of the same area based on an analytic legend which shows topographic elements and landforms and specifies their age and genesis (and not morphological complexes). The map clearly displays the relief history and evolution, and geomorphic structure resulted from endogenic and exogenic factors interplay, and the recent dynamics of the topography. The map may be used in education as well as applied to solving scientific and practical tasks.</p></abstract><trans-abstract xml:lang="en"><p>As distinct from the Geomorphological map of the European USSR, scale 1: 2 500 000, published in 1966, the new geomorphological map of the same area based on an analytic legend which shows topographic elements and landforms and specifies their age and genesis (and not morphological complexes). The map clearly displays the relief history and evolution, and geomorphic structure resulted from endogenic and exogenic factors interplay, and the recent dynamics of the topography. The map may be used in education as well as applied to solving scientific and practical tasks.</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>
