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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-2619</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>Оценка степени сохранности ледникового рельефа области московского оледенения</article-title><trans-title-group xml:lang="en"><trans-title>Estimate of glacial topography preservation within the limits of the Moscow ice sheet</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>Лехт</surname><given-names>Э. Е.</given-names></name><name name-style="western" xml:lang="en"><surname>Lekht</surname><given-names>E. E.</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>Чеботарева</surname><given-names>Н. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Chebotareva</surname><given-names>N. S.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Московская комплексная геолого-гидрогеологическая экспедиция ГУЦР</institution><country>Russian Federation</country></aff><aff xml:lang="ru" id="aff-2"><institution>Институт географии АН СССР</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>1986</year></pub-date><pub-date pub-type="epub"><day>09</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>64</fpage><lpage>70</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Лехт Э.Е., Чеботарева Н.С., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Лехт Э.Е., Чеботарева Н.С.</copyright-holder><copyright-holder xml:lang="en">Lekht E.E., Chebotareva N.S.</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/2619">https://geomorphology.igras.ru/jour/article/view/2619</self-uri><abstract><p>Studies of the topography modeled by the Moscow ice sheet revealed its primary features being rather well preserved. It’s morphological and morphometric parameters distinctly differ from those of older (Dnieper) and younger (Valdai) ice ages.</p></abstract><trans-abstract xml:lang="en"><p>Studies of the topography modeled by the Moscow ice sheet revealed its primary features being rather well preserved. It’s morphological and morphometric parameters distinctly differ from those of older (Dnieper) and younger (Valdai) ice ages.</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>
