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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-2027</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>Реликтовый мерзлотный микрорельеф в бассейне верхней Волги</article-title><trans-title-group xml:lang="en"><trans-title>The relic cryogenic microrelief in the basin of the Upper Volga</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>Бердников</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Berdnikov</surname><given-names>V. V.</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>1970</year></pub-date><pub-date pub-type="epub"><day>20</day><month>06</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>63</fpage><lpage>70</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Бердников В.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Бердников В.В.</copyright-holder><copyright-holder xml:lang="en">Berdnikov 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/2027">https://geomorphology.igras.ru/jour/article/view/2027</self-uri><abstract><p>A typical relic hillock-hollow microrelief is discovered on the North of the Yaroslavi region. It is clearly distinct on aero-photographs of the scales 1:15000-1:5000. Topographical works disclosed a system of hillocks and hollows 15-25 metres in size with hillocks rising over hollows by 2 metres. Geological section in lowering of microrelief revealed specific structures which are interpreted as traces of melted and later on filled glacial veins. By the sum of geomorphological signs the hillock - hollow microrelief is determined as the remaining system of the cryogenic genesis. This relic microrelief concludes a genetically unique chain of formations: grounds-blocks-hillocks in the general series of forms of relic cryogenic morphosculpture.</p></abstract><trans-abstract xml:lang="en"><p>A typical relic hillock-hollow microrelief is discovered on the North of the Yaroslavi region. It is clearly distinct on aero-photographs of the scales 1:15000-1:5000. Topographical works disclosed a system of hillocks and hollows 15-25 metres in size with hillocks rising over hollows by 2 metres. Geological section in lowering of microrelief revealed specific structures which are interpreted as traces of melted and later on filled glacial veins. By the sum of geomorphological signs the hillock - hollow microrelief is determined as the remaining system of the cryogenic genesis. This relic microrelief concludes a genetically unique chain of formations: grounds-blocks-hillocks in the general series of forms of relic cryogenic morphosculpture.</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>
