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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-2045</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>Пояса краевых ледниковых образований Кольского региона</article-title><trans-title-group xml:lang="en"><trans-title>Marginal glacial formations of Kola region, North-west Russia</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>Евзеров</surname><given-names>В. Я.</given-names></name><name name-style="western" xml:lang="en"><surname>Yevserov</surname><given-names>V. Ya.</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>Николаева</surname><given-names>С. Б.</given-names></name><name name-style="western" xml:lang="en"><surname>Nikolayeva</surname><given-names>S. B.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Геологический институт Кольского научного центра РАН</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2000</year></pub-date><pub-date pub-type="epub"><day>28</day><month>06</month><year>2022</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>61</fpage><lpage>73</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Евзеров В.Я., Николаева С.Б., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Евзеров В.Я., Николаева С.Б.</copyright-holder><copyright-holder xml:lang="en">Yevserov V.Y., Nikolayeva S.B.</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/2045">https://geomorphology.igras.ru/jour/article/view/2045</self-uri><abstract><p>In the Kola region four belts of marginal formations of the Scandinavian ice sheet were formed during the Late Weichselian glaciation. These belts correspond to four interstadial cycles of the Late Pleistocene. They moved gradually towards the main ice divide situated near the Scandinavian mountains. However ice spreads a considerably larger area during each phase of stadial cooling than during previous phases of interstadial warming. The ice sheet reached its maximum in the Kola regions later than on the western or southern flanks of the Late Weichselian glaciation.</p></abstract><trans-abstract xml:lang="en"><p>In the Kola region four belts of marginal formations of the Scandinavian ice sheet were formed during the Late Weichselian glaciation. These belts correspond to four interstadial cycles of the Late Pleistocene. They moved gradually towards the main ice divide situated near the Scandinavian mountains. However ice spreads a considerably larger area during each phase of stadial cooling than during previous phases of interstadial warming. The ice sheet reached its maximum in the Kola regions later than on the western or southern flanks of the Late Weichselian glaciation.</p></trans-abstract></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Lehman S.J., Keigwin L.D. Sudden changes in North Atlantic circulation during the last deglaciation // Nature. 1992. V. 356. P. 757‑762.</mixed-citation><mixed-citation xml:lang="en">Lehman S.J., Keigwin L.D. Sudden changes in North Atlantic circulation during the last deglaciation // Nature. 1992. V. 356. P. 757‑762.</mixed-citation></citation-alternatives></ref><ref id="cit2"><label>2</label><citation-alternatives><mixed-citation xml:lang="ru">Johnsen S.J., Clausen H.B., Dansgaard W. et al. Irregular glacial interstadials recorded in a new Greenland ice core // Nature. 1992. V. 359. 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