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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-1908</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>Крупная экзарационная рытвина о. Келли (оз. Эри), ее происхождение и микрорельеф</article-title><trans-title-group xml:lang="en"><trans-title>Large exaration trough at the Kelly Island, its origin and microrelief</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>Лаврушин</surname><given-names>Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Lavrushin</surname><given-names>Yu.</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>Голдтвейт</surname><given-names>Р.</given-names></name><name name-style="western" xml:lang="en"><surname>Goldthwait</surname><given-names>R.</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>Геологический институт АН СССР</institution><country>Россия</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт полярных исследований Государственного университета г. Колумбус, США</institution><country>Соединённые Штаты Америки</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1978</year></pub-date><pub-date pub-type="epub"><day>14</day><month>06</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>79</fpage><lpage>84</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Лаврушин Ю., Голдтвейт Р., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Лаврушин Ю., Голдтвейт Р.</copyright-holder><copyright-holder xml:lang="en">Lavrushin Y., Goldthwait R.</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/1908">https://geomorphology.igras.ru/jour/article/view/1908</self-uri><abstract><p>The paper describes a large expiration trough at the Kelly island. Conclusions on the trough origin are based on the microrelief analysis, some microrelief elements are considered to be probable model of gigantic expiration troughs and drumlinoids origin.</p></abstract><trans-abstract xml:lang="en"><p>The paper describes a large expiration trough at the Kelly island. Conclusions on the trough origin are based on the microrelief analysis, some microrelief elements are considered to be probable model of gigantic expiration troughs and drumlinoids origin.</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>
