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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 pub-id-type="doi">10.15356/0435-4281-1971-1-39-46</article-id><article-id custom-type="elpub" pub-id-type="custom">geomorf-914</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>Дискуссии</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Discussions</subject></subj-group></article-categories><title-group><article-title>О РАЦИОНАЛЬНЫХ ГРАНИЦАХ ГЕОМОРФОЛОГИЧЕСКОГО АНАЛИЗА И НЕКОТОРЫХ ВРЕМЕННЫХ ОПРЕДЕЛЕНИЯХ</article-title><trans-title-group xml:lang="en"><trans-title>ON RATIONAL LIMITS OF THE GEOMORPHOLOGICAL ANALYSIS AND SOME TIME DEFINITIONS</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>Флоренсов</surname><given-names>Н. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Florensov</surname><given-names>N. A.</given-names></name></name-alternatives><email xlink:type="simple">geomorfologiya@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт земной коры СО АН СССР, Иркутск</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of the Earth’s Crust AS USSR, Irkutsk</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1971</year></pub-date><pub-date pub-type="epub"><day>30</day><month>11</month><year>2016</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>39</fpage><lpage>46</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Флоренсов Н.А., 2016</copyright-statement><copyright-year>2016</copyright-year><copyright-holder xml:lang="ru">Флоренсов Н.А.</copyright-holder><copyright-holder xml:lang="en">Florensov N.A.</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/914">https://geomorphology.igras.ru/jour/article/view/914</self-uri><abstract><p>Наблюдающееся в последние годы расширение содержания геомор¬фологии за ее традиционные рамки приводит, с одной стороны, к полез¬ному углублению контактов со смежными науками, особенно с геоло¬гией, а с другой — отвлекает геоморфологию от ее основной задачи — изучения современного рельефа и современных внешних геодинамических процессов. Взаимодействуя со смежными науками, геоморфология должна сохранять присущее ей место, предмет и метод. Реконструкция рельефа прошлых геологических эпох — задача исторической геологии и особенно палеогеоморфологии, которую следует рассматривать, как ветвь геологии.</p></abstract><trans-abstract xml:lang="en"><p>The expansion of modern geomorphology beyond its traditional limits leads, on the one hand, to the strengthening of its contacts with adjacent sciences, particularly with geology, on the other hand, to the distraction of its attention from the main aim — a study of present-day landforms and external geodynamic processes. While interacting with («ther science about the Earth, geomorphology must preserve its distinctive features and position. Reconstructions of landforms of the past geological epochs is the problem of historical geology and, particularly, paleogeomorphology, which is a branch of geology.</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>
