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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-1813</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>Морфологический анализ рельефа северо-восточной части Балтийского щита</article-title><trans-title-group xml:lang="en"><trans-title>Morphological analysis of the N-E Baltic shield relief</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>Корсакова</surname><given-names>О. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Korsakova</surname><given-names>O. P.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Геологический институт КНЦ РАН</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2002</year></pub-date><pub-date pub-type="epub"><day>27</day><month>05</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>87</fpage><lpage>95</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Корсакова О.П., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Корсакова О.П.</copyright-holder><copyright-holder xml:lang="en">Korsakova O.P.</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/1813">https://geomorphology.igras.ru/jour/article/view/1813</self-uri><abstract><p>The paper is emphasized on the problem of determining of the North-East Baltic Shield morphological structure. It consists of different rank landforms, which may be distinguished by their area and altitudes. For this purpose the generalization of topographic surface was made by the method of different scale averaging of relief and the distribution of the heights above sea level was used. The main regional hypsometric boundaries of landforms were determined. As a result the morphological zoning of the northern part of the Baltic Shield was carried out.</p></abstract><trans-abstract xml:lang="en"><p>The paper is emphasized on the problem of determining of the North-East Baltic Shield morphological structure. It consists of different rank landforms, which may be distinguished by their area and altitudes. For this purpose the generalization of topographic surface was made by the method of different scale averaging of relief and the distribution of the heights above sea level was used. The main regional hypsometric boundaries of landforms were determined. As a result the morphological zoning of the northern part of the Baltic Shield was carried out.</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>
