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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-2973</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>Отражение кольцевых структур Белоруссии в ландшафтах и рельефе земной поверхности</article-title><trans-title-group xml:lang="en"><trans-title>Annular structures as reflected in landscapes and topography of Byelorussia</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>Матвеев</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Matveev</surname><given-names>A. V.</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>Нечипоренко</surname><given-names>Л. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Nechiporenko</surname><given-names>L. A.</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>Институт геохимии и геофизики АН Беларуси</institution><country>Беларусь</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1992</year></pub-date><pub-date pub-type="epub"><day>21</day><month>01</month><year>2023</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>79</fpage><lpage>85</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Матвеев А.В., Нечипоренко Л.А., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Матвеев А.В., Нечипоренко Л.А.</copyright-holder><copyright-holder xml:lang="en">Matveev A.V., Nechiporenko L.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/2973">https://geomorphology.igras.ru/jour/article/view/2973</self-uri><abstract><p>Annular structures identified from space photos are revealed in the drainage pattern and in the distribution of bogs and various types of relief and landforms (of glacial, lacustrine, fluvial and eolian origin). Structures of the 2nd to 4th order appeared to be most distinct in relief, while larger structures are distinguishable only locally and by fragments. Some differences in the geomorphic manifestation of annular structures are found related to the age of topography.</p></abstract><trans-abstract xml:lang="en"><p>Annular structures identified from space photos are revealed in the drainage pattern and in the distribution of bogs and various types of relief and landforms (of glacial, lacustrine, fluvial and eolian origin). Structures of the 2nd to 4th order appeared to be most distinct in relief, while larger structures are distinguishable only locally and by fragments. Some differences in the geomorphic manifestation of annular structures are found related to the age of topography.</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>
