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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-2276</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>О возрасте речных террас Центрального Предкавказья</article-title><trans-title-group xml:lang="en"><trans-title>On the age of river terraces of the central part of the Caucasian foreland</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>Лукина</surname><given-names>Н. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Lukina</surname><given-names>N. V.</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 АН СССР</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1981</year></pub-date><pub-date pub-type="epub"><day>08</day><month>09</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>68</fpage><lpage>75</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Лукина Н.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Лукина Н.В.</copyright-holder><copyright-holder xml:lang="en">Lukina N.V.</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/2276">https://geomorphology.igras.ru/jour/article/view/2276</self-uri><abstract><p>A new chronological classification is introduced for fluvial terraces of the Kuma and Podkumok rivers based on the terraces' mapping, on their correlation with transgressive levels of fluvio-marine plains of the Caspian region and dated planation surfaces within the mountain area, and on the analysis of geomorphic position of fossil mammals in the Mashuk's travertines. The author distinguishes the Holocene low and high floodplain levels, 4 terraces of Late Pleistocene age, 2 terraces of Middle Pleistocene age and 2 of Early Pleistocene age as well as Apsheronian and Akchagylian topographic levels.</p></abstract><trans-abstract xml:lang="en"><p>A new chronological classification is introduced for fluvial terraces of the Kuma and Podkumok rivers based on the terraces' mapping, on their correlation with transgressive levels of fluvio-marine plains of the Caspian region and dated planation surfaces within the mountain area, and on the analysis of geomorphic position of fossil mammals in the Mashuk's travertines. The author distinguishes the Holocene low and high floodplain levels, 4 terraces of Late Pleistocene age, 2 terraces of Middle Pleistocene age and 2 of Early Pleistocene age as well as Apsheronian and Akchagylian topographic levels.</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>
