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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-2784</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>Дискретность и непрерывность в земной поверхности, ее геоморфологическая и топографическая модели</article-title><trans-title-group xml:lang="en"><trans-title>Discreteness and continuity of the Earth's surface: geomorphological and topographic models</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>Ласточкин</surname><given-names>А. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Lastochkin</surname><given-names>A. N.</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>Ленинградский государственный университет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1988</year></pub-date><pub-date pub-type="epub"><day>21</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>21</fpage><lpage>29</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Ласточкин А.Н., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Ласточкин А.Н.</copyright-holder><copyright-holder xml:lang="en">Lastochkin A.N.</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/2784">https://geomorphology.igras.ru/jour/article/view/2784</self-uri><abstract><p>Both topography and geomorphology study the surf ace of the Earth, and topographic and geomorphological models reflect two sides of the object- its continuity and discreteness. It manifests the transition from quantitative changes on the surface of the Earth to qualitative ones, which in turn reflects continuous and discrete character of lithodynamic flows. The geomorphological studies require reduction of the Earth surface to elementary units, the procedure being the basis of all subsequent data processing.</p></abstract><trans-abstract xml:lang="en"><p>Both topography and geomorphology study the surf ace of the Earth, and topographic and geomorphological models reflect two sides of the object- its continuity and discreteness. It manifests the transition from quantitative changes on the surface of the Earth to qualitative ones, which in turn reflects continuous and discrete character of lithodynamic flows. The geomorphological studies require reduction of the Earth surface to elementary units, the procedure being the basis of all subsequent data processing.</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>
