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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-3153</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>Земная поверхность и ее дискретизация</article-title><trans-title-group xml:lang="en"><trans-title>The Earth surface and its discrete evaluation</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>Лазаревич</surname><given-names>К. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Lazarevich</surname><given-names>K. S.</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>Госцентр «Природа»</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1994</year></pub-date><pub-date pub-type="epub"><day>02</day><month>03</month><year>2023</year></pub-date><volume>0</volume><issue>4</issue><fpage>25</fpage><lpage>28</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Лазаревич К.С., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Лазаревич К.С.</copyright-holder><copyright-holder xml:lang="en">Lazarevich K.S.</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/3153">https://geomorphology.igras.ru/jour/article/view/3153</self-uri><abstract><p>Contrary to views of A. N. Lastochkin, discussed in the paper, the author is of opinion that the topography representation on maps by means of isolines is not necessarily continuous, gradual and unambiguous. Landforms and their elements should be identified using structural lines based on extreme values of elevations, their 1st and 2nd derivatives that, in turn, require the elevations to be rigorously set as a function of horizontal coordinates, which is not possible as yet. Hierarchic classification of the surface landforms is needless if only morphology matters, though it becomes necessary when the genesis and age of the relief are considered.</p></abstract><trans-abstract xml:lang="en"><p>Contrary to views of A. N. Lastochkin, discussed in the paper, the author is of opinion that the topography representation on maps by means of isolines is not necessarily continuous, gradual and unambiguous. Landforms and their elements should be identified using structural lines based on extreme values of elevations, their 1st and 2nd derivatives that, in turn, require the elevations to be rigorously set as a function of horizontal coordinates, which is not possible as yet. Hierarchic classification of the surface landforms is needless if only morphology matters, though it becomes necessary when the genesis and age of the relief are considered.</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>
