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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-3557</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>Теория морфометрии: новый этап</article-title><trans-title-group xml:lang="en"><trans-title>Theory of morphometry: new phase</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>Берлянт</surname><given-names>А. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Berlyant</surname><given-names>A. M.</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>Московский государственный университет имени М.В. Ломоносова, географический факультет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1999</year></pub-date><pub-date pub-type="epub"><day>10</day><month>01</month><year>2024</year></pub-date><volume>0</volume><issue>2</issue><fpage>22</fpage><lpage>28</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Берлянт А.М., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Берлянт А.М.</copyright-holder><copyright-holder xml:lang="en">Berlyant A.M.</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/3557">https://geomorphology.igras.ru/jour/article/view/3557</self-uri><abstract><p>Morphometry is rising today a new higher level due to theoretical understanding its subject and method. The theory is based on considering the landforms as' its object, as well as their distinction, boundary's character, types of points, lines and surfaces which make up structural invariants, the manifestation of the latter in the land surface. In the development of morphometry the cartographic sign systems play the large role, as well as morphometrical mapping techniques of which isolineal pictures are the most convenient. In prospect morphometry and cartometry will become the nucleus of many interconnected metric disciplines such as photogrammetry, photometry, dynamic cartometry, hologrammetry etc. The "Morphometrical analysis of landforms" by Yu. Simonov is analyzed in connection with these problems.</p></abstract><trans-abstract xml:lang="en"><p>Morphometry is rising today a new higher level due to theoretical understanding its subject and method. The theory is based on considering the landforms as' its object, as well as their distinction, boundary's character, types of points, lines and surfaces which make up structural invariants, the manifestation of the latter in the land surface. In the development of morphometry the cartographic sign systems play the large role, as well as morphometrical mapping techniques of which isolineal pictures are the most convenient. In prospect morphometry and cartometry will become the nucleus of many interconnected metric disciplines such as photogrammetry, photometry, dynamic cartometry, hologrammetry etc. The "Morphometrical analysis of landforms" by Yu. Simonov is analyzed in connection with these problems.</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>
