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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-2592</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>Методика научных исследований</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Scientific Research Methods</subject></subj-group></article-categories><title-group><article-title>Методические проблемы изучения экзогенных геоморфологических процессов</article-title><trans-title-group xml:lang="en"><trans-title>Methodic problems of study of exogenous geomorphic processes</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>Агафонов</surname><given-names>Б. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Agafonov</surname><given-names>B. P.</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 земной коры СО АН СССР</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1986</year></pub-date><pub-date pub-type="epub"><day>09</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>24</fpage><lpage>31</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Агафонов Б.П., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Агафонов Б.П.</copyright-holder><copyright-holder xml:lang="en">Agafonov B.P.</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/2592">https://geomorphology.igras.ru/jour/article/view/2592</self-uri><abstract><p>Perspectives of study of exogenous geomorphic processes are described based on century-old regime observations, taking into consideration influence of both natural and technological sources of vibration. Recommendations are provided on the improved technique of the rate of exogeomorphic processes measurements based on the author's experience. Fundamental differences are noted in denudation rates of similar by appearance fresh artificial and old natural exposures of solid rocks.</p></abstract><trans-abstract xml:lang="en"><p>Perspectives of study of exogenous geomorphic processes are described based on century-old regime observations, taking into consideration influence of both natural and technological sources of vibration. Recommendations are provided on the improved technique of the rate of exogeomorphic processes measurements based on the author's experience. Fundamental differences are noted in denudation rates of similar by appearance fresh artificial and old natural exposures of solid rocks.</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>
