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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-2269</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Article</subject></subj-group></article-categories><title-group><article-title>Механическая денудация гор Субарктики и умеренного пояса (по данным анализа стока взвешенных наносов)</article-title><trans-title-group xml:lang="en"><trans-title>Mechanical denudation in mountains of the Subarctic and temperate zone (as revealed by solid discharge analysis) 14-22</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>Дедков</surname><given-names>А. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Dedkov</surname><given-names>A. P.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Мозжерин</surname><given-names>В. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Mozzherin</surname><given-names>V. I.</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>Казанский государственный университет</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>14</fpage><lpage>22</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Дедков А.П., Мозжерин В.И., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Дедков А.П., Мозжерин В.И.</copyright-holder><copyright-holder xml:lang="en">Dedkov A.P., Mozzherin V.I.</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/2269">https://geomorphology.igras.ru/jour/article/view/2269</self-uri><abstract><p>По данным анализа взвешенных наносов рассматривается зависимость общей интенсивности механической денудации горных областей от геоморфологических, ландшафтно-климатических, геологических, антропогенных и некоторых других факторов. Проведено сравнение интенсивности механической денудации в горах и на равнинах в одинаковых ландшафтных условиях, интенсивности механической, и химической денудации в различных ландшафтных поясах гор.</p></abstract><trans-abstract xml:lang="en"><p>On the average the mechanic erosion values at Subarctic and temperate zone mountains exceed those of plains (under the same landscape conditions) by factor 2,5 to 3. The erosion rate increases eastward due to increase of the climatic continentality. Within mountain regions the mechanical erosion intensity is controlled by a series of factors, the most important being land-scape-climatic conditions and rocks' composition. The human economy impact is of much importance in regions of high economic development. In the forest zone the mechanical erosion is less than the chemical one, and in the mountain tundra it exceeds the chemical erosion considerably.</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>
