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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 pub-id-type="doi">10.15356/0435-4281-1971-1-23-28</article-id><article-id custom-type="elpub" pub-id-type="custom">geomorf-912</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>Общетеоретические статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Articles</subject></subj-group></article-categories><title-group><article-title>ИНТЕНСИВНОСТЬ ДЕНУДАЦИИ НА КАВКАЗЕ</article-title><trans-title-group xml:lang="en"><trans-title>THE INTENSITY OF DENUDATION IN THE CAUCASUS</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>Габриелян</surname><given-names>Г. К.</given-names></name><name name-style="western" xml:lang="en"><surname>Gabrielyan</surname><given-names>G. K.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Географический факультет</p></bio><bio xml:lang="en"><p>Faculty of Geography</p></bio><email xlink:type="simple">geomorfologiya@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Ереванский государственный университет</institution><country>Армения</country></aff><aff xml:lang="en"><institution>Yerevan State University</institution><country>Armenia</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1971</year></pub-date><pub-date pub-type="epub"><day>30</day><month>11</month><year>2016</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>22</fpage><lpage>27</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Габриелян Г.К., 2016</copyright-statement><copyright-year>2016</copyright-year><copyright-holder xml:lang="ru">Габриелян Г.К.</copyright-holder><copyright-holder xml:lang="en">Gabrielyan G.K.</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/912">https://geomorphology.igras.ru/jour/article/view/912</self-uri><abstract><p>Приводятся количественные данные по отдельным компонентам денудации. Ежегодно с территории Кавказа процессами флювиальной денудации удаляется в Черное, Азовское и Каспийское моря 180 млн. г, или 90 млн. мг веществ. Денудационный метр охватывает период в 4900 лет.</p></abstract><trans-abstract xml:lang="en"><p>In the Caucasus chemical denudation makes up 34 million tons each year and its annual layer is 38 microns. In the basin of the Black Sea It is most intensive — 130 microns — due to the solubility of mountain rocks and the abundance of atmospheric precipitation. To the east the chemical denudation becomes weaker. Denudation according to the suspended alluvium of rivers makes up 130 million tons, and the annual layer—150 microns. It is most intensive in the basins of Samur and Sulak — up to 3500 tons per sq. km. The involved alluvium makes from 10 to 50 per cent of the suspended one.</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>
