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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-2720</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>Научные сообщения</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Short communications</subject></subj-group></article-categories><title-group><article-title>Скорость современной денудации Крымских гор</article-title><trans-title-group xml:lang="en"><trans-title>Recent erosion rate in the Crimean Mountains</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>Благоволин</surname><given-names>Н. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Blagovolin</surname><given-names>N. S.</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>Клюкин</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Klyukin</surname><given-names>A. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт географии АН СССР</institution><country>Россия</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Симферопольский университет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1987</year></pub-date><pub-date pub-type="epub"><day>17</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>42</fpage><lpage>49</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Благоволин Н.С., Клюкин А.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Благоволин Н.С., Клюкин А.А.</copyright-holder><copyright-holder xml:lang="en">Blagovolin N.S., Klyukin A.A.</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/2720">https://geomorphology.igras.ru/jour/article/view/2720</self-uri><abstract><p>The rate of chemical, mechanical and total «transit» erosion of the Crimean moun'tains was calculated and corresponding schematic maps were compiled on the basis of data on rivers solid and chemical discharge. The chemical erosion rate averages to 0.007 mm per year, it is prevalent over the karst region of the Main Ridge (about 20% of the total area of the Crimean mountains) where the Upper Jurassic limestones are prone to both surficial and subterraneous dissolution. Mechanical erosion proceeds at a rate of 0.05 mm per year and reaches its maximum in the regions built of terrigenous ilysch. Total «transit» erosion on the average is about 0.06 mm per year, with allowance for flash floods and mudilows it may be high as 0.08 mm per year. Rivers remove from the Crimean mountains about 0,7 mln tons of solid and dissolved substance per year, almost 90% of the quantity being debris produced by the mechanical erosion.</p></abstract><trans-abstract xml:lang="en"><p>The rate of chemical, mechanical and total «transit» erosion of the Crimean moun'tains was calculated and corresponding schematic maps were compiled on the basis of data on rivers solid and chemical discharge. The chemical erosion rate averages to 0.007 mm per year, it is prevalent over the karst region of the Main Ridge (about 20% of the total area of the Crimean mountains) where the Upper Jurassic limestones are prone to both surficial and subterraneous dissolution. Mechanical erosion proceeds at a rate of 0.05 mm per year and reaches its maximum in the regions built of terrigenous ilysch. Total «transit» erosion on the average is about 0.06 mm per year, with allowance for flash floods and mudilows it may be high as 0.08 mm per year. Rivers remove from the Crimean mountains about 0,7 mln tons of solid and dissolved substance per year, almost 90% of the quantity being debris produced by the mechanical erosion.</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>
