<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD JATS (Z39.96) Journal Publishing DTD v1.3 20210610//EN" "JATS-journalpublishing1-3.dtd">
<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-3498</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>Эволюция крутых склонов Крымских гор</article-title><trans-title-group xml:lang="en"><trans-title>Evolution of steep slopes 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>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-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Симферопольский государственный университет</institution><country>Украина</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1998</year></pub-date><pub-date pub-type="epub"><day>21</day><month>12</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>59</fpage><lpage>66</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Клюкин А.А., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Клюкин А.А.</copyright-holder><copyright-holder xml:lang="en">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/3498">https://geomorphology.igras.ru/jour/article/view/3498</self-uri><abstract><p>The slopes with inclination close to the angle of repose constitute a specific group and present an intermediate stage in the transformation of steep slopes made of solid rocks into less steep slopes covered by soil. In the climate that is transitional from Mediterranean to temperate continental they develop being controlled by the intensive deluvia demolition and creep.</p></abstract><trans-abstract xml:lang="en"><p>The slopes with inclination close to the angle of repose constitute a specific group and present an intermediate stage in the transformation of steep slopes made of solid rocks into less steep slopes covered by soil. In the climate that is transitional from Mediterranean to temperate continental they develop being controlled by the intensive deluvia demolition and creep.</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>
