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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-2987</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>Изучение опасных природных процессов в Калмыкии и Предкавказье по аэро- и космоснимкам</article-title><trans-title-group xml:lang="en"><trans-title>Studies of natural hazards in Kalmykia and the Caucasian forelands using aerial and space photoes</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>Пастушкова</surname><given-names>С. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Pastushkova</surname><given-names>S. 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>ПНИИИС</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1992</year></pub-date><pub-date pub-type="epub"><day>21</day><month>01</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><issue-title>Геоморфология</issue-title><fpage>32</fpage><lpage>36</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Пастушкова С.А., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Пастушкова С.А.</copyright-holder><copyright-holder xml:lang="en">Pastushkova S.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/2987">https://geomorphology.igras.ru/jour/article/view/2987</self-uri><abstract><p>The paper discusses possibilities to identify some natural hazards from images on topographic maps and aerial photoes. Particular meso- and micro-Iandforms produce characteristic pattern which indicate such phenomena as potential subsidence in loess, sheet and rill erosion, salinization of soils, suffusion, karst and some others. Some quantitative characteristics of dangerous processes which are important from the practical point of view may be obtained on the basis of the found functional relationships between quantitative indices of landscape pattern and the geodynamic conditions of key sites.</p></abstract><trans-abstract xml:lang="en"><p>The paper discusses possibilities to identify some natural hazards from images on topographic maps and aerial photoes. Particular meso- and micro-Iandforms produce characteristic pattern which indicate such phenomena as potential subsidence in loess, sheet and rill erosion, salinization of soils, suffusion, karst and some others. Some quantitative characteristics of dangerous processes which are important from the practical point of view may be obtained on the basis of the found functional relationships between quantitative indices of landscape pattern and the geodynamic conditions of key sites.</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>
