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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-3070</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>Экологическая и прикладная геоморфология</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Ecological and Applied Geomorphology</subject></subj-group></article-categories><title-group><article-title>Геоморфологические аспекты природно-техногенных кризисов и катастроф в переходных зонах от континента к океану</article-title><trans-title-group xml:lang="en"><trans-title>Geomorphological aspects of natural-technogenic crises-catastrophs within zones of continent-ocean transition</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>Александров</surname><given-names>С. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Aleksandrov</surname><given-names>S. M.</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>Институт географии РАН</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1993</year></pub-date><pub-date pub-type="epub"><day>03</day><month>02</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><issue-title>Геоморфология</issue-title><fpage>37</fpage><lpage>43</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Александров С.М., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Александров С.М.</copyright-holder><copyright-holder xml:lang="en">Aleksandrov S.M.</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/3070">https://geomorphology.igras.ru/jour/article/view/3070</self-uri><abstract><p>Significant differences in the intensity of the present-day genetically different geomorphic processes should be taken into account when classifying natural hazards, some catastrophic processes, such as infrequent but extreme (in wave height) storms, and even more so tsunamis, cause damage comparable to that resulting from long-term marine erosion by medium-high waves. Natural-technogenic processes are close in their destructive power over short time interval to anomalous and catastrophic natural phenomena.</p></abstract><trans-abstract xml:lang="en"><p>Significant differences in the intensity of the present-day genetically different geomorphic processes should be taken into account when classifying natural hazards, some catastrophic processes, such as infrequent but extreme (in wave height) storms, and even more so tsunamis, cause damage comparable to that resulting from long-term marine erosion by medium-high waves. Natural-technogenic processes are close in their destructive power over short time interval to anomalous and catastrophic natural phenomena.</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>
