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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">sergeogr</journal-id><journal-title-group><journal-title xml:lang="ru">Известия Российской академии наук. Серия географическая</journal-title><trans-title-group xml:lang="en"><trans-title>Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2587-5566</issn><issn pub-type="epub">2658-6975</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.31857/S2587556622020054</article-id><article-id custom-type="elpub" pub-id-type="custom">sergeogr-1536</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>Природные процессы и динамика геосистем</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Natural Processes and Dynamics of Geosystems</subject></subj-group></article-categories><title-group><article-title>Кратерные и кальдерные озера Дальнего Востока России: морфология котловин и динамика развития</article-title><trans-title-group xml:lang="en"><trans-title>Crater and Caldera Lakes of Far East of Russia: Morphology of Basins and Dynamic of Development</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>Козлов</surname><given-names>Д. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Kozlov</surname><given-names>D. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Южно-Сахалинск</p></bio><bio xml:lang="en"><p>Yuzhno-Sakhalinsk</p></bio><email xlink:type="simple">kozlovdn@bk.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Лебедева</surname><given-names>Е. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Lebedeva</surname><given-names>E. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Москва</p></bio><bio xml:lang="en"><p>Moscow</p></bio><email xlink:type="simple">Ekaterina.lebedeva@gmail.com</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт морской геологии и геофизики ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Marine Geology and Geophysics FEB RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт географии РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Geography RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>27</day><month>05</month><year>2022</year></pub-date><volume>86</volume><issue>2</issue><fpage>204</fpage><lpage>219</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Козлов Д.Н., Лебедева Е.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Козлов Д.Н., Лебедева Е.В.</copyright-holder><copyright-holder xml:lang="en">Kozlov D.N., Lebedeva E.V.</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://izvestia.igras.ru/jour/article/view/1536">https://izvestia.igras.ru/jour/article/view/1536</self-uri><abstract><p>По результатам комплекса полевых и камеральных работ получены и проанализированы данные по особенностям строения котловин и динамике развития 15 кратерных и кальдерных озер КурилоКамчатского региона. Рассчитаны их основные морфометрические характеристики. Установлено, что группа кальдерных озер менее однородна по всем морфометрическим показателям. Выявлено, что котловины водоемов одного генетического типа на Курильских островах и Камчатке схожи по формам и глубинам, но абсолютные высоты камчатских водоемов в целом больше курильских, впрочем, как нередко и размеры котловин. Изучение котловин 10 озер при помощи современной методики цифровой эхолокационной съемки позволило выявить специфические особенности морфологии котловин каждой из групп. Установлено, что котловины ряда кальдерных озер региона осложнены эксплозивными воронками, экструзивными или эффузивными куполами со следами гидротермальной деятельности; определены их параметры. Важной отличительной чертой многих вулканических озер является возможность стремительного изменения их основных характеристик (формы, объема, температуры, химического состава воды и др.) в широких пределах, что обусловлено особенностями функционирования близлежащих вулканических центров. По этим параметрам водоемы могут быть разделены на: 1) весьма динамичные молодые озера, расположенные в кратерах действующих вулканов или в активных кальдерах в непосредственной близости от них; 2) более стабильные, реликтовые водоемы в кальдерах спящих или потухших вулканов. Результаты повторных наблюдений позволили получить представление о примерных скоростях изменения уровней озер для интервалов в несколько десятилетий. Определена скорость роста подводного купола, обнаруженного авторами в 2016 г. в оз. Штюбеля (кальдера Ксудач, Камчатка). </p></abstract><trans-abstract xml:lang="en"><p>Based on the results of a set of field and cameral work data on the structural features of the basins and the dynamics of development of 15 crater and caldera lakes in the Kuril-Kamchatka region were obtained and analyzed. Their main morphometric characteristics were calculated. It was found that the group of caldera lakes is less homogeneous in all morphometric parameters. It was revealed that the basins of water bodies of the same genetic type on the Kuril Islands and Kamchatka are similar in shape and depth, but the absolute heights of Kamchatka water bodies are generally higher than those of the Kuril ones, however, as is often the size of the basins. The study of 10 lakes using the modern digital echolocation survey technique made it possible to reveal the specific features of the morphology of the basins of each of the groups. It was found that the basins of a number of caldera lakes in the region are complicated by explosive funnels, extrusive or effusive domes with traces of hydrothermal activity; their parameters were identified. An important distinguishing feature of many volcanic lakes is the possibility of rapid changes in their main characteristics (shape, volume, temperature, chemical composition of water, etc.) over a wide range, which is due to the peculiarities of the functioning of nearby volcanic centers. According to these parameters, volcanic lakes can be divided into: 1) very dynamic young lakes located in the craters of active volcanoes or active calderas in their immediate vicinity; 2) more stable, relict water bodies in the calderas of dormant or extinct volcanoes. The results of repeated observations after several decades made it possible to calculate the approximate rates of change in the levels of some lakes. It was found that the rate of fluctuations in the levels of caldera lakes is generally lower than that of crater lakes. The rate of growth of the underwater dome, discovered by the authors in 2016 in Lake Shtyubel (Ksudach caldera, Kamchatka), was determined. </p></trans-abstract><kwd-group xml:lang="ru"><kwd>вулканические озера</kwd><kwd>эксплозивная воронка</kwd><kwd>подводный купол</kwd><kwd>эхолокационная съемка</kwd><kwd>вулканическая деятельность</kwd><kwd>газогидротермы</kwd><kwd>Камчатка</kwd><kwd>Курильские острова</kwd></kwd-group><kwd-group xml:lang="en"><kwd>volcanic lakes</kwd><kwd>explosive funnel</kwd><kwd>underwater dome</kwd><kwd>echolocation survey</kwd><kwd>volcanic activity</kwd><kwd>gas hydrotherms</kwd><kwd>Kamchatka</kwd><kwd>Kuril Islands</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Анализ материалов выполнен в рамках тем государственных заданий ИМГиГ ДВО РАН и ИГ РАН (АААА-А19-119021990091-4, FMGE-2019-0005).</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Аракельянц А.Д., Ткаченко О.В. 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