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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">geomgou</journal-id><journal-title-group><journal-title xml:lang="ru">Географическая среда и живые системы</journal-title><trans-title-group xml:lang="en"><trans-title>Geographical Environment and Living Systems</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2712-7613</issn><issn pub-type="epub">2712-7621</issn><publisher><publisher-name>Московский государственный областной университет</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">geomgou-867</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>Статьи</subject></subj-group></article-categories><title-group><article-title>КЛАССИФИКАЦИЯ И ОСОБЕННОСТИ ОПОЛЗНЕЙ ХАШТИНСКОЙ ОБЛАСТИ (Северо-Западный ИРАН )</article-title><trans-title-group xml:lang="en"><trans-title>Landslides characteristics and classificationsin hashtjin area (Northwest of - Iran)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="western" xml:lang="en"><surname>Talaei</surname><given-names>Reza</given-names></name></name-alternatives><email xlink:type="simple">RZTALA @yahoo.
com</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="western" xml:lang="en"><surname>Sardar</surname><given-names>Samadov. .</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="en" id="aff-1"><institution>Baku State University</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2010</year></pub-date><pub-date pub-type="epub"><day>27</day><month>05</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><fpage>90</fpage><lpage>94</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Talaei R., Sardar S..., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Talaei R., Sardar S...</copyright-holder><copyright-holder xml:lang="en">Talaei R., Sardar S...</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://www.geoecosreda.ru/jour/article/view/867">https://www.geoecosreda.ru/jour/article/view/867</self-uri><abstract><p>Идентификация и признание различных типов оползня в области
Hashtjin (ИРАН СЗ), и их определенные особенности были главной целью этого исследо-
вания. Результаты исследований показали, что более чем 13% региона подвергается воз-
действиям оползней. Оползни разделены на две категории: единственные и общие. 55%
оползней активны и движения их изменяются различными агентами. Приблизительно
95% убытков происходит в областях сельского хозяйства и пастбищах.</p></abstract><trans-abstract xml:lang="en"><p>Identification and recognition of various types of landslide in Hashtjin area
(NW-IRAN), and their specific characteristics were the main purpose of this study. The results
of this study showed that Hashtjin is of the area most susceptible to landslide in Iran wite more
than 13% its surface being affected by mass movement activity. Two categories of landslide
have been identified, single and zone landslides Active landslides make up 55% of the total
number of the landslides, and they vary in characteristics and factors. Approximately, 95% of
the damages occur in pastures and agricultural lands.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>оползень</kwd><kwd>особенности</kwd><kwd>классификации</kwd><kwd>восприимчивые области и убытки</kwd></kwd-group><kwd-group xml:lang="en"><kwd>landslide</kwd><kwd>characteristics</kwd><kwd>classifications</kwd><kwd>susceptible areas and damages</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Ansari F. and Blurchi M.J. (1994) Landslide in the Ardebil province, geotechnical and structural land shake management, geological science organization of Iran, pp. 46.</mixed-citation><mixed-citation xml:lang="en">Ansari F. and Blurchi M.J. 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