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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="en"><front><journal-meta><journal-id journal-id-type="publisher-id">gesj</journal-id><journal-title-group><journal-title xml:lang="en">GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY</journal-title><trans-title-group xml:lang="ru"><trans-title>GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2071-9388</issn><issn pub-type="epub">2542-1565</issn><publisher><publisher-name>Russian Geographical Society</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.24057/2071-9388-2011-4-1-59-68</article-id><article-id custom-type="elpub" pub-id-type="custom">gesj-229</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="en"><subject>ENVIRONMENT</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>Окружающая среда</subject></subj-group></article-categories><title-group><article-title>LANDSLIDES IN A RURAL MOUNTAINOUS REGION: DAMAGING AND RESOURCE-FORMING IMPACTS (SOUTH CAUCASUS, GEORGIA)</article-title><trans-title-group xml:lang="ru"><trans-title></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>Gracheva</surname><given-names>Raisa</given-names></name></name-alternatives><bio xml:lang="en"><p>Institute of Geography of RAS, Staromonetny per. 29 Moscow 119017 Russia</p></bio><email xlink:type="simple">gracheva04@list.ru</email></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="western" xml:lang="en"><surname>Urushadze</surname><given-names>Tengiz</given-names></name></name-alternatives><bio xml:lang="en"><p>Ivane Javakhishvili Tbilisi State University, 3 Ilia Chavchavadze Ave. 0128 Tbilisi, Georgia</p></bio><email xlink:type="simple">t_urushadze@yahoo.com</email></contrib></contrib-group><pub-date pub-type="collection"><year>2011</year></pub-date><pub-date pub-type="epub"><day>01</day><month>03</month><year>2011</year></pub-date><volume>4</volume><issue>1</issue><fpage>59</fpage><lpage>68</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Gracheva R., Urushadze T., 2011</copyright-statement><copyright-year>2011</copyright-year><copyright-holder xml:lang="ru">Gracheva R., Urushadze T.</copyright-holder><copyright-holder xml:lang="en">Gracheva R., Urushadze T.</copyright-holder><license 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://ges.rgo.ru/jour/article/view/229">https://ges.rgo.ru/jour/article/view/229</self-uri><abstract><p>Catastrophic loss of soils and slope sediments by landslides causes destruction of mountainous environment and outflow of population from affected areas. However, the role of landslides in mountainous regions goes beyond direct destructive activity. The sliding mass expose surfaces for weathering and accumulate loose mineral material, the vital resource for mountain biota and population thus starting new cycles in ecosystems development, forming new habitats for biota and, in some cases, new lands for farming. A chronological sequence of landslides and their adaptation for human needs was studied in Adjara province, the South Caucasus mountainous region, Georgia. As a rule, in 15 years, a thin and compacted soil layer is formed on low and mound surface of a landslide. In 30 years, people start recultivation of the landslide area. After 40–60 years, the landslide area is used as a hayfield. 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