Please use this identifier to cite or link to this item: http://dspace.onu.edu.ua:8080/handle/123456789/2395
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dc.contributor.authorKonikov, Yevhenii G.-
dc.contributor.authorPedan, Halyna S.-
dc.contributor.authorKravchuk, Anna O.-
dc.contributor.authorПедан, Галина Сергіївна-
dc.date.accessioned2012-04-23T10:37:00Z-
dc.date.available2012-04-23T10:37:00Z-
dc.date.issued2006-
dc.identifier.citationBlack sea – mediterranean corridor during the last 30 ky: sea level change and human adaptation (2005–2009) : ІІ plenary meeting and field trip of project IGCP-521 (Odessa, 20–28 August 2006). – Odessa : Astroprint, 2006.-
dc.identifier.urihttp://dspace.onu.edu.ua:8080/handle/123456789/2395-
dc.descriptionДруга пленарна конференція та польові екскурсії з Проекту IGCP-521 «Чорноморсько-Середземноморський Коридор упродовж останніх 30 тисяч років: мінливість рівня моря й адаптація людини» (2005-2009).Путівник.-Одеса:Астрапринт,2006uk
dc.description.abstractThe ancient city of Olbia is situated on the paleo-slope of a landslide.The Upper City sits on the plateau,with absolute elevations of 38-42 m (Fig. 8).The Lower City is on the upper landslide terrace,which is 40-85 m wide and has an elevation of 6.5-12.5 m.The surface of the plateau,slope,and terrace are covered by diluvium and cultural layers totaling on average 4-6 m in thickness.Part of the Lower City and the port are currently submerged beneath waters of Bugsky Liman and are located on the lower landslide terrace.uk
dc.language.isoenuk
dc.publisherAstroprintuk
dc.subjectLower Plioceneen
dc.subjectBugsky Limanen
dc.titleAncient landslide (Olbia) on the right (west) shore of Dnieper-Bugsky limanen
dc.typeArticle-
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