Please use this identifier to cite or link to this item: http://dspace.onu.edu.ua:8080/handle/123456789/2401
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dc.contributor.authorKonikov, Yevhenii G.-
dc.contributor.authorPedan, Halyna S.-
dc.contributor.authorПедан, Галина Сергіївна-
dc.date.accessioned2012-04-23T11:16:43Z-
dc.date.available2012-04-23T11:16:43Z-
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.uk
dc.identifier.urihttp://dspace.onu.edu.ua:8080/handle/123456789/2401-
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 Tilgulsky Liman (known as Deliogolsky Liman before the XVII century CE), which covers an area of -14 km2 and is more than 4 km wide, is located on the border between Odessa and Nikolaev Regions. To the north, the baymouth barrier abuts the Odessa- Nikolaev highway.The mainland shores of the liman form the western and eastern boundaries of the barrier (Fig. 40,42).Its surface is covered by salt-rich soils (solonchak and solonets),solonchak meadows, and partially by steppe xerophyte areas. Large seaward portions of the barrier have been developed for resort complexes, recreation facilities,and motels.The erosional depth of Tiligul River at the mouth of the modern liman reaches approximately 38 m.uk
dc.language.isoenuk
dc.publisherAstroprintuk
dc.subjectTilgulsky Limanen
dc.subjectNikolaev Regionsen
dc.titleBaymouth barrier of Tiligul liman (TLBB)en
dc.typeArticleuk
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