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Zastosuj identyfikator do podlinkowania lub zacytowania tej pozycji: http://hdl.handle.net/20.500.12128/6769
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dc.contributor.authorKozyreva, Elena A.-
dc.contributor.authorSzczypek, Tadeusz-
dc.contributor.authorTrzcinskij, Jurij B.-
dc.contributor.authorWika, Stanisław-
dc.date.accessioned2018-10-17T08:25:13Z-
dc.date.available2018-10-17T08:25:13Z-
dc.date.issued2007-
dc.identifier.citationActa Geographica Silesiana, [T.] 1 (2007), s. 29-34pl_PL
dc.identifier.issn1897-5100-
dc.identifier.urihttp://hdl.handle.net/20.500.12128/6769-
dc.description.abstractAgainst the background of general characteristics of physicogeographical conditions of northern Baikal and its neighbourhood the origin (lagoon formed in result of accumulation of lacustrine and fluvial deposits of the Verkhnaya Angara and Kichera) and de-velopment of Yarki island were presented, taking the special account into its contemporary degradation under the influence of natural factors (general development of Baikal rift) and anthropogenic ones: tourism development, vegetation disturbing, dune blowing out and their washing by Baikal waves, intensified after dam building in Irkutsk. The contemporary aeolian relief of island was also described (predominance of blown old dunes and diversifying of aeolian relief by north-eastern and – to smaller degree – by south-western winds, and vegetation, which is floristically poor, weakly diversified and to significant degree changed by human being, was also presented.pl_PL
dc.language.isoplpl_PL
dc.rightsUznanie autorstwa-Użycie niekomercyjne-Bez utworów zależnych 3.0 Polska*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/pl/*
dc.subjectkrajobraz eolicznypl_PL
dc.subjectwyspa Jarkipl_PL
dc.subjectBajkałpl_PL
dc.titleKrajobraz eoliczny wyspy Jarki na północnym Bajkalepl_PL
dc.typeinfo:eu-repo/semantics/articlepl_PL
dc.relation.journalActa Geographica Silesianapl_PL
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