Prediction of the Vistula channel development between Wloclawek and Torun: evaluation with regard to the new geological survey

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dc.contributor.authorBabiński, Zygmunt
dc.contributor.authorHabel, Michał
dc.contributor.authorChalov, Sergey
dc.date.accessioned2016-12-02T12:59:10Z
dc.date.available2016-12-02T12:59:10Z
dc.date.issued2014
dc.description.abstractThe aim of this paper is to present the geological structure of the Vistula river valley floor as the modifying factor of fluvial processes and present the development conditions of the contemporary Vistula river channel, which underwent marked transformation due to bed erosion and lateral erosion below the Włocławek reservoir. The analysis of the geological data and the geological survey conducted at the study reach of the Vistula between Włocławek and Toruń resulted in an image of the geological structure of the channel bed along the longitudinal profile.pl_PL
dc.identifier.citationQuaestiones Geographicae vol. 33 (3), 2014, pp. 7-15pl_PL
dc.identifier.issn0137-477X
dc.identifier.urihttp://hdl.handle.net/10593/16065
dc.language.isoengpl_PL
dc.publisherWydział Nauk Geograficznych i Geologicznych Uniwersytetu im. Adama Mickiewiczapl_PL
dc.rightsinfo:eu-repo/semantics/openAccesspl_PL
dc.subjectgeological surveypl_PL
dc.subjectgeological structurepl_PL
dc.subjectfluvial processespl_PL
dc.subjectVistula Riverpl_PL
dc.titlePrediction of the Vistula channel development between Wloclawek and Torun: evaluation with regard to the new geological surveypl_PL
dc.typeArtykułpl_PL

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Quaestiones Geographicae vol. 33 (3), 2014