In:
Quaestiones Geographicae, Adam Mickiewicz University Poznan, Vol. 33, No. 3 ( 2014-09-01), p. 7-15
Abstract:
The 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
Type of Medium:
Online Resource
ISSN:
2081-6383
DOI:
10.2478/quageo-2014-0025
Language:
English
Publisher:
Adam Mickiewicz University Poznan
Publication Date:
2014
detail.hit.zdb_id:
3100991-8
detail.hit.zdb_id:
2690180-8