Prediction of the Vistula Channel Development Between Wloclawek and Torun: Evaluation with Regard to the New Geological Survey-Reference-Cited by-同舟云学术

Prediction of the Vistula Channel Development Between Wloclawek and Torun: Evaluation with Regard to the New Geological Survey

Published:2014-09-01 Issue:3 Volume:33 Page:7-15
ISSN:2081-6383
Container-title:Quaestiones Geographicae
language:en
Short-container-title:

Author:

Babiński Zygmunt¹,Habel Michał¹,Chalov Sergey²

Affiliation:

1. Department of Waterways, Kazimierz Wielki University in Bydgoszcz, Poland

2. Faculty of Geography, Moscow State University, Moscow, Russia

Abstract

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

Publisher

Walter de Gruyter GmbH

Subject

General Earth and Planetary Sciences

Link

https://www.sciendo.com/pdf/10.2478/quageo-2014-0025

Reference24 articles.

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3. Babiński Z., 2002. Wpływ zapór na procesy korytowe rzek aluwialnych (Impact of the dams on the fluvial processes on alluvial rivers). Akademia Bydgoska im. Kazimierza Wielkiego.

4. Babiński Z., Habel M., 2009. Dynamika strefy akumulacyjnej poniżej czoła strefy erozyjnej Zbiornika Włocławskiego (Dynamics of the accumulation zone below erosion zone of the Włocławek Reservoir). In: A.T. Jankowski, D.

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