Geometria i rozwój wałów lodowo-morenowych na obszarze moreny kutnowskiej: zapis w litofacjach i strukturach deformacyjnych osadów supraglacjalnych w stanowisku Daszyna

The ice-cored ridges are important for palaeogeographical studies of retreating margins of glaciers. Earlier recon-structions of ice-cored ridges in marginal zones of the Pleistocene ice-sheets have been made based on sedimentological studies.Applying such approach, research were able only to show i...

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Published inActa geographica Lodziensia no. 116; pp. 189 - 204
Main Authors Włodarski, Wojciech, ORŁOWSKA, ANNA, WASILUK, RADOSŁAW
Format Journal Article
LanguagePolish
Published Lódz Łódzkie Towarzystwo Naukowe 2024
Lodz Scientific Society
Lódzkie Towarzystwo Naukowe
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Summary:The ice-cored ridges are important for palaeogeographical studies of retreating margins of glaciers. Earlier recon-structions of ice-cored ridges in marginal zones of the Pleistocene ice-sheets have been made based on sedimentological studies.Applying such approach, research were able only to show in which degree depressions between ice-cored ridges influencedspatial variations in depositional processes. There is possible to determine more precise characteristics of ice-cored ridgesgeometry based on detailed analysis of collapse structures. The shape, elongation and orientation of ice-cored ridges can bederived from geometry and kinematics of folds and faults as major elements of the collapse structures. Integration sedimento-logical studies of supraglacial deposits with analysis of collapse structures also allows to determine the evolution of ice-coredridges up to final deicing. This approach is the subject of case study performed in Daszyna site located in the Kutno Moraine.
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ISSN:0065-1249
2451-0319
DOI:10.26485/AGL/2024/116/11