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 in | Acta geographica Lodziensia no. 116; pp. 189 - 204 |
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Main Authors | , , |
Format | Journal Article |
Language | Polish |
Published |
Lódz
Łódzkie Towarzystwo Naukowe
2024
Lodz Scientific Society Lódzkie Towarzystwo Naukowe |
Subjects | |
Online Access | Get full text |
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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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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 |
ISSN: | 0065-1249 2451-0319 |
DOI: | 10.26485/AGL/2024/116/11 |