Postglacial morpholineaments as an indicator of ice sheet dynamics during the Saale Glaciation in the Białystok Plateau and Sokółka Hills (NE Poland)

Rychel, J.; Morawski, M.

doi:10.7306/gq.1352

Artykuł - szczegóły

Tytuł artykułu

Postglacial morpholineaments as an indicator of ice sheet dynamics during the Saale Glaciation in the Białystok Plateau and Sokółka Hills (NE Poland)

Autorzy

Rychel J. , Morawski M.

Treść / Zawartość

Pełne teksty:

Rychel_J_Postglacial_Geol. Quart._Vol. 61, No 2_2017.pdf

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Identyfikatory

DOI

10.7306/gq.1352

Warianty tytułu

Języki publikacji

Abstrakty

The palaeogeographical reconstruction of the deglaciation process in NE Poland during the Odranian Glaciation Wartanian Stadial (Saale MIS 6) is based mainly on the analysis of glacial morpholineaments, performed using the GIS programs that provide us with better understanding of the glacial landscape evolution, spatial reconstruction of glacial processes, and postglacial landscape development. Analysis of postglacial morpholineaments was carried out based on the Digital Elevation Model (DEM) as well as geological, geomorphological and topographic maps. It resulted in the delimitation of visible linear postglacial landforms, their identification and classification, and the determination of their genetic and chronological relations. Directions of the lineaments were determined through quantitative analysis. Qualitative analysis was applied to determine the spatial and temporal sequence of events, directions of ice movement and its range. Two glacial lobes, Biebrza and Neman, existed in the north-western part of the Białystok Plateau and Sokółka Hills during the last glacial advance. The lobed nature of the ice sheet can be confirmed by field data collected from, e.g., sites in Knyszewicze, and by topographic analysis of Quaternary sediments, combined with their thickness and genesis. The obtained reconstruction of the last glacial advance and retreat in the study area can be used in further regional discussions on the character and dynamics of the last glaciation in this region.

Słowa kluczowe

morpholineament Saalian ice-sheet movement lobe NE Poland

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2017

Tom

Vol. 61, No. 2

Strony

334--349

Opis fizyczny

Bibliogr. 95 poz., rys., tab., wykr.

Twórcy

autor

Rychel J.

joanna.rychel@pgi.gov.pl

Polish Geological Institute - National Research Institute, Rakowiecka 4, 00-975 Warszawa, Poland

autor

Morawski M.

l'immeuble SarSaara Lot 124B-2 Yoff Toundoup Rya, Dakar, Senegal

Bibliografia

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Uwagi

Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017).

Typ dokumentu

Bibliografia

Identyfikator YADDA

bwmeta1.element.baztech-1f1ec364-7dcf-4b2f-8b78-a9f9ff914f7b