Ice-Sheet Dynamics of Warta Glaciation (Saale) in the Marginal Zone of Knyszewicze Area, Northeastern Poland

Rychel, J.; Woronko, B.; Karasiewicz, M. T.; Szymczuk, P.; Morawski, M.

doi:10.1515/squa-2015-0007

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Ice-Sheet Dynamics of Warta Glaciation (Saale) in the Marginal Zone of Knyszewicze Area, Northeastern Poland

Autorzy

Rychel J. , Woronko B. , Karasiewicz M. T. , Szymczuk P. , Morawski M.

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DOI

10.1515/squa-2015-0007

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Abstrakty

The paper presents a research on a marginal zone near Knyszewicze in the southern part of Sokółka Hills (northeastern Poland). Terminal moraine hills are arranged amphitheatrically in a lobal pattern. Dynamics of the Knyszewicze frontal ice-sheet lobe during the Saale Glaciation and successive stages of the marginal zone near the village of Knyszewicze were reconstructed based on sedimentary and geomorphological analysis, using a digital elevation model and morpholineaments. Three main phases of the Knyszewicze glacial-lobe activity were identified including accumulation of glaciofluvial deposits, advances of the ice margin and ice-lobe retreat. Moraine hills developed at a stable ice-lobe terminus, initially as short end-moraine fans with the following sequence of lithofacies Gh=>SGh=>Sh or Gm=>Gh=>Sh. Such a sequence indicates cyclic sheet-floods. During a small but dynamic advance of the ice sheet terminus, these deposits were moved forward and monoclinally folded, then furrowed with sloping faults due to horizontal pressure. Typical thrust-block push moraines developed in this way. Ice sheet advance took place when permafrost was present in the substratum and very high water pressure occurred at glacial terminus. Inside a lobal configuration of moraines, there is a rich inventory of glacial forms with a classic terminal depression in the central part. Based on this landform pattern, their shape, rhythm and glaciotectonic disturbances, the land relief may be referred to as a hill-hole pair. The structure of Horczaki Knoll, deposited on the sub-Quaternary tectonic structure, significantly contributed to a development of this marginal zone.

Słowa kluczowe

ice lobe marginal zone glaciotectonic disturbances thrust-block push moraines morpholineaments

Wydawca

Institute of Geological Science Polish Academy of Science

Czasopismo

Studia Quaternaria

Rocznik

2015

Tom

Vol. 32, Nr 2

Strony

79--90

Opis fizyczny

Bibliogr. 76 poz., rys.

Twórcy

autor

Rychel J.

joanna.rychel@pgi.gov.pl

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

autor

Woronko B.

bworonko@uw.edu.pl

Faculty of Geology University of Warsaw, Żwirki i Wigury 93, 02-089 Warsaw, Poland

autor

Karasiewicz M. T.

mtkar@umk.pl

Faculty of Earth Sciences, Nicolaus Copernicus University, Lwowska 1, 87-100 Toruń, Poland

autor

Szymczuk P.

Faculty of Geography and Regional Studies, University of Warsaw, Krakowskie Przedmieście 30, 00-927 Warsaw, Poland

autor

Morawski M.

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

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