Unravelling the complex nature of the Upper Weichselian till section at Gdynia Babie Doły, northern Poland
Loading...
Date
2016-04
Authors
Advisor
Editor
Journal Title
Journal ISSN
Volume Title
Publisher
Instytut Geologii UAM
Title alternative
Abstract
The complexity of glacial sequences may increase when these formed underneath ice sheets despite subsequent changes
in their extent that are accompanied by alterations in the direction of the ice flow. Our aim was to determine whether
or not changes in ice sheet dynamics during the Late Weichselian are also recorded in sediments formed north of the
area of its fluctuating margin (i.e., where the ice sheet prevailed independent of such fluctuations). It is shown that in
these areas such a record could have occurred, as documented by results of till studies at Babie Doły. The examination
was carried out using several analyses: lithofacies properties of sediments, petrographic till composition (fine gravel
fraction, indicator erratics), till matrix CaCO3 content, till fabric, as well as orientation of striae on the top surfaces of
large clasts. In parallel, datings of sub- and supra-till sediments using the TL method were carried out. The basal till at
Babie Doły represents almost the entire Upper Weichselian, but it can be divided into subunits whose features indicate
different ice flow directions and debris supply. The lower subunit developed as a result of the palaeo-ice stream along
the main axis of the Baltic Sea (from the north), expanding to areas adjacent to the depression of the Gulf of Gdańsk. The
upper subunit developed when the influence of the palaeo-ice stream in the study area decreased, the main role having
been taken over by the ice flowing from the northwest. The till analysed also shows considerable lateral variation,
indicative of the mosaic nature of subglacial sedimentation. We consider the diversity of permeability of deposits over
which the ice sheet extended to be the prime factor that determined such a situation.
Description
Sponsor
Keywords
subglacial processes, till fabric, till petrography, Gulf of Gdańsk, Pleistocene, Fennoscandian Ice Sheet
Citation
Geologos, 2016, 22, 1, pp.15-32
Seria
ISBN
ISBN 978-83-232187-4-6
ISSN
ISSN 1426-8981