Southern Baltic area during the last deglaciation
In the Polish economical zone of the Baltic Sea there are boulder fields (residuum of end moraines), remnants of end moraines, glaciofluvial deltas, eskers, and ice·dam lake deposits formed during a decay of the last Scandinavian ice sheet. Landforms and deposits of three ice marginal zones were dis...
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Polish Geological Institute-National Research Institute
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ftjgq:oai:geojournals.pgi.gov.pl:article/8189 2024-09-15T18:12:26+00:00 Southern Baltic area during the last deglaciation Uścinowicz, Szymon 2013-02-14 application/pdf https://gq.pgi.gov.pl/article/view/8189 eng eng Polish Geological Institute-National Research Institute https://gq.pgi.gov.pl/article/view/8189/pdf_281 10.7306/gq.v43i2.8189.g6733 https://gq.pgi.gov.pl/article/view/8189 Geological Quarterly; Vol. 43 No. 2 (1999); 137-148 Geological Quarterly; Tom 43 Nr 2 (1999); 137-148 1641-7291 10.7306/gq.v43i2 Baltic Sea Słupsk Bank Southern Middle Bank Pleistocene Late Glacial deglaciation info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2013 ftjgq https://doi.org/10.7306/gq.v43i2 2024-07-30T03:29:08Z In the Polish economical zone of the Baltic Sea there are boulder fields (residuum of end moraines), remnants of end moraines, glaciofluvial deltas, eskers, and ice·dam lake deposits formed during a decay of the last Scandinavian ice sheet. Landforms and deposits of three ice marginal zones were distinguished in the Southern Baltic. The Gardno Phase probably corresponds to the Halland-West Sk¯ne Phase, dated at ca. 14 ka BP, and to the Middle Lithuanian Phase. The Słupsk Bank Phase is marked at a bottom of the Baltic Sea by boulder fields on the Słupsk Bank and by remnants of end moraines in the southern Bornholm Basin and the western Gdańsk Basin. It is to be correlated with the ice limit in Sk¯ne, dated at 13.5 ka BP, and with the North Lithuanian Phase at ca. 13.2 ka BP. The Southern Middle Bank Phase, marked by glaciofluvial deltas on this bank and by end moraines in the central Bornholm Basin, most probably corresponds to the ice margin in Sk¯ne, dated at 13.0-12.9 ka BP, and to the Otep¬¬ Phase in the east. Article in Journal/Newspaper Ice Sheet Geological Quarterly |
institution |
Open Polar |
collection |
Geological Quarterly |
op_collection_id |
ftjgq |
language |
English |
topic |
Baltic Sea Słupsk Bank Southern Middle Bank Pleistocene Late Glacial deglaciation |
spellingShingle |
Baltic Sea Słupsk Bank Southern Middle Bank Pleistocene Late Glacial deglaciation Uścinowicz, Szymon Southern Baltic area during the last deglaciation |
topic_facet |
Baltic Sea Słupsk Bank Southern Middle Bank Pleistocene Late Glacial deglaciation |
description |
In the Polish economical zone of the Baltic Sea there are boulder fields (residuum of end moraines), remnants of end moraines, glaciofluvial deltas, eskers, and ice·dam lake deposits formed during a decay of the last Scandinavian ice sheet. Landforms and deposits of three ice marginal zones were distinguished in the Southern Baltic. The Gardno Phase probably corresponds to the Halland-West Sk¯ne Phase, dated at ca. 14 ka BP, and to the Middle Lithuanian Phase. The Słupsk Bank Phase is marked at a bottom of the Baltic Sea by boulder fields on the Słupsk Bank and by remnants of end moraines in the southern Bornholm Basin and the western Gdańsk Basin. It is to be correlated with the ice limit in Sk¯ne, dated at 13.5 ka BP, and with the North Lithuanian Phase at ca. 13.2 ka BP. The Southern Middle Bank Phase, marked by glaciofluvial deltas on this bank and by end moraines in the central Bornholm Basin, most probably corresponds to the ice margin in Sk¯ne, dated at 13.0-12.9 ka BP, and to the Otep¬¬ Phase in the east. |
format |
Article in Journal/Newspaper |
author |
Uścinowicz, Szymon |
author_facet |
Uścinowicz, Szymon |
author_sort |
Uścinowicz, Szymon |
title |
Southern Baltic area during the last deglaciation |
title_short |
Southern Baltic area during the last deglaciation |
title_full |
Southern Baltic area during the last deglaciation |
title_fullStr |
Southern Baltic area during the last deglaciation |
title_full_unstemmed |
Southern Baltic area during the last deglaciation |
title_sort |
southern baltic area during the last deglaciation |
publisher |
Polish Geological Institute-National Research Institute |
publishDate |
2013 |
url |
https://gq.pgi.gov.pl/article/view/8189 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Geological Quarterly; Vol. 43 No. 2 (1999); 137-148 Geological Quarterly; Tom 43 Nr 2 (1999); 137-148 1641-7291 10.7306/gq.v43i2 |
op_relation |
https://gq.pgi.gov.pl/article/view/8189/pdf_281 10.7306/gq.v43i2.8189.g6733 https://gq.pgi.gov.pl/article/view/8189 |
op_doi |
https://doi.org/10.7306/gq.v43i2 |
_version_ |
1810450023873249280 |