Nowe znaleziska narzutniaków porfiru rombowego z Oslo na terenie północno-zachodniej Polski

NEW FINDS OF ERRATICS OF THE OSLO RHOMB PORPHYRY IN NORTH-WESTERN POLAND Summary Two specimens of Oslo rhomb porphyries find on the Wolin Island beach between Międzyzdroje and Grodno are extraordinary finds among the entire population of Scandinavian indicator erratics within glacial sediments in no...

Full description

Bibliographic Details
Main Author: Górska, Maria
Format: Article in Journal/Newspaper
Language:Polish
Published: Państwowy Instytut Geologiczny - PIB 2003
Subjects:
Online Access:https://gq.pgi.gov.pl/pg/article/view/14135
id ftjgq:oai:geojournals.pgi.gov.pl:article/14135
record_format openpolar
spelling ftjgq:oai:geojournals.pgi.gov.pl:article/14135 2023-05-15T16:40:42+02:00 Nowe znaleziska narzutniaków porfiru rombowego z Oslo na terenie północno-zachodniej Polski Górska, Maria 2003-07-18 application/pdf https://gq.pgi.gov.pl/pg/article/view/14135 pol pol Państwowy Instytut Geologiczny - PIB https://gq.pgi.gov.pl/pg/article/view/14135/12440 Przegląd Geologiczny; Vol 51, No 7 (2003); 580–585 0033-2151 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion artykuł naukowy 2003 ftjgq 2019-08-13T17:58:52Z NEW FINDS OF ERRATICS OF THE OSLO RHOMB PORPHYRY IN NORTH-WESTERN POLAND Summary Two specimens of Oslo rhomb porphyries find on the Wolin Island beach between Międzyzdroje and Grodno are extraordinary finds among the entire population of Scandinavian indicator erratics within glacial sediments in northern Poland. Only around 20 localities of erratics from Oslo have been noted in that part of Poland so far (Schulz, 1973). Unfortunately, the stratigraphy of the Wolin erratics is not known, because they have been found on the stony abrasion shelf at the foot of a cliff. The cliff itself consists of two separate till layers. The petrographical analysis of the lower bed of gray glacial till where rhomb porphyries had been found, point to distinctly north-western direction of an ice sheet advance (50 % of the entire population of erratics from sample 3 derive from western mother regions in the southern Baltic bottom). The analysed indicator erratics form the lower Wolin till represent the south-eastern Sweden and western part of the bottom of Baltic depression. The ice-sheet, approaching from the north, has transgressed on these outcrops before reaching the mother regions of Cretaceous limestones, which are located in the direct vicinity of the Wolin Island. The ample content of western erratics in sampled sediments of the Wolin cliff as well as the Oslo rhomb porphyries are of high interest. Have they come in icebergs (Benn & Evans, 1998, see Donner, 1995) or maybe their presence in glacial sediments should be connected with the Lagerlund’s ice dome (1987, 1995)? Schulz (2003) suggests a ship transport (as ballast stones). The planned detailed petrographical analysis on the Scandinavian erratics of the Wolin cliff should clarify the issue. Article in Journal/Newspaper Ice Sheet Geological Quarterly
institution Open Polar
collection Geological Quarterly
op_collection_id ftjgq
language Polish
description NEW FINDS OF ERRATICS OF THE OSLO RHOMB PORPHYRY IN NORTH-WESTERN POLAND Summary Two specimens of Oslo rhomb porphyries find on the Wolin Island beach between Międzyzdroje and Grodno are extraordinary finds among the entire population of Scandinavian indicator erratics within glacial sediments in northern Poland. Only around 20 localities of erratics from Oslo have been noted in that part of Poland so far (Schulz, 1973). Unfortunately, the stratigraphy of the Wolin erratics is not known, because they have been found on the stony abrasion shelf at the foot of a cliff. The cliff itself consists of two separate till layers. The petrographical analysis of the lower bed of gray glacial till where rhomb porphyries had been found, point to distinctly north-western direction of an ice sheet advance (50 % of the entire population of erratics from sample 3 derive from western mother regions in the southern Baltic bottom). The analysed indicator erratics form the lower Wolin till represent the south-eastern Sweden and western part of the bottom of Baltic depression. The ice-sheet, approaching from the north, has transgressed on these outcrops before reaching the mother regions of Cretaceous limestones, which are located in the direct vicinity of the Wolin Island. The ample content of western erratics in sampled sediments of the Wolin cliff as well as the Oslo rhomb porphyries are of high interest. Have they come in icebergs (Benn & Evans, 1998, see Donner, 1995) or maybe their presence in glacial sediments should be connected with the Lagerlund’s ice dome (1987, 1995)? Schulz (2003) suggests a ship transport (as ballast stones). The planned detailed petrographical analysis on the Scandinavian erratics of the Wolin cliff should clarify the issue.
format Article in Journal/Newspaper
author Górska, Maria
spellingShingle Górska, Maria
Nowe znaleziska narzutniaków porfiru rombowego z Oslo na terenie północno-zachodniej Polski
author_facet Górska, Maria
author_sort Górska, Maria
title Nowe znaleziska narzutniaków porfiru rombowego z Oslo na terenie północno-zachodniej Polski
title_short Nowe znaleziska narzutniaków porfiru rombowego z Oslo na terenie północno-zachodniej Polski
title_full Nowe znaleziska narzutniaków porfiru rombowego z Oslo na terenie północno-zachodniej Polski
title_fullStr Nowe znaleziska narzutniaków porfiru rombowego z Oslo na terenie północno-zachodniej Polski
title_full_unstemmed Nowe znaleziska narzutniaków porfiru rombowego z Oslo na terenie północno-zachodniej Polski
title_sort nowe znaleziska narzutniaków porfiru rombowego z oslo na terenie północno-zachodniej polski
publisher Państwowy Instytut Geologiczny - PIB
publishDate 2003
url https://gq.pgi.gov.pl/pg/article/view/14135
genre Ice Sheet
genre_facet Ice Sheet
op_source Przegląd Geologiczny; Vol 51, No 7 (2003); 580–585
0033-2151
op_relation https://gq.pgi.gov.pl/pg/article/view/14135/12440
_version_ 1766031107620339712