Lithostratigraphie et dynamique glaciaires au Wisconsinien, île d'Anticosti, golfe du Saint-Laurent

The Laurentide Ice Sheet deposited three tills on Anticosti Island. The oldest, the Rivière à la Patate Till, was formed by southeastward-flowing ice as determined from till fabrics. The till has an estimated age of 85 000 years BP based on the aminoacid racemization of shell fragments in overlying...

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Published in:Canadian Journal of Earth Sciences
Main Authors: St-Pierre, Luc, Gwyn, Q. H. J., Dubois, J. M. M.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1987
Subjects:
Online Access:http://dx.doi.org/10.1139/e87-175
http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-175
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record_format openpolar
spelling crcansciencepubl:10.1139/e87-175 2024-04-28T08:24:00+00:00 Lithostratigraphie et dynamique glaciaires au Wisconsinien, île d'Anticosti, golfe du Saint-Laurent St-Pierre, Luc Gwyn, Q. H. J. Dubois, J. M. M. 1987 http://dx.doi.org/10.1139/e87-175 http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-175 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 24, issue 9, page 1847-1858 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1987 crcansciencepubl https://doi.org/10.1139/e87-175 2024-04-09T06:56:26Z The Laurentide Ice Sheet deposited three tills on Anticosti Island. The oldest, the Rivière à la Patate Till, was formed by southeastward-flowing ice as determined from till fabrics. The till has an estimated age of 85 000 years BP based on the aminoacid racemization of shell fragments in overlying marine sediments. Thus it is probably Early Wisconsinan in age. The Middle Wisconsinan Rivière Jupiter Till and the Late Wisconsinan Île d'Anticosti Till are the result of the southwest-flowing Laurentide ice. The ice flowed without restriction though without accomplishing deep erosion of the bedrock, as indicated by glaciotectonic structures and till fabrics. However, striated blocks and pebbles in the tills reveal that basal shearing occurred. The ice limit in the Gulf of St. Lawrence from about 36 000 years BP onwards was located along the south coast of the island. This was the result of active calving at the margin of the relatively slow moving ice sheet. During retreat of the ice sheet, an ice cap became isolated on the island. It appears to have remained active in the western part of the island, where it formed the Sainte-Marie Moraine on the south, west, and north coasts, but was less active in the eastern part of the island, where a loose, sandy, but rare till (the Sainte-Marie Till) is the only proof of its activity. Deeper water in the eastern end of the Jacques-Cartier Strait, north of the island, accelerated ice calving and thus probably reduced the ice dynamic in the eastern part of the island. The names of tills used here are proposed as formal nomenclature. Article in Journal/Newspaper Ice cap Ice Sheet Canadian Science Publishing Canadian Journal of Earth Sciences 24 9 1847 1858
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
topic General Earth and Planetary Sciences
spellingShingle General Earth and Planetary Sciences
St-Pierre, Luc
Gwyn, Q. H. J.
Dubois, J. M. M.
Lithostratigraphie et dynamique glaciaires au Wisconsinien, île d'Anticosti, golfe du Saint-Laurent
topic_facet General Earth and Planetary Sciences
description The Laurentide Ice Sheet deposited three tills on Anticosti Island. The oldest, the Rivière à la Patate Till, was formed by southeastward-flowing ice as determined from till fabrics. The till has an estimated age of 85 000 years BP based on the aminoacid racemization of shell fragments in overlying marine sediments. Thus it is probably Early Wisconsinan in age. The Middle Wisconsinan Rivière Jupiter Till and the Late Wisconsinan Île d'Anticosti Till are the result of the southwest-flowing Laurentide ice. The ice flowed without restriction though without accomplishing deep erosion of the bedrock, as indicated by glaciotectonic structures and till fabrics. However, striated blocks and pebbles in the tills reveal that basal shearing occurred. The ice limit in the Gulf of St. Lawrence from about 36 000 years BP onwards was located along the south coast of the island. This was the result of active calving at the margin of the relatively slow moving ice sheet. During retreat of the ice sheet, an ice cap became isolated on the island. It appears to have remained active in the western part of the island, where it formed the Sainte-Marie Moraine on the south, west, and north coasts, but was less active in the eastern part of the island, where a loose, sandy, but rare till (the Sainte-Marie Till) is the only proof of its activity. Deeper water in the eastern end of the Jacques-Cartier Strait, north of the island, accelerated ice calving and thus probably reduced the ice dynamic in the eastern part of the island. The names of tills used here are proposed as formal nomenclature.
format Article in Journal/Newspaper
author St-Pierre, Luc
Gwyn, Q. H. J.
Dubois, J. M. M.
author_facet St-Pierre, Luc
Gwyn, Q. H. J.
Dubois, J. M. M.
author_sort St-Pierre, Luc
title Lithostratigraphie et dynamique glaciaires au Wisconsinien, île d'Anticosti, golfe du Saint-Laurent
title_short Lithostratigraphie et dynamique glaciaires au Wisconsinien, île d'Anticosti, golfe du Saint-Laurent
title_full Lithostratigraphie et dynamique glaciaires au Wisconsinien, île d'Anticosti, golfe du Saint-Laurent
title_fullStr Lithostratigraphie et dynamique glaciaires au Wisconsinien, île d'Anticosti, golfe du Saint-Laurent
title_full_unstemmed Lithostratigraphie et dynamique glaciaires au Wisconsinien, île d'Anticosti, golfe du Saint-Laurent
title_sort lithostratigraphie et dynamique glaciaires au wisconsinien, île d'anticosti, golfe du saint-laurent
publisher Canadian Science Publishing
publishDate 1987
url http://dx.doi.org/10.1139/e87-175
http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-175
genre Ice cap
Ice Sheet
genre_facet Ice cap
Ice Sheet
op_source Canadian Journal of Earth Sciences
volume 24, issue 9, page 1847-1858
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e87-175
container_title Canadian Journal of Earth Sciences
container_volume 24
container_issue 9
container_start_page 1847
op_container_end_page 1858
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