Precambrian Glaciated Surface Beneath the Gowganda Formation, Lake Timagami, Ontario

Glacial deposition of the Gowganda formation is established by the discovery of an extensive, well-marked, glaciated, basal contact surface. This surface is exposed near the southeastern end of Lake Timagami, northern Ontario. The Precambrian ice sheet advanced three times from the northeast over th...

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Bibliographic Details
Published in:Science
Main Author: Schenk, Paul E.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1965
Subjects:
Ice Sheet
Online Access:http://dx.doi.org/10.1126/science.149.3680.176
https://www.science.org/doi/pdf/10.1126/science.149.3680.176
id craaas:10.1126/science.149.3680.176
record_format openpolar
spelling craaas:10.1126/science.149.3680.176 2024-06-09T07:46:47+00:00 Precambrian Glaciated Surface Beneath the Gowganda Formation, Lake Timagami, Ontario Schenk, Paul E. 1965 http://dx.doi.org/10.1126/science.149.3680.176 https://www.science.org/doi/pdf/10.1126/science.149.3680.176 en eng American Association for the Advancement of Science (AAAS) Science volume 149, issue 3680, page 176-177 ISSN 0036-8075 1095-9203 journal-article 1965 craaas https://doi.org/10.1126/science.149.3680.176 2024-05-16T12:55:23Z Glacial deposition of the Gowganda formation is established by the discovery of an extensive, well-marked, glaciated, basal contact surface. This surface is exposed near the southeastern end of Lake Timagami, northern Ontario. The Precambrian ice sheet advanced three times from the northeast over the area. Article in Journal/Newspaper Ice Sheet AAAS Resource Center (American Association for the Advancement of Science) Science 149 3680 176 177
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Glacial deposition of the Gowganda formation is established by the discovery of an extensive, well-marked, glaciated, basal contact surface. This surface is exposed near the southeastern end of Lake Timagami, northern Ontario. The Precambrian ice sheet advanced three times from the northeast over the area.
format Article in Journal/Newspaper
author Schenk, Paul E.
spellingShingle Schenk, Paul E.
Precambrian Glaciated Surface Beneath the Gowganda Formation, Lake Timagami, Ontario
author_facet Schenk, Paul E.
author_sort Schenk, Paul E.
title Precambrian Glaciated Surface Beneath the Gowganda Formation, Lake Timagami, Ontario
title_short Precambrian Glaciated Surface Beneath the Gowganda Formation, Lake Timagami, Ontario
title_full Precambrian Glaciated Surface Beneath the Gowganda Formation, Lake Timagami, Ontario
title_fullStr Precambrian Glaciated Surface Beneath the Gowganda Formation, Lake Timagami, Ontario
title_full_unstemmed Precambrian Glaciated Surface Beneath the Gowganda Formation, Lake Timagami, Ontario
title_sort precambrian glaciated surface beneath the gowganda formation, lake timagami, ontario
publisher American Association for the Advancement of Science (AAAS)
publishDate 1965
url http://dx.doi.org/10.1126/science.149.3680.176
https://www.science.org/doi/pdf/10.1126/science.149.3680.176
genre Ice Sheet
genre_facet Ice Sheet
op_source Science
volume 149, issue 3680, page 176-177
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.149.3680.176
container_title Science
container_volume 149
container_issue 3680
container_start_page 176
op_container_end_page 177
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