Seven Million Years of Glaciation in Greenland

Glacial till, glaciomarine diamictites, and ice-rafted detritus found in marine cores collected off the shore of southeast Greenland record multiple Late Cenozoic glaciations beginning in the Late Miocene. Distinct rock assemblages and seismic stratigraphic control correlate the diamictites with gla...

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Published in:Science
Main Authors: Larsen, H. C., Saunders, A. D., Clift, P. D., Beget, J., Wei, W., Spezzaferri, S.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1994
Subjects:
Online Access:http://dx.doi.org/10.1126/science.264.5161.952
https://www.science.org/doi/pdf/10.1126/science.264.5161.952
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spelling craaas:10.1126/science.264.5161.952 2024-06-23T07:53:07+00:00 Seven Million Years of Glaciation in Greenland Larsen, H. C. Saunders, A. D. Clift, P. D. Beget, J. Wei, W. Spezzaferri, S. 1994 http://dx.doi.org/10.1126/science.264.5161.952 https://www.science.org/doi/pdf/10.1126/science.264.5161.952 en eng American Association for the Advancement of Science (AAAS) Science volume 264, issue 5161, page 952-955 ISSN 0036-8075 1095-9203 journal-article 1994 craaas https://doi.org/10.1126/science.264.5161.952 2024-05-24T12:53:43Z Glacial till, glaciomarine diamictites, and ice-rafted detritus found in marine cores collected off the shore of southeast Greenland record multiple Late Cenozoic glaciations beginning in the Late Miocene. Distinct rock assemblages and seismic stratigraphic control correlate the diamictites with glaciation of the southeast Greenland margin. Glaciers advanced to the sea during several intervals in the Pliocene and Pleistocene. North Atlantic glaciation may have nucleated in southern Greenland rather than further north because of the high mountains and the high levels of precipitation in this region. Article in Journal/Newspaper Greenland North Atlantic AAAS Resource Center (American Association for the Advancement of Science) Greenland Science 264 5161 952 955
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Glacial till, glaciomarine diamictites, and ice-rafted detritus found in marine cores collected off the shore of southeast Greenland record multiple Late Cenozoic glaciations beginning in the Late Miocene. Distinct rock assemblages and seismic stratigraphic control correlate the diamictites with glaciation of the southeast Greenland margin. Glaciers advanced to the sea during several intervals in the Pliocene and Pleistocene. North Atlantic glaciation may have nucleated in southern Greenland rather than further north because of the high mountains and the high levels of precipitation in this region.
format Article in Journal/Newspaper
author Larsen, H. C.
Saunders, A. D.
Clift, P. D.
Beget, J.
Wei, W.
Spezzaferri, S.
spellingShingle Larsen, H. C.
Saunders, A. D.
Clift, P. D.
Beget, J.
Wei, W.
Spezzaferri, S.
Seven Million Years of Glaciation in Greenland
author_facet Larsen, H. C.
Saunders, A. D.
Clift, P. D.
Beget, J.
Wei, W.
Spezzaferri, S.
author_sort Larsen, H. C.
title Seven Million Years of Glaciation in Greenland
title_short Seven Million Years of Glaciation in Greenland
title_full Seven Million Years of Glaciation in Greenland
title_fullStr Seven Million Years of Glaciation in Greenland
title_full_unstemmed Seven Million Years of Glaciation in Greenland
title_sort seven million years of glaciation in greenland
publisher American Association for the Advancement of Science (AAAS)
publishDate 1994
url http://dx.doi.org/10.1126/science.264.5161.952
https://www.science.org/doi/pdf/10.1126/science.264.5161.952
geographic Greenland
geographic_facet Greenland
genre Greenland
North Atlantic
genre_facet Greenland
North Atlantic
op_source Science
volume 264, issue 5161, page 952-955
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.264.5161.952
container_title Science
container_volume 264
container_issue 5161
container_start_page 952
op_container_end_page 955
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