Dispersal Patterns of Pleistocene Sands on the North Atlantic Deep-Sea Floor

Glauconitic, quartzose sands previously modified on the continental shelf from feldspathic glacial detritus were transported through submarine canyons onto the Hudson deep-sea fan, the Hatteras abyssal plain, and the western and central Sohm abyssal plain. These feldspar-poor, quartzose sands contra...

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Bibliographic Details
Published in:Science
Main Author: Hubert, John F.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1962
Subjects:
Hudson
Sohm
Newfoundland
North Atlantic
Online Access:http://dx.doi.org/10.1126/science.136.3514.383
https://www.science.org/doi/pdf/10.1126/science.136.3514.383
id craaas:10.1126/science.136.3514.383
record_format openpolar
spelling craaas:10.1126/science.136.3514.383 2024-06-09T07:47:50+00:00 Dispersal Patterns of Pleistocene Sands on the North Atlantic Deep-Sea Floor Hubert, John F. 1962 http://dx.doi.org/10.1126/science.136.3514.383 https://www.science.org/doi/pdf/10.1126/science.136.3514.383 en eng American Association for the Advancement of Science (AAAS) Science volume 136, issue 3514, page 383-384 ISSN 0036-8075 1095-9203 journal-article 1962 craaas https://doi.org/10.1126/science.136.3514.383 2024-05-16T12:54:27Z Glauconitic, quartzose sands previously modified on the continental shelf from feldspathic glacial detritus were transported through submarine canyons onto the Hudson deep-sea fan, the Hatteras abyssal plain, and the western and central Sohm abyssal plain. These feldspar-poor, quartzose sands contrast with highly feldspathic sands derived directly from a glacial source and probably transported through the Newfoundland abyssal gap onto the eastern and southern Sohm abyssal plain. Article in Journal/Newspaper Newfoundland North Atlantic AAAS Resource Center (American Association for the Advancement of Science) Hudson Sohm ENVELOPE(-64.800,-64.800,-66.067,-66.067) Science 136 3514 383 384
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Glauconitic, quartzose sands previously modified on the continental shelf from feldspathic glacial detritus were transported through submarine canyons onto the Hudson deep-sea fan, the Hatteras abyssal plain, and the western and central Sohm abyssal plain. These feldspar-poor, quartzose sands contrast with highly feldspathic sands derived directly from a glacial source and probably transported through the Newfoundland abyssal gap onto the eastern and southern Sohm abyssal plain.
format Article in Journal/Newspaper
author Hubert, John F.
spellingShingle Hubert, John F.
Dispersal Patterns of Pleistocene Sands on the North Atlantic Deep-Sea Floor
author_facet Hubert, John F.
author_sort Hubert, John F.
title Dispersal Patterns of Pleistocene Sands on the North Atlantic Deep-Sea Floor
title_short Dispersal Patterns of Pleistocene Sands on the North Atlantic Deep-Sea Floor
title_full Dispersal Patterns of Pleistocene Sands on the North Atlantic Deep-Sea Floor
title_fullStr Dispersal Patterns of Pleistocene Sands on the North Atlantic Deep-Sea Floor
title_full_unstemmed Dispersal Patterns of Pleistocene Sands on the North Atlantic Deep-Sea Floor
title_sort dispersal patterns of pleistocene sands on the north atlantic deep-sea floor
publisher American Association for the Advancement of Science (AAAS)
publishDate 1962
url http://dx.doi.org/10.1126/science.136.3514.383
https://www.science.org/doi/pdf/10.1126/science.136.3514.383
long_lat ENVELOPE(-64.800,-64.800,-66.067,-66.067)
geographic Hudson
Sohm
geographic_facet Hudson
Sohm
genre Newfoundland
North Atlantic
genre_facet Newfoundland
North Atlantic
op_source Science
volume 136, issue 3514, page 383-384
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.136.3514.383
container_title Science
container_volume 136
container_issue 3514
container_start_page 383
op_container_end_page 384
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