Submerged drainage patterns in Barrow Strait, Canadian Arctic

Recent detailed bathymetric maps of Barrow Strait enabled a reconsideration of the Tertiary fluvial erosion model used to account for the physiography of the Canadian Arctic Archipelago. Five distinct drainage basins were distinguished within Barrow Strait, including both dendritic and rectangular d...

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Published in:Canadian Journal of Earth Sciences
Main Authors: Bornhold, Brian D., Finlayson, Nancy M., Monahan, David
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1976
Subjects:
Online Access:http://dx.doi.org/10.1139/e76-032
http://www.nrcresearchpress.com/doi/pdf/10.1139/e76-032
id crcansciencepubl:10.1139/e76-032
record_format openpolar
spelling crcansciencepubl:10.1139/e76-032 2023-12-17T10:23:37+01:00 Submerged drainage patterns in Barrow Strait, Canadian Arctic Bornhold, Brian D. Finlayson, Nancy M. Monahan, David 1976 http://dx.doi.org/10.1139/e76-032 http://www.nrcresearchpress.com/doi/pdf/10.1139/e76-032 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 13, issue 2, page 305-311 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1976 crcansciencepubl https://doi.org/10.1139/e76-032 2023-11-19T13:38:55Z Recent detailed bathymetric maps of Barrow Strait enabled a reconsideration of the Tertiary fluvial erosion model used to account for the physiography of the Canadian Arctic Archipelago. Five distinct drainage basins were distinguished within Barrow Strait, including both dendritic and rectangular drainage patterns. The latter were controlled by normal faults along the Precambrian–Paleozoic contact in Peel Sound and Barrow Strait.Several changes in the original model are proposed, including the placement of the main east–west drainage divide through Somerset Island and across Barrow Strait and southern Wellington Channel to Devon Island. Article in Journal/Newspaper Arctic Archipelago Arctic Canadian Arctic Archipelago Devon Island Somerset Island Canadian Science Publishing (via Crossref) Arctic Canadian Arctic Archipelago Devon Island ENVELOPE(-88.000,-88.000,75.252,75.252) Somerset Island ENVELOPE(-93.500,-93.500,73.251,73.251) Barrow Strait ENVELOPE(-94.168,-94.168,74.402,74.402) Peel Sound ENVELOPE(-96.334,-96.334,73.001,73.001) Wellington Channel ENVELOPE(-93.201,-93.201,75.468,75.468) Canadian Journal of Earth Sciences 13 2 305 311
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic General Earth and Planetary Sciences
spellingShingle General Earth and Planetary Sciences
Bornhold, Brian D.
Finlayson, Nancy M.
Monahan, David
Submerged drainage patterns in Barrow Strait, Canadian Arctic
topic_facet General Earth and Planetary Sciences
description Recent detailed bathymetric maps of Barrow Strait enabled a reconsideration of the Tertiary fluvial erosion model used to account for the physiography of the Canadian Arctic Archipelago. Five distinct drainage basins were distinguished within Barrow Strait, including both dendritic and rectangular drainage patterns. The latter were controlled by normal faults along the Precambrian–Paleozoic contact in Peel Sound and Barrow Strait.Several changes in the original model are proposed, including the placement of the main east–west drainage divide through Somerset Island and across Barrow Strait and southern Wellington Channel to Devon Island.
format Article in Journal/Newspaper
author Bornhold, Brian D.
Finlayson, Nancy M.
Monahan, David
author_facet Bornhold, Brian D.
Finlayson, Nancy M.
Monahan, David
author_sort Bornhold, Brian D.
title Submerged drainage patterns in Barrow Strait, Canadian Arctic
title_short Submerged drainage patterns in Barrow Strait, Canadian Arctic
title_full Submerged drainage patterns in Barrow Strait, Canadian Arctic
title_fullStr Submerged drainage patterns in Barrow Strait, Canadian Arctic
title_full_unstemmed Submerged drainage patterns in Barrow Strait, Canadian Arctic
title_sort submerged drainage patterns in barrow strait, canadian arctic
publisher Canadian Science Publishing
publishDate 1976
url http://dx.doi.org/10.1139/e76-032
http://www.nrcresearchpress.com/doi/pdf/10.1139/e76-032
long_lat ENVELOPE(-88.000,-88.000,75.252,75.252)
ENVELOPE(-93.500,-93.500,73.251,73.251)
ENVELOPE(-94.168,-94.168,74.402,74.402)
ENVELOPE(-96.334,-96.334,73.001,73.001)
ENVELOPE(-93.201,-93.201,75.468,75.468)
geographic Arctic
Canadian Arctic Archipelago
Devon Island
Somerset Island
Barrow Strait
Peel Sound
Wellington Channel
geographic_facet Arctic
Canadian Arctic Archipelago
Devon Island
Somerset Island
Barrow Strait
Peel Sound
Wellington Channel
genre Arctic Archipelago
Arctic
Canadian Arctic Archipelago
Devon Island
Somerset Island
genre_facet Arctic Archipelago
Arctic
Canadian Arctic Archipelago
Devon Island
Somerset Island
op_source Canadian Journal of Earth Sciences
volume 13, issue 2, page 305-311
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e76-032
container_title Canadian Journal of Earth Sciences
container_volume 13
container_issue 2
container_start_page 305
op_container_end_page 311
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