I.—On the Eastern Margin of the North Atlantic Basin

Quiting the more northern parts of the great Atlantic depression, we have next to consider an extensive water-space of a much shallower character. Here the volcanic masses of Iceland and the Fseroes with their submarine attachments have produced a marked effect on the depths of the ocean. The Norweg...

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Published in:Geological Magazine
Main Author: Hudleston, Wilfrid H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1899
Subjects:
Online Access:http://dx.doi.org/10.1017/s0016756800142979
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800142979
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spelling crcambridgeupr:10.1017/s0016756800142979 2024-03-03T08:45:42+00:00 I.—On the Eastern Margin of the North Atlantic Basin Hudleston, Wilfrid H. 1899 http://dx.doi.org/10.1017/s0016756800142979 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800142979 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 6, issue 4, page 146-157 ISSN 0016-7568 1469-5081 Geology journal-article 1899 crcambridgeupr https://doi.org/10.1017/s0016756800142979 2024-02-08T08:34:33Z Quiting the more northern parts of the great Atlantic depression, we have next to consider an extensive water-space of a much shallower character. Here the volcanic masses of Iceland and the Fseroes with their submarine attachments have produced a marked effect on the depths of the ocean. The Norwegian Atlantic connects with the main Atlantic by three straits, whose central channels present the following depths at their shallowest:— Article in Journal/Newspaper Iceland North Atlantic Cambridge University Press Geological Magazine 6 4 146 157
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
spellingShingle Geology
Hudleston, Wilfrid H.
I.—On the Eastern Margin of the North Atlantic Basin
topic_facet Geology
description Quiting the more northern parts of the great Atlantic depression, we have next to consider an extensive water-space of a much shallower character. Here the volcanic masses of Iceland and the Fseroes with their submarine attachments have produced a marked effect on the depths of the ocean. The Norwegian Atlantic connects with the main Atlantic by three straits, whose central channels present the following depths at their shallowest:—
format Article in Journal/Newspaper
author Hudleston, Wilfrid H.
author_facet Hudleston, Wilfrid H.
author_sort Hudleston, Wilfrid H.
title I.—On the Eastern Margin of the North Atlantic Basin
title_short I.—On the Eastern Margin of the North Atlantic Basin
title_full I.—On the Eastern Margin of the North Atlantic Basin
title_fullStr I.—On the Eastern Margin of the North Atlantic Basin
title_full_unstemmed I.—On the Eastern Margin of the North Atlantic Basin
title_sort i.—on the eastern margin of the north atlantic basin
publisher Cambridge University Press (CUP)
publishDate 1899
url http://dx.doi.org/10.1017/s0016756800142979
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800142979
genre Iceland
North Atlantic
genre_facet Iceland
North Atlantic
op_source Geological Magazine
volume 6, issue 4, page 146-157
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0016756800142979
container_title Geological Magazine
container_volume 6
container_issue 4
container_start_page 146
op_container_end_page 157
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