IV.—The Physical History of the Norwegian Fjords
The Scandinavian Promontory . — This remarkable promontory, extending for over a thousand miles from the Naze to the North Cape, is formed mainly of Archæan rocks, consisting of gneiss, crystalline schists, and other metamorphic rocks, penetrated by granite and other igneous dykes of later date. The...
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Cambridge University Press (CUP)
1913
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Online Access: | http://dx.doi.org/10.1017/s0016756800125488 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800125488 |
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crcambridgeupr:10.1017/s0016756800125488 2024-03-03T08:47:10+00:00 IV.—The Physical History of the Norwegian Fjords Hull, Edward 1913 http://dx.doi.org/10.1017/s0016756800125488 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800125488 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 10, issue 1, page 9-14 ISSN 0016-7568 1469-5081 Geology journal-article 1913 crcambridgeupr https://doi.org/10.1017/s0016756800125488 2024-02-08T08:36:15Z The Scandinavian Promontory . — This remarkable promontory, extending for over a thousand miles from the Naze to the North Cape, is formed mainly of Archæan rocks, consisting of gneiss, crystalline schists, and other metamorphic rocks, penetrated by granite and other igneous dykes of later date. These primeval rocks are overlain throughout a portion of their extent by Cambrian and Lower Palæozoic (or Lower Silurian) beds, between which and the Archaean masses there is entire discordancy, and, as regards their respective ages, a long period of unrepresented time. The Palæozoic beds are themselves highly altered when in contact with the intrusive igneous masses, so that it is difficult to distinguish them from the more ancient masses in some districts. Article in Journal/Newspaper North Cape Cambridge University Press North Cape ENVELOPE(165.700,165.700,-70.650,-70.650) Naze ENVELOPE(-57.517,-57.517,-63.917,-63.917) The Naze ENVELOPE(-57.533,-57.533,-63.950,-63.950) Geological Magazine 10 1 9 14 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology |
spellingShingle |
Geology Hull, Edward IV.—The Physical History of the Norwegian Fjords |
topic_facet |
Geology |
description |
The Scandinavian Promontory . — This remarkable promontory, extending for over a thousand miles from the Naze to the North Cape, is formed mainly of Archæan rocks, consisting of gneiss, crystalline schists, and other metamorphic rocks, penetrated by granite and other igneous dykes of later date. These primeval rocks are overlain throughout a portion of their extent by Cambrian and Lower Palæozoic (or Lower Silurian) beds, between which and the Archaean masses there is entire discordancy, and, as regards their respective ages, a long period of unrepresented time. The Palæozoic beds are themselves highly altered when in contact with the intrusive igneous masses, so that it is difficult to distinguish them from the more ancient masses in some districts. |
format |
Article in Journal/Newspaper |
author |
Hull, Edward |
author_facet |
Hull, Edward |
author_sort |
Hull, Edward |
title |
IV.—The Physical History of the Norwegian Fjords |
title_short |
IV.—The Physical History of the Norwegian Fjords |
title_full |
IV.—The Physical History of the Norwegian Fjords |
title_fullStr |
IV.—The Physical History of the Norwegian Fjords |
title_full_unstemmed |
IV.—The Physical History of the Norwegian Fjords |
title_sort |
iv.—the physical history of the norwegian fjords |
publisher |
Cambridge University Press (CUP) |
publishDate |
1913 |
url |
http://dx.doi.org/10.1017/s0016756800125488 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800125488 |
long_lat |
ENVELOPE(165.700,165.700,-70.650,-70.650) ENVELOPE(-57.517,-57.517,-63.917,-63.917) ENVELOPE(-57.533,-57.533,-63.950,-63.950) |
geographic |
North Cape Naze The Naze |
geographic_facet |
North Cape Naze The Naze |
genre |
North Cape |
genre_facet |
North Cape |
op_source |
Geological Magazine volume 10, issue 1, page 9-14 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800125488 |
container_title |
Geological Magazine |
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10 |
container_issue |
1 |
container_start_page |
9 |
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14 |
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1792503320067178496 |