The Vulcano-Glacial Palagonite Formation of Iceland
The geological feature which strikes the traveller in Iceland perhaps most forcibly is the complete contrast afforded by the well-ordered, level, or gently dipping basalt sheets with almost negligible tuff intercalations which constitute the Pre-glacial Kainozoic Plateau and the Late-glacial and Rec...
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Language: | English |
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Cambridge University Press (CUP)
1926
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Online Access: | http://dx.doi.org/10.1017/s0016756800085137 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800085137 |
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crcambridgeupr:10.1017/s0016756800085137 2024-09-15T18:13:18+00:00 The Vulcano-Glacial Palagonite Formation of Iceland Peacock, Martin A. 1926 http://dx.doi.org/10.1017/s0016756800085137 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800085137 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 63, issue 9, page 385-399 ISSN 0016-7568 1469-5081 journal-article 1926 crcambridgeupr https://doi.org/10.1017/s0016756800085137 2024-07-31T04:04:38Z The geological feature which strikes the traveller in Iceland perhaps most forcibly is the complete contrast afforded by the well-ordered, level, or gently dipping basalt sheets with almost negligible tuff intercalations which constitute the Pre-glacial Kainozoic Plateau and the Late-glacial and Recent volcanic formations, and the enormous, chaotic, rarely-bedded accumulations of the Palagonite Formation in which lava flows are subordinate in amount; and he is at once presented with the question: Why did igneous action which produced lava sheets in Pre-glacial times result in dominant tuffs and breccias in the period which followed, and then revert to the production of lavas in later times ? This question has not yet been fully answered. Article in Journal/Newspaper Iceland Cambridge University Press Geological Magazine 63 9 385 399 |
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Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
The geological feature which strikes the traveller in Iceland perhaps most forcibly is the complete contrast afforded by the well-ordered, level, or gently dipping basalt sheets with almost negligible tuff intercalations which constitute the Pre-glacial Kainozoic Plateau and the Late-glacial and Recent volcanic formations, and the enormous, chaotic, rarely-bedded accumulations of the Palagonite Formation in which lava flows are subordinate in amount; and he is at once presented with the question: Why did igneous action which produced lava sheets in Pre-glacial times result in dominant tuffs and breccias in the period which followed, and then revert to the production of lavas in later times ? This question has not yet been fully answered. |
format |
Article in Journal/Newspaper |
author |
Peacock, Martin A. |
spellingShingle |
Peacock, Martin A. The Vulcano-Glacial Palagonite Formation of Iceland |
author_facet |
Peacock, Martin A. |
author_sort |
Peacock, Martin A. |
title |
The Vulcano-Glacial Palagonite Formation of Iceland |
title_short |
The Vulcano-Glacial Palagonite Formation of Iceland |
title_full |
The Vulcano-Glacial Palagonite Formation of Iceland |
title_fullStr |
The Vulcano-Glacial Palagonite Formation of Iceland |
title_full_unstemmed |
The Vulcano-Glacial Palagonite Formation of Iceland |
title_sort |
vulcano-glacial palagonite formation of iceland |
publisher |
Cambridge University Press (CUP) |
publishDate |
1926 |
url |
http://dx.doi.org/10.1017/s0016756800085137 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800085137 |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Geological Magazine volume 63, issue 9, page 385-399 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800085137 |
container_title |
Geological Magazine |
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63 |
container_issue |
9 |
container_start_page |
385 |
op_container_end_page |
399 |
_version_ |
1810450985545367552 |