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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Published in:Geological Magazine
Main Author: Peacock, Martin A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1926
Subjects:
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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spelling 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
institution 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
container_volume 63
container_issue 9
container_start_page 385
op_container_end_page 399
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