Vesiculated tuffs and associated features
ABSTRACT Vesiculated tuffs are tuffs that contain vesicles between the ash particles. Formation of the vesicles is the result of trapping of steam, the transporting agent of volcanic base surges, in wet, muddy or sticky ash deposited by the base surges. Vesiculated tuffs are described from various m...
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crwiley:10.1111/j.1365-3091.1974.tb02059.x 2024-09-15T18:13:41+00:00 Vesiculated tuffs and associated features LORENZ, V. 1974 http://dx.doi.org/10.1111/j.1365-3091.1974.tb02059.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-3091.1974.tb02059.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-3091.1974.tb02059.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Sedimentology volume 21, issue 2, page 273-291 ISSN 0037-0746 1365-3091 journal-article 1974 crwiley https://doi.org/10.1111/j.1365-3091.1974.tb02059.x 2024-08-09T04:30:58Z ABSTRACT Vesiculated tuffs are tuffs that contain vesicles between the ash particles. Formation of the vesicles is the result of trapping of steam, the transporting agent of volcanic base surges, in wet, muddy or sticky ash deposited by the base surges. Vesiculated tuffs are described from various maars and tuff‐rings in Europe (Iceland, France, Germany) and USA together with associated surface features such as: gravity flowage ripples, mud flow channels, current ripples, and current ridges. Other features described are: plastering of ash against obstacles and vesiculated accretionary lapilli, the latter containing vesicles in the outer layer. Vesiculated base surge deposits probably contained as much as 20–30% of interstitial water and fell out of the base surge clouds en masse owing to non‐free flow and consequent accretion. Article in Journal/Newspaper Iceland Wiley Online Library Sedimentology 21 2 273 291 |
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Wiley Online Library |
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English |
description |
ABSTRACT Vesiculated tuffs are tuffs that contain vesicles between the ash particles. Formation of the vesicles is the result of trapping of steam, the transporting agent of volcanic base surges, in wet, muddy or sticky ash deposited by the base surges. Vesiculated tuffs are described from various maars and tuff‐rings in Europe (Iceland, France, Germany) and USA together with associated surface features such as: gravity flowage ripples, mud flow channels, current ripples, and current ridges. Other features described are: plastering of ash against obstacles and vesiculated accretionary lapilli, the latter containing vesicles in the outer layer. Vesiculated base surge deposits probably contained as much as 20–30% of interstitial water and fell out of the base surge clouds en masse owing to non‐free flow and consequent accretion. |
format |
Article in Journal/Newspaper |
author |
LORENZ, V. |
spellingShingle |
LORENZ, V. Vesiculated tuffs and associated features |
author_facet |
LORENZ, V. |
author_sort |
LORENZ, V. |
title |
Vesiculated tuffs and associated features |
title_short |
Vesiculated tuffs and associated features |
title_full |
Vesiculated tuffs and associated features |
title_fullStr |
Vesiculated tuffs and associated features |
title_full_unstemmed |
Vesiculated tuffs and associated features |
title_sort |
vesiculated tuffs and associated features |
publisher |
Wiley |
publishDate |
1974 |
url |
http://dx.doi.org/10.1111/j.1365-3091.1974.tb02059.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-3091.1974.tb02059.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-3091.1974.tb02059.x |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Sedimentology volume 21, issue 2, page 273-291 ISSN 0037-0746 1365-3091 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1365-3091.1974.tb02059.x |
container_title |
Sedimentology |
container_volume |
21 |
container_issue |
2 |
container_start_page |
273 |
op_container_end_page |
291 |
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1810451447163125760 |