Using scoria cones, lava lakes and tephra islands to understand the evolution of basaltic fissure eruptions
Basaltic fissure eruptions are the most common eruption type on Earth. They are characterised by linear lava fountains that construct pyroclastic cones and expansive lava flow fields. The histories of these eruptions can be notoriously difficult to interpret due to the geochemical homogeneity of the...
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crwiley:10.1111/gto.12223 2024-06-02T08:09:15+00:00 Using scoria cones, lava lakes and tephra islands to understand the evolution of basaltic fissure eruptions Reynolds, P. Brown, R.J. 2018 http://dx.doi.org/10.1111/gto.12223 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fgto.12223 https://onlinelibrary.wiley.com/doi/pdf/10.1111/gto.12223 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Geology Today volume 34, issue 2, page 66-72 ISSN 0266-6979 1365-2451 journal-article 2018 crwiley https://doi.org/10.1111/gto.12223 2024-05-03T11:44:46Z Basaltic fissure eruptions are the most common eruption type on Earth. They are characterised by linear lava fountains that construct pyroclastic cones and expansive lava flow fields. The histories of these eruptions can be notoriously difficult to interpret due to the geochemical homogeneity of the tephra, and due to the fact that many of the early deposits become buried during later stages of the eruption. Furthermore, observing the construction of the pyroclastic cones is inherently difficult and dangerous due to the presence of active lava fountains. However, glacial outbursts in the north of Iceland have dissected the products of a Holocene fissure eruption. Examination of the pyroclastic cones, tephra deposits and a solidified lava lake along the fissure has allowed us to elucidate the complex eruptive processes that occur during these eruptions. Article in Journal/Newspaper Iceland Wiley Online Library Lava Lake ENVELOPE(-128.996,-128.996,55.046,55.046) Lava Lakes ENVELOPE(-130.904,-130.904,56.433,56.433) Geology Today 34 2 66 72 |
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Open Polar |
collection |
Wiley Online Library |
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crwiley |
language |
English |
description |
Basaltic fissure eruptions are the most common eruption type on Earth. They are characterised by linear lava fountains that construct pyroclastic cones and expansive lava flow fields. The histories of these eruptions can be notoriously difficult to interpret due to the geochemical homogeneity of the tephra, and due to the fact that many of the early deposits become buried during later stages of the eruption. Furthermore, observing the construction of the pyroclastic cones is inherently difficult and dangerous due to the presence of active lava fountains. However, glacial outbursts in the north of Iceland have dissected the products of a Holocene fissure eruption. Examination of the pyroclastic cones, tephra deposits and a solidified lava lake along the fissure has allowed us to elucidate the complex eruptive processes that occur during these eruptions. |
format |
Article in Journal/Newspaper |
author |
Reynolds, P. Brown, R.J. |
spellingShingle |
Reynolds, P. Brown, R.J. Using scoria cones, lava lakes and tephra islands to understand the evolution of basaltic fissure eruptions |
author_facet |
Reynolds, P. Brown, R.J. |
author_sort |
Reynolds, P. |
title |
Using scoria cones, lava lakes and tephra islands to understand the evolution of basaltic fissure eruptions |
title_short |
Using scoria cones, lava lakes and tephra islands to understand the evolution of basaltic fissure eruptions |
title_full |
Using scoria cones, lava lakes and tephra islands to understand the evolution of basaltic fissure eruptions |
title_fullStr |
Using scoria cones, lava lakes and tephra islands to understand the evolution of basaltic fissure eruptions |
title_full_unstemmed |
Using scoria cones, lava lakes and tephra islands to understand the evolution of basaltic fissure eruptions |
title_sort |
using scoria cones, lava lakes and tephra islands to understand the evolution of basaltic fissure eruptions |
publisher |
Wiley |
publishDate |
2018 |
url |
http://dx.doi.org/10.1111/gto.12223 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fgto.12223 https://onlinelibrary.wiley.com/doi/pdf/10.1111/gto.12223 |
long_lat |
ENVELOPE(-128.996,-128.996,55.046,55.046) ENVELOPE(-130.904,-130.904,56.433,56.433) |
geographic |
Lava Lake Lava Lakes |
geographic_facet |
Lava Lake Lava Lakes |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Geology Today volume 34, issue 2, page 66-72 ISSN 0266-6979 1365-2451 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/gto.12223 |
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Geology Today |
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34 |
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2 |
container_start_page |
66 |
op_container_end_page |
72 |
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1800754939522187264 |