Forecasting the path of a laterally propagating dike

An important aspect of eruption forecasting is predicting the path of propagating dikes. We show how lateral dike propagation can be forecast using the minimum potential energy principle. We compare theory to observed propagation paths of dikes originating at the Bárðarbunga volcano, Iceland, in 201...

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Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Heimisson, ER, Hooper, A, Sigmundsson, F
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2015
Subjects:
Online Access:https://eprints.whiterose.ac.uk/96992/
https://eprints.whiterose.ac.uk/96992/14/Heimisson_et_al-2015-Journal_of_Geophysical_Research-_Solid_Earth.pdf
https://doi.org/10.1002/2015JB012402
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spelling ftleedsuniv:oai:eprints.whiterose.ac.uk:96992 2023-05-15T16:50:43+02:00 Forecasting the path of a laterally propagating dike Heimisson, ER Hooper, A Sigmundsson, F 2015-12-28 text https://eprints.whiterose.ac.uk/96992/ https://eprints.whiterose.ac.uk/96992/14/Heimisson_et_al-2015-Journal_of_Geophysical_Research-_Solid_Earth.pdf https://doi.org/10.1002/2015JB012402 en eng American Geophysical Union https://eprints.whiterose.ac.uk/96992/14/Heimisson_et_al-2015-Journal_of_Geophysical_Research-_Solid_Earth.pdf Heimisson, ER, Hooper, A and Sigmundsson, F (2015) Forecasting the path of a laterally propagating dike. Journal of Geophysical Research: Solid Earth, 120 (12). pp. 8774-8792. ISSN 2169-9356 Article NonPeerReviewed 2015 ftleedsuniv https://doi.org/10.1002/2015JB012402 2023-01-30T21:40:25Z An important aspect of eruption forecasting is predicting the path of propagating dikes. We show how lateral dike propagation can be forecast using the minimum potential energy principle. We compare theory to observed propagation paths of dikes originating at the Bárðarbunga volcano, Iceland, in 2014 and 1996, by developing a probability distribution for the most likely propagation path. The observed propagation paths agree well with the model prediction. We find that topography is very important for the model, and our preferred forecasting model considers its influence on the potential energy change of the crust and magma. We tested the influence of topography by running the model assuming no topography and found that the path of the 2014 dike could not be hindcasted. The results suggest that lateral dike propagation is governed not only by deviatoric stresses but also by pressure gradients and gravitational potential energy. Furthermore, the model predicts the formation of curved dikes around cone-shaped structures without the assumption of a local deviatoric stress field. We suggest that a likely eruption site for a laterally propagating dike is in topographic lows. The method presented here is simple and computationally feasible. Our results indicate that this kind of a model can be applied to mitigate volcanic hazards in regions where the tectonic setting promotes formation of laterally propagating vertical intrusive sheets. Article in Journal/Newspaper Iceland White Rose Research Online (Universities of Leeds, Sheffield & York) Journal of Geophysical Research: Solid Earth 120 12 8774 8792
institution Open Polar
collection White Rose Research Online (Universities of Leeds, Sheffield & York)
op_collection_id ftleedsuniv
language English
description An important aspect of eruption forecasting is predicting the path of propagating dikes. We show how lateral dike propagation can be forecast using the minimum potential energy principle. We compare theory to observed propagation paths of dikes originating at the Bárðarbunga volcano, Iceland, in 2014 and 1996, by developing a probability distribution for the most likely propagation path. The observed propagation paths agree well with the model prediction. We find that topography is very important for the model, and our preferred forecasting model considers its influence on the potential energy change of the crust and magma. We tested the influence of topography by running the model assuming no topography and found that the path of the 2014 dike could not be hindcasted. The results suggest that lateral dike propagation is governed not only by deviatoric stresses but also by pressure gradients and gravitational potential energy. Furthermore, the model predicts the formation of curved dikes around cone-shaped structures without the assumption of a local deviatoric stress field. We suggest that a likely eruption site for a laterally propagating dike is in topographic lows. The method presented here is simple and computationally feasible. Our results indicate that this kind of a model can be applied to mitigate volcanic hazards in regions where the tectonic setting promotes formation of laterally propagating vertical intrusive sheets.
format Article in Journal/Newspaper
author Heimisson, ER
Hooper, A
Sigmundsson, F
spellingShingle Heimisson, ER
Hooper, A
Sigmundsson, F
Forecasting the path of a laterally propagating dike
author_facet Heimisson, ER
Hooper, A
Sigmundsson, F
author_sort Heimisson, ER
title Forecasting the path of a laterally propagating dike
title_short Forecasting the path of a laterally propagating dike
title_full Forecasting the path of a laterally propagating dike
title_fullStr Forecasting the path of a laterally propagating dike
title_full_unstemmed Forecasting the path of a laterally propagating dike
title_sort forecasting the path of a laterally propagating dike
publisher American Geophysical Union
publishDate 2015
url https://eprints.whiterose.ac.uk/96992/
https://eprints.whiterose.ac.uk/96992/14/Heimisson_et_al-2015-Journal_of_Geophysical_Research-_Solid_Earth.pdf
https://doi.org/10.1002/2015JB012402
genre Iceland
genre_facet Iceland
op_relation https://eprints.whiterose.ac.uk/96992/14/Heimisson_et_al-2015-Journal_of_Geophysical_Research-_Solid_Earth.pdf
Heimisson, ER, Hooper, A and Sigmundsson, F (2015) Forecasting the path of a laterally propagating dike. Journal of Geophysical Research: Solid Earth, 120 (12). pp. 8774-8792. ISSN 2169-9356
op_doi https://doi.org/10.1002/2015JB012402
container_title Journal of Geophysical Research: Solid Earth
container_volume 120
container_issue 12
container_start_page 8774
op_container_end_page 8792
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