Gradual caldera collapse at Bárdarbunga volcano, Iceland, regulated by lateral magma outflow
Large volcanic eruptions on Earth commonly occur with a collapse of the roof of a crustal magma reservoir, forming a caldera. Only a few such collapses occur per century, and the lack of detailed observations has obscured insight into the mechanical interplay between collapse and eruption.We usemult...
Published in: | Science |
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Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2016
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Subjects: | |
Online Access: | https://research.manchester.ac.uk/en/publications/a96577cf-06f5-4f40-a0ce-d3ad96c0fd05 https://doi.org/10.1126/science.aaf8988 https://pure.manchester.ac.uk/ws/files/39451470/aaf8988_16June_Bardarbunga_revised_ALL.pdf http://www.scopus.com/inward/record.url?scp=84978402488&partnerID=8YFLogxK |
Summary: | Large volcanic eruptions on Earth commonly occur with a collapse of the roof of a crustal magma reservoir, forming a caldera. Only a few such collapses occur per century, and the lack of detailed observations has obscured insight into the mechanical interplay between collapse and eruption.We usemultiparameter geophysical and geochemical data to show that the 110-squarekilometer and 65-meter-deep collapse of Bárdarbunga caldera in 2014-2015 was initiated through withdrawal of magma, and lateral migration through a 48-kilometers-long dike, from a 12-kilometers deep reservoir. Interaction between the pressure exerted by the subsiding reservoir roof and the physical properties of the subsurface flow path explain the gradual, nearexponential decline of both collapse rate and the intensity of the 180-day-long eruption. |
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