Classification of long-term very long period (VLP) volcanic earthquakes at Whakaari/White Island volcano, New Zealand

Abstract We have observed very long period earthquakes (VLPs) over the period 2007 to the end of 2019 at Whakaari/White Island volcano, New Zealand. The earthquakes exhibit similitude between waveforms which suggests repeating source locations and processes. VLPs recorded at two permanent stations w...

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Main Authors: Iseul Park, Arthur Jolly, Ivan Lokmer, Ben Kennedy
Format: Article
Language:English
Published: SpringerOpen 2020-07-01
Series:Earth, Planets and Space
Subjects:
VLP
Online Access:http://link.springer.com/article/10.1186/s40623-020-01224-z
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spelling doaj-34db6e80b1774d4ba4824ed1540506172020-11-25T04:04:44ZengSpringerOpenEarth, Planets and Space1880-59812020-07-0172111010.1186/s40623-020-01224-zClassification of long-term very long period (VLP) volcanic earthquakes at Whakaari/White Island volcano, New ZealandIseul Park0Arthur Jolly1Ivan Lokmer2Ben Kennedy3Department of Geological Sciences, University of CanterburyGNS ScienceSchool of Earth Sciences, University College DublinDepartment of Geological Sciences, University of CanterburyAbstract We have observed very long period earthquakes (VLPs) over the period 2007 to the end of 2019 at Whakaari/White Island volcano, New Zealand. The earthquakes exhibit similitude between waveforms which suggests repeating source locations and processes. VLPs recorded at two permanent stations were detected using waveform semblance and were then classified into two main families (F1 and F2) using a clustering analysis. The two families are characterized by ‘mirror image’ reverse waveform polarity suggesting that they are genetically related, but occur during different evolutionary phases of volcanic activity. F1 events occurred throughout the observation period, while F2 events mainly occurred as swarms that mark the onset of volcanic unrest. A detailed cluster analysis reveals possible sub-families implying slight temporal evolutions within a family. Our results add to our understanding of the volcanic magma–hydrothermal system at Whakaari/White Island indicating that relatively stable VLP sources may be exploited to improve monitoring for future unrest.http://link.springer.com/article/10.1186/s40623-020-01224-zVLPEarthquake familySwarmVolcanic unrestClustering analysis
collection DOAJ
language English
format Article
sources DOAJ
author Iseul Park
Arthur Jolly
Ivan Lokmer
Ben Kennedy
spellingShingle Iseul Park
Arthur Jolly
Ivan Lokmer
Ben Kennedy
Classification of long-term very long period (VLP) volcanic earthquakes at Whakaari/White Island volcano, New Zealand
Earth, Planets and Space
VLP
Earthquake family
Swarm
Volcanic unrest
Clustering analysis
author_facet Iseul Park
Arthur Jolly
Ivan Lokmer
Ben Kennedy
author_sort Iseul Park
title Classification of long-term very long period (VLP) volcanic earthquakes at Whakaari/White Island volcano, New Zealand
title_short Classification of long-term very long period (VLP) volcanic earthquakes at Whakaari/White Island volcano, New Zealand
title_full Classification of long-term very long period (VLP) volcanic earthquakes at Whakaari/White Island volcano, New Zealand
title_fullStr Classification of long-term very long period (VLP) volcanic earthquakes at Whakaari/White Island volcano, New Zealand
title_full_unstemmed Classification of long-term very long period (VLP) volcanic earthquakes at Whakaari/White Island volcano, New Zealand
title_sort classification of long-term very long period (vlp) volcanic earthquakes at whakaari/white island volcano, new zealand
publisher SpringerOpen
series Earth, Planets and Space
issn 1880-5981
publishDate 2020-07-01
description Abstract We have observed very long period earthquakes (VLPs) over the period 2007 to the end of 2019 at Whakaari/White Island volcano, New Zealand. The earthquakes exhibit similitude between waveforms which suggests repeating source locations and processes. VLPs recorded at two permanent stations were detected using waveform semblance and were then classified into two main families (F1 and F2) using a clustering analysis. The two families are characterized by ‘mirror image’ reverse waveform polarity suggesting that they are genetically related, but occur during different evolutionary phases of volcanic activity. F1 events occurred throughout the observation period, while F2 events mainly occurred as swarms that mark the onset of volcanic unrest. A detailed cluster analysis reveals possible sub-families implying slight temporal evolutions within a family. Our results add to our understanding of the volcanic magma–hydrothermal system at Whakaari/White Island indicating that relatively stable VLP sources may be exploited to improve monitoring for future unrest.
topic VLP
Earthquake family
Swarm
Volcanic unrest
Clustering analysis
url http://link.springer.com/article/10.1186/s40623-020-01224-z
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