Temporal variations in volumetric magma eruption rates of Quaternary volcanoes in Japan

Abstract Long-term evaluations of hazard and risk related to volcanoes rely on extrapolations from volcano histories, including the uniformity of their eruption rates. We calculated volumetric magma eruption rates, compiled from quantitative eruption histories of 29 Japanese Quaternary volcanoes, an...

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Main Authors: Takahiro Yamamoto, Takashi Kudo, Osamu Isizuka
Format: Article
Language:English
Published: SpringerOpen 2018-04-01
Series:Earth, Planets and Space
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40623-018-0849-x
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spelling doaj-df1ca1ecbe454a488d2c9e705a434f4b2020-11-25T01:14:46ZengSpringerOpenEarth, Planets and Space1880-59812018-04-0170111210.1186/s40623-018-0849-xTemporal variations in volumetric magma eruption rates of Quaternary volcanoes in JapanTakahiro Yamamoto0Takashi Kudo1Osamu Isizuka2Geological Survey of Japan, AISTGeological Survey of Japan, AISTGeological Survey of Japan, AISTAbstract Long-term evaluations of hazard and risk related to volcanoes rely on extrapolations from volcano histories, including the uniformity of their eruption rates. We calculated volumetric magma eruption rates, compiled from quantitative eruption histories of 29 Japanese Quaternary volcanoes, and analyzed them with respect to durations spanning 101–105 years. Calculated eruption rates vary greatly (101–10−4 km3 dense-rock equivalent/1000 years) between individual volcanoes. Although large basaltic stratovolcanoes tend to have high eruption rates and relatively constant repose intervals, these cases are not representative of the various types of volcanoes in Japan. At many Japanese volcanoes, eruption rates are not constant through time, but increase, decrease, or fluctuate. Therefore, it is important to predict whether eruption rates will increase or decrease for long-term risk assessment. Several temporal co-variations of eruption rate and magmatic evolution suggest that there are connections between them. In some cases, magma supply rates increased in response to changing magma-generation processes. On the other hand, stable plumbing systems without marked changes in magma composition show decreasing eruption rates through time.http://link.springer.com/article/10.1186/s40623-018-0849-xEruption rateMagma-discharge step diagramQuaternary volcanoJapan
collection DOAJ
language English
format Article
sources DOAJ
author Takahiro Yamamoto
Takashi Kudo
Osamu Isizuka
spellingShingle Takahiro Yamamoto
Takashi Kudo
Osamu Isizuka
Temporal variations in volumetric magma eruption rates of Quaternary volcanoes in Japan
Earth, Planets and Space
Eruption rate
Magma-discharge step diagram
Quaternary volcano
Japan
author_facet Takahiro Yamamoto
Takashi Kudo
Osamu Isizuka
author_sort Takahiro Yamamoto
title Temporal variations in volumetric magma eruption rates of Quaternary volcanoes in Japan
title_short Temporal variations in volumetric magma eruption rates of Quaternary volcanoes in Japan
title_full Temporal variations in volumetric magma eruption rates of Quaternary volcanoes in Japan
title_fullStr Temporal variations in volumetric magma eruption rates of Quaternary volcanoes in Japan
title_full_unstemmed Temporal variations in volumetric magma eruption rates of Quaternary volcanoes in Japan
title_sort temporal variations in volumetric magma eruption rates of quaternary volcanoes in japan
publisher SpringerOpen
series Earth, Planets and Space
issn 1880-5981
publishDate 2018-04-01
description Abstract Long-term evaluations of hazard and risk related to volcanoes rely on extrapolations from volcano histories, including the uniformity of their eruption rates. We calculated volumetric magma eruption rates, compiled from quantitative eruption histories of 29 Japanese Quaternary volcanoes, and analyzed them with respect to durations spanning 101–105 years. Calculated eruption rates vary greatly (101–10−4 km3 dense-rock equivalent/1000 years) between individual volcanoes. Although large basaltic stratovolcanoes tend to have high eruption rates and relatively constant repose intervals, these cases are not representative of the various types of volcanoes in Japan. At many Japanese volcanoes, eruption rates are not constant through time, but increase, decrease, or fluctuate. Therefore, it is important to predict whether eruption rates will increase or decrease for long-term risk assessment. Several temporal co-variations of eruption rate and magmatic evolution suggest that there are connections between them. In some cases, magma supply rates increased in response to changing magma-generation processes. On the other hand, stable plumbing systems without marked changes in magma composition show decreasing eruption rates through time.
topic Eruption rate
Magma-discharge step diagram
Quaternary volcano
Japan
url http://link.springer.com/article/10.1186/s40623-018-0849-x
work_keys_str_mv AT takahiroyamamoto temporalvariationsinvolumetricmagmaeruptionratesofquaternaryvolcanoesinjapan
AT takashikudo temporalvariationsinvolumetricmagmaeruptionratesofquaternaryvolcanoesinjapan
AT osamuisizuka temporalvariationsinvolumetricmagmaeruptionratesofquaternaryvolcanoesinjapan
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