EARTHQUAKE SWARMS ON MOUNT EREBUS, ANTARCTICA

P(論文) Mount Erebus (77°30'S, 167°09'E, 3794m) is the only active volcano in Antarctica at present. The most notable feature of the volcano is the existence of the convecting lava lake at the summit inner crater for more than ten years. Seven seismic explosion experiments at four different...

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Main Authors: ムラカミ, カツミ, カミヌマ, カツタダ, MURAKAMI, Katsumi, KAMINUMA, Katsutada
Language:English
Published: National Institute of Polar Research 1988
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/2571/files/KJ00002368161.pdf
https://doi.org/10.15094/00002571
https://nipr.repo.nii.ac.jp/records/2571
_version_ 1829302057510633472
author ムラカミ, カツミ
カミヌマ, カツタダ
MURAKAMI, Katsumi
KAMINUMA, Katsutada
author_facet ムラカミ, カツミ
カミヌマ, カツタダ
MURAKAMI, Katsumi
KAMINUMA, Katsutada
author_sort ムラカミ, カツミ
collection National Institute of Polar Research Repository, Japan
description P(論文) Mount Erebus (77°30'S, 167°09'E, 3794m) is the only active volcano in Antarctica at present. The most notable feature of the volcano is the existence of the convecting lava lake at the summit inner crater for more than ten years. Seven seismic explosion experiments at four different shot points were made on Mount Erebus in December 1984. The average numbers of earthquakes per day which occurred around Mount Erebus in 1982,1983,and January-August 1984 are 64,134 and 146 events, and the numbers of earthquake swarms with more than 250 events per 24h are 3,7 and 6 events respectively. A new volcanic eruptive activity began on 13 September 1984 and continued until December. After the activity, the average numbers of earthquakes per day in 1985 and 1986 are 23 and 17 events, and the numbers of earthquake swarms are only one (85-A) and two (86-A, 86-B) events respectively. The earthquake swarm activities of 85-A, 86-A and 86-B are as follows : 1) The durations of the activities are 66,24 and 59h. 2) The total numbers of earthquakes are 2315,357 and 689 events. 3) Only seven earthquakes of 86-A and 86-B were determined to be located in the area beneath Mount Erebus, and the other earthquakes could not be located because the number of the stations is not enough for determining the earthquake locations.Both the activity durations and the total number of earthquakes of the three earthquake swarms are smaller than those of the swarms which occurred before the September 1984 activity. departmental bulletin paper
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
geographic Lava Lake
Mount Erebus
Inner Crater
geographic_facet Lava Lake
Mount Erebus
Inner Crater
id ftnipr:oai:nipr.repo.nii.ac.jp:00002571
institution Open Polar
language English
long_lat ENVELOPE(-128.996,-128.996,55.046,55.046)
ENVELOPE(167.167,167.167,-77.533,-77.533)
ENVELOPE(167.167,167.167,-77.533,-77.533)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00002571
op_relation Proceedings of the NIPR Symposium on Antarctic Geosciences
2
169
AA1072335X
https://nipr.repo.nii.ac.jp/record/2571/files/KJ00002368161.pdf
https://doi.org/10.15094/00002571
https://nipr.repo.nii.ac.jp/records/2571
publishDate 1988
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00002571 2025-04-13T14:10:15+00:00 EARTHQUAKE SWARMS ON MOUNT EREBUS, ANTARCTICA ムラカミ, カツミ カミヌマ, カツタダ MURAKAMI, Katsumi KAMINUMA, Katsutada 1988-09 application/pdf https://nipr.repo.nii.ac.jp/record/2571/files/KJ00002368161.pdf https://doi.org/10.15094/00002571 https://nipr.repo.nii.ac.jp/records/2571 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Antarctic Geosciences 2 169 AA1072335X https://nipr.repo.nii.ac.jp/record/2571/files/KJ00002368161.pdf https://doi.org/10.15094/00002571 https://nipr.repo.nii.ac.jp/records/2571 1988 ftnipr https://doi.org/10.15094/00002571 2025-03-19T10:19:57Z P(論文) Mount Erebus (77°30'S, 167°09'E, 3794m) is the only active volcano in Antarctica at present. The most notable feature of the volcano is the existence of the convecting lava lake at the summit inner crater for more than ten years. Seven seismic explosion experiments at four different shot points were made on Mount Erebus in December 1984. The average numbers of earthquakes per day which occurred around Mount Erebus in 1982,1983,and January-August 1984 are 64,134 and 146 events, and the numbers of earthquake swarms with more than 250 events per 24h are 3,7 and 6 events respectively. A new volcanic eruptive activity began on 13 September 1984 and continued until December. After the activity, the average numbers of earthquakes per day in 1985 and 1986 are 23 and 17 events, and the numbers of earthquake swarms are only one (85-A) and two (86-A, 86-B) events respectively. The earthquake swarm activities of 85-A, 86-A and 86-B are as follows : 1) The durations of the activities are 66,24 and 59h. 2) The total numbers of earthquakes are 2315,357 and 689 events. 3) Only seven earthquakes of 86-A and 86-B were determined to be located in the area beneath Mount Erebus, and the other earthquakes could not be located because the number of the stations is not enough for determining the earthquake locations.Both the activity durations and the total number of earthquakes of the three earthquake swarms are smaller than those of the swarms which occurred before the September 1984 activity. departmental bulletin paper Other/Unknown Material Antarc* Antarctica National Institute of Polar Research Repository, Japan Lava Lake ENVELOPE(-128.996,-128.996,55.046,55.046) Mount Erebus ENVELOPE(167.167,167.167,-77.533,-77.533) Inner Crater ENVELOPE(167.167,167.167,-77.533,-77.533)
spellingShingle ムラカミ, カツミ
カミヌマ, カツタダ
MURAKAMI, Katsumi
KAMINUMA, Katsutada
EARTHQUAKE SWARMS ON MOUNT EREBUS, ANTARCTICA
title EARTHQUAKE SWARMS ON MOUNT EREBUS, ANTARCTICA
title_full EARTHQUAKE SWARMS ON MOUNT EREBUS, ANTARCTICA
title_fullStr EARTHQUAKE SWARMS ON MOUNT EREBUS, ANTARCTICA
title_full_unstemmed EARTHQUAKE SWARMS ON MOUNT EREBUS, ANTARCTICA
title_short EARTHQUAKE SWARMS ON MOUNT EREBUS, ANTARCTICA
title_sort earthquake swarms on mount erebus, antarctica
url https://nipr.repo.nii.ac.jp/record/2571/files/KJ00002368161.pdf
https://doi.org/10.15094/00002571
https://nipr.repo.nii.ac.jp/records/2571