Iceshock Swarms Observed at Mizuho Camp, Antarctica
The wintering party of the 14th Japanese Antarctic Research Expedition carried out a temporary seismological observation with one vertical component seismograph at the Mizuho Camp on September 10-27, 1973. The Mizuho Camp is located at about 300km southeast of Syowa Station in Antarctica, where the...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
National Institute of Polar Research
1975
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Subjects: | |
Online Access: | https://doi.org/10.15094/00007835 https://doaj.org/article/8030a3489e7b4d77a491fcd74afe8d6d |
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author | Katsutada KAMINUMA Masayoshi TAKAHASHI |
author_facet | Katsutada KAMINUMA Masayoshi TAKAHASHI |
author_sort | Katsutada KAMINUMA |
collection | Unknown |
description | The wintering party of the 14th Japanese Antarctic Research Expedition carried out a temporary seismological observation with one vertical component seismograph at the Mizuho Camp on September 10-27, 1973. The Mizuho Camp is located at about 300km southeast of Syowa Station in Antarctica, where the ice thickness is about 2,100 m. The seismological observation was disturbed by the ground noise of many kinds of artificial origin, but good records for 210 hours in total were obtained. Natural earthquakes were not detected by this temporary observation, but many iceshocks, mostly of swarm type, were recorded. These swarms occurred in the nighttime. The air temperature during the iceshocks was below -35℃, and the falling rate of temperature was -2.5℃ per hour for a short period, or about -1℃/hour though the lowering continued for a few hours. When the largest swarm during this observation period occurred, the wintering members at the Mizuho Camp heard sound from shocks and recognized many cracks on the snow surface around the area of the sound. Therefore, the depth of the swarm was estimated to be very shallow. Some shocks were interpreted to have been originated from the upper snow layers quite near the surface, so they may be called snowquakes. |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctic Antarctica |
genre_facet | Antarc* Antarctic Antarctica |
geographic | Antarctic Syowa Station Mizuho |
geographic_facet | Antarctic Syowa Station Mizuho |
id | fttriple:oai:gotriple.eu:oai:doaj.org/article:8030a3489e7b4d77a491fcd74afe8d6d |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(44.317,44.317,-70.683,-70.683) |
op_collection_id | fttriple |
op_doi | https://doi.org/10.15094/00007835 |
op_relation | doi:10.15094/00007835 0085-7289 2432-079X https://doaj.org/article/8030a3489e7b4d77a491fcd74afe8d6d |
op_rights | undefined |
op_source | Antarctic Record, Iss 54, Pp 75-83 (1975) |
publishDate | 1975 |
publisher | National Institute of Polar Research |
record_format | openpolar |
spelling | fttriple:oai:gotriple.eu:oai:doaj.org/article:8030a3489e7b4d77a491fcd74afe8d6d 2025-01-16T19:09:27+00:00 Iceshock Swarms Observed at Mizuho Camp, Antarctica Katsutada KAMINUMA Masayoshi TAKAHASHI 1975-12-01 https://doi.org/10.15094/00007835 https://doaj.org/article/8030a3489e7b4d77a491fcd74afe8d6d en other eng National Institute of Polar Research doi:10.15094/00007835 0085-7289 2432-079X https://doaj.org/article/8030a3489e7b4d77a491fcd74afe8d6d undefined Antarctic Record, Iss 54, Pp 75-83 (1975) geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1975 fttriple https://doi.org/10.15094/00007835 2023-01-22T18:04:04Z The wintering party of the 14th Japanese Antarctic Research Expedition carried out a temporary seismological observation with one vertical component seismograph at the Mizuho Camp on September 10-27, 1973. The Mizuho Camp is located at about 300km southeast of Syowa Station in Antarctica, where the ice thickness is about 2,100 m. The seismological observation was disturbed by the ground noise of many kinds of artificial origin, but good records for 210 hours in total were obtained. Natural earthquakes were not detected by this temporary observation, but many iceshocks, mostly of swarm type, were recorded. These swarms occurred in the nighttime. The air temperature during the iceshocks was below -35℃, and the falling rate of temperature was -2.5℃ per hour for a short period, or about -1℃/hour though the lowering continued for a few hours. When the largest swarm during this observation period occurred, the wintering members at the Mizuho Camp heard sound from shocks and recognized many cracks on the snow surface around the area of the sound. Therefore, the depth of the swarm was estimated to be very shallow. Some shocks were interpreted to have been originated from the upper snow layers quite near the surface, so they may be called snowquakes. Article in Journal/Newspaper Antarc* Antarctic Antarctica Unknown Antarctic Syowa Station Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) |
spellingShingle | geo Katsutada KAMINUMA Masayoshi TAKAHASHI Iceshock Swarms Observed at Mizuho Camp, Antarctica |
title | Iceshock Swarms Observed at Mizuho Camp, Antarctica |
title_full | Iceshock Swarms Observed at Mizuho Camp, Antarctica |
title_fullStr | Iceshock Swarms Observed at Mizuho Camp, Antarctica |
title_full_unstemmed | Iceshock Swarms Observed at Mizuho Camp, Antarctica |
title_short | Iceshock Swarms Observed at Mizuho Camp, Antarctica |
title_sort | iceshock swarms observed at mizuho camp, antarctica |
topic | geo |
topic_facet | geo |
url | https://doi.org/10.15094/00007835 https://doaj.org/article/8030a3489e7b4d77a491fcd74afe8d6d |