Seismic activity of Mount Erebus, Antarctica in 1982-1983

Mount Erebus is an active volcano with a persistent convecting lava lake at the summit crater, located on Ross Island, Antarctica. Since December 1980 the seismic activity of Mount Erebus has been continuously monitored using a radio-telemetered network of six seismic stations. A 50-day temporary se...

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Bibliographic Details
Main Authors: Sadato Ueki, Katsutada Kaminuma, Megumi Baba, Etsuro Koyama, Juergen Kienle
Format: Report
Language:English
Published: Faculty of Science, Tohoku University/National Institute of Polar Research/Department of Earth Science, Faculty of Science, Chiba University/Earthquake Research Institute, University of Tokyo/Geophysical Institute, University of Alaska 1984
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Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1637
http://id.nii.ac.jp/1291/00001637/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1637&item_no=1&attribute_id=18&file_no=1
Description
Summary:Mount Erebus is an active volcano with a persistent convecting lava lake at the summit crater, located on Ross Island, Antarctica. Since December 1980 the seismic activity of Mount Erebus has been continuously monitored using a radio-telemetered network of six seismic stations. A 50-day temporary seismic observation was also carried out in the 1982-1983 Antarctic field season. The following seismic activities were observed during this field season : 1) Explosion earthquakes accompanied with Strombolian eruptions from the lava lake occurred at a rate of 0-4 times per day which is slightly lower than the rate in the previous season; 2) an intense earthquake swarm, which is possibly related to the underground movement of magma, occurred in October 1982 near Abbott Peak, 10km northwest of the summit; 3) there were other source regions of seismicity in Ross Island, fairly distant from Mount Erebus to the east.