Volcanic earthquake swarms at Mt. Erebus, Antarctica

1985 ◽  
Vol 114 (1-4) ◽  
pp. 357-369 ◽  
Author(s):  
Katsutada Kaminuma ◽  
Sadato Ueki ◽  
Kienle Juergen
1996 ◽  
Vol 39 (2) ◽  
Author(s):  
J. P. Benoit ◽  
S. R. McNutt

Global data from 1979 to 1989 pertaining to volcanic earthquake swarms have been compiled into a custom-designed relational database. The database is composed of three sections: 1) a section containing general information on volcanoes, 2) a section containing earthquake swarm data (such as dates of swarm occurrence and durations), and 3) a section containing eruption information. The most abundant and reliable parameter, duration of volcanic earthquake swarms, was chosen for preliminary analysis. The distribution of all swarm durations was found to have a geometric mean of 5.5 days. Precursory swarms were then separated from those not associated with eruptions. The geometric mean precursory swarm duration was 8 days whereas the geometric mean duration of swarms not associated with eruptive activity was 3.5 days. Two groups of precursory swarms are apparent when duration is compared with the eruption repose time. Swarms with durations shorter than 4 months showed no clear relationship with the eruption repose time. However, the second group, lasting longer than 4 months, showed a significant positive correlation with the log10 of the eruption repose period. The two groups suggest that different suites of physical processes are involved in the generation of volcanic earthquake swarms.


2009 ◽  
Vol 36 (17) ◽  
Author(s):  
Karin Bräuer ◽  
Horst Kämpf ◽  
Gerhard Strauch
Keyword(s):  

2000 ◽  
Vol 101 (1-2) ◽  
pp. 83-104 ◽  
Author(s):  
J Neuberg ◽  
R Luckett ◽  
B Baptie ◽  
K Olsen

2012 ◽  
Vol 331-332 ◽  
pp. 215-223 ◽  
Author(s):  
O. Lengliné ◽  
J.E. Elkhoury ◽  
G. Daniel ◽  
J. Schmittbuhl ◽  
R. Toussaint ◽  
...  

2021 ◽  
Vol 574 ◽  
pp. 117160
Author(s):  
Wei Peng ◽  
David Marsan ◽  
Kate Huihsuan Chen ◽  
Erwan Pathier

1982 ◽  
Vol 72 (5) ◽  
pp. 1591-1599
Author(s):  
Anthony Qamar ◽  
Jerry Kogan ◽  
Michael C. Stickney

abstract Since 1900, more than 290 earthquakes have been reported near Flathead Lake, Montana. Surprisingly, none has exceeded magnitude 5 to 512. Most recent earthquake swarms appear to result from east-west or northwest-southeast extension along short fault segments west and north of the lake. Major normal faults like the Swan and Mission faults east of the lake may pose higher risk, but they appear dormant today. Deformation of sediments in Flathead Lake may be caused by several large earthquakes more than 10,000 years ago but is more probably due to glacial processes accompanying the last retreat of the Cordilleran ice sheet.


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