Item talk:Q314099
From geokb
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"name": "Slow slip event at Kilauea Volcano",
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"url": "https://doi.org/10.1029/2010EO130002"
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"name": "Eos, Transactions, American Geophysical Union",
"volumeNumber": "91",
"issueNumber": "13"
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"datePublished": "2010",
"dateModified": "2018-10-30",
"abstract": "Early in the morning of 1 February 2010 (UTC; early afternoon 31 January 2010 local time), continuous Global Positioning System (GPS) and tilt instruments detected a slow slip event (SSE) on the south flank of Kilauea volcano, Hawaii. The SSE lasted at least 36 hours and resulted in a maximum of about 3 centimeters of seaward displacement. About 10 hours after the start of the slip, a flurry of small earthquakes began (Figure 1) in an area of the south flank recognized as having been seismically active during past SSEs [Wolfe et al., 2007], suggesting that the February earthquakes were triggered by stress associated with slip [Segall et al., 2006].",
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"name": "American Geophysical Union"
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"name": "Poland, Michael P. mpoland@usgs.gov",
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"url": "https://www.usgs.gov/centers/volcano-science-center"
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"name": "Okubo, Paul G. pokubo@usgs.gov",
"givenName": "Paul G.",
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