Asta Miklius J. David Wilson Paul G. Okubo Emily Montgomery-Brown Paul Segall Benjamin Brooks James Foster Cecily Wolfe Ellen Syracuse Clifford Thurbe Michael P. Poland 2010 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]. application/pdf 10.1029/2010EO130002 en American Geophysical Union Slow slip event at Kilauea Volcano article