Figure 8. Illustration of the doughnut effect for (a) the 7 November 2016 M  5 Cushing, Oklahoma, earthquake and (b) the 30 October 2016 M  6.6 Norcia, Italy, earthquake. For the Cushing earthquake, the maximum “Did You Feel It?” (DYFI) intensity is of 6.7 at 5.5 km of the epicenter (see Data

with their identification code: (a) event EMSC‐20161030_0000029 30 October 2016 Norcia (Italy; CLO station); (b) event IT‐2009‐0009 6 April 2009 L’Aquila (Italy; AQV station); and (c) event USGS‐us20005iis 15 April 2016 Kumamoto (Japan; KMM18 station). DS, Displacement Spectra; EMSC, European‐Mediterranean Seismological

velocity traces recorded at IT.ACC station (2016 M w  6.5 Norcia, Italy, event) and BO.SMN01 station (2000 M w  6.6 Tottori, Japan, earthquake) and wavelet representation ( Baker, 2007 ) of the velocity pulse (black thick line); (b) velocity traces (fault‐normal components) recorded at two

Figure 2. RRSM event page (see Data and Resources ) for the Norcia (Central Italy) earthquake that occurred on 30 October 2016 at 06:40:18 UTC. There are 121 triaxial station recordings of this event in the RRSM database; the “List of Stations” in the screenshot—ordered by decreasing peak ground

Figure 5. ESM “Event” webpage of the M w  6.5 Norcia (Central Italy) earthquake (see Data and Resources ). The color version of this figure is available only in the electronic edition.

Figure 2. Velocity (Vp left panels, Vp/Vs right panels) along the Norcia fault, Italy, (trace in Fig. 1A ) with snapshots at different times before the largest earthquake: (A) 13 September 2016 (first fully resolved image), (B) 26 October (before Mw 5.5 shock) and (C) 30 October (before main

Figure 3. Velocity (Vp top panels, Vp/Vs lower panels) across the Norcia fault, Italy, (traces in Fig. 1A ) with snapshots at different times before largest earthquake: (A) 13 September 2016, (B) 26 October, and (C) 30 October (before main shock). Purple lines indicate similarly well-resolved