| Latitude | Longitude | Depth (km) | Dist (Deg) | Dist (Km) | Azimuth | |
|---|---|---|---|---|---|---|
| 51.363 | -178.331 | 27.8 | 66.8 | 7,426 | 55.4 |
Dayplot showing this earthquake on the green line (08:30), lower right.
Local SeisComP3 P-wave Arrivals
| Latitude | Longitude | Depth (km) | Dist (Deg) | Dist (Km) | Azimuth | |
|---|---|---|---|---|---|---|
| -21.671 | 169.804 | 20.0 | 122.4 | 13,592 | 55.5 |
Local SeisComP3 P-wave Arrivals
| Latitude | Longitude | Depth (km) | Dist (Deg) | Dist (Km) | Azimuth | |
|---|---|---|---|---|---|---|
| 36.668 | -97.696 | 5.0 | 17.7 | 1,961 | 71.3 |
Dayplot Image. The event is in green on the 20h line.
Trace of this event. The P to S interval is very weak, with much stronger S and surface waves.
Local SeisComP3 traces.
| Latitude | Longitude | Depth (km) | Dist (Deg) | Dist (Km) | Azimuth | |
|---|---|---|---|---|---|---|
| -31.455 | -69.232 | 109.3 | 71.5 | 7,942 | 354.8 |
Local SeisComP3 P-wave Arrivals
| Latitude | Longitude | Depth (km) | Dist (Deg) | Dist (Km) | Azimuth | |
|---|---|---|---|---|---|---|
| -4.081 | 152.569 | 10.0 | 123.9 | 13,766 | 43.3 |
The May 14, 2019, M 7.5 earthquake in the New Ireland region of Papua New Guinea occurred as the result of shallow strike-slip faulting within the interior of the Pacific plate. Focal mechanism solutions for the earthquake indicate that rupture occurred on either a right-lateral northeast striking or a left-lateral southeast-striking fault. In this region, the Australia plate moves to the east-northeast with respect to the Pacific plate at a velocity of about 105 mm/yr. At the location of the earthquake, some researchers consider the edges of the Australia and Pacific plates to be divided into several microplates that take up the overall convergence between Australia and the Pacific, including the Solomon Sea, South Bismark, and Manus microplates near this event. In this context, the May 14th event occurred along the boundary between the South Bismark and Manus microplates. This fault structure was also the location of a M 8.0 earthquake in November 2000.
While commonly plotted as points on maps, earthquakes of this size are more appropriately described as slip over a larger fault area. Strike-slip events of the size of the May 14, 2019 M 7.5 earthquake are typically about 130×22 km (length x width).
Shallow earthquakes predominantly represent deformation along plate boundaries and associated structures, rather than within subducted slabs where intermediate-depth and deep earthquakes (70–300 and 300+ km, respectively) occur. This region hosts shallow, intermediate-and deep events, and the Australia plate in this region is known to be seismically active to depths of more than 500 km.
Within 250 km of the May 14th M 7.5 earthquake, there have been 36 other events of at least M 7 over the preceding century. Three of these events were M 8 or larger, including the November 16, 2000 M 8.0 earthquake, 45 km to the northwest of this May 14 event. The November 2000 event was also followed by two M 7.8 aftershocks on the subduction zone megathrust interface between the Australia and Pacific plates to the south of this event, respectively 3 hours and 17 hours after the M 8.0 event. The November 2000, M 8.0 earthquake resulted in at least 1 fatality, left several thousand homeless, and triggered several landslides in the nearby region.
P to S-Wave trace in Exton PA
Dayplot showing this event. Note the long term surface waves.
Local SeisComP3 P-wave Arrivals
SeisComP3 Fault Plane Solution
| Latitude | Longitude | Depth (km) | Dist (Deg) | Dist (Km) | Azimuth | |
|---|---|---|---|---|---|---|
| -19.751 | 169.086 | 111.0 | 121.9 | 13,532 | 54.5 |
Waveform between the P and S wave arrivals (0.7 – 2.0 hz Butterworth bandpass filter).
Local SeisComP3 P-wave Arrivals
SeisComp3 Fault Plane Solution
