Off Oregon Coast – M5.4 – Aug 16, 2019 at 15:23:19 UTC

Off the coast of Oregon

Latitude Longitude Depth (km) Dist (Deg) Dist (Km) Azimuth
44.262 -129.373 10.0 39.5 4,390 76.8

 

USGS Information Page

Local SeisComP3 P-wave Arrivals

Kansas – M4.2 – Aug 16, 2019 at 12:59:10 UTC

4km WSW of South Hutchinson, Kansas

Latitude Longitude Depth (km) Dist (Deg) Dist (Km) Azimuth
38.010 -97.988 5.0 17.5 1,946 76.4

 

USGS Information Page

Helicorder trace

Local SeisComP3 P-wave Arrivals

Mexico – M5.8 – Aug 14, 2019 at 21:35:19 UTC

262km NE of Socorro Island, Mexico

Latitude Longitude Depth (km) Dist (Deg) Dist (Km) Azimuth
20.469 -109.240 10.0 34.7 3,859 48.3

 

USGS Information Page

Waveform showing P-S and surface waves. The trace was rather weak at this location, but can be seen over the noise when filtered.

Heliocorder trace.

Local SeisComP3 P-wave Arrivals

Fault Plane Solution

Mexico – M5.5 – Aug 12, 2019 at 20:39:34 UTC

14km SSE of Tonala, Mexico

Latitude Longitude Depth (km) Dist (Deg) Dist (Km) Azimuth
15.958 -93.699 92.6 28.7 3,192 29.8

 

USGS Information Page

Local SeisComP3 P-wave Arrivals

Indonesia – M6.9 – Aug 2, 2019 at 12:03:27 UTC

102km WSW of Tugu Hilir, Indonesia

Latitude Longitude Depth (km) Dist (Deg) Dist (Km) Azimuth
-7.267 104.825 52.8 147.3 16,376 0.6

 

USGS Information Page

Tectonic Summary

From the USGS Information Page

The August 2, 2019, M 6.9 earthquake off the western end of the Indonesian island of Java occurred as the result of oblique reverse faulting, near the boundary between the Australia and Sunda plates. Focal mechanism solutions for the event indicate rupture occurred on either a moderately dipping fault striking towards the SSW, or on a moderately dipping fault striking towards the ENE. At the location of this earthquake, the Australian plate is moving northeast relative to the Sunda plate at a rate of approximately 60 mm/yr. The Australia plate begins subducting beneath the Sunda Plate at the Sunda-Java trench, approximately 100 km southwest of this earthquake. The location, depth and preliminary focal mechanism solution for this earthquake indicate the event likely occurred within the subducting lithosphere of the Australia plate, rather than on the shallower interplate thrust boundary.The plate boundary region between the Australia and Sunda plates is highly seismically active, with past strong earthquakes having occurred within each of the Australia and Sunda plates as well as on the plate interface. Two earthquakes above M 7.0 have occurred within 250 km of this event within the past century, including a M 7.1 and M 7.6 events in 1943 and 1933, respectively. Further afield, the M 7.8 earthquake of June 2, 1994, and the M 7.7 earthquake of July 17, 2006, both of which occurred south of Java and both of which produced destructive tsunamis, occurred as the result of thrust faulting on the shallow plate interface near the Sunda-Java Trench. The devastating Yogyakarta earthquake of May 26, 2006, M 6.3, occurred at shallow depth within the overriding Sunda plate, 600 km to the east of the August 2, 2019 event, killing more than 5000 people. The M 7.5 Java earthquake of August 28, 2007, occurred at a depth of about 290 km within the subducted Australia plate, 325 km to the northeast of today’s event.

Heliocorder Traces

P to S interval waveform

Local SeisComP3 P-wave Arrivals

Fault Plane Solution