SeisComP3 traces for AM.R8C73.00.SHZ (Exton PA), LD.WUPA.BHZ (West Chester University, West Chester PA), and PE.PSUB.HHZ (Penn State Delaware County Campus).

Distance: 32.0 deg. – 3,542 km

Azimuth: 10.9 deg.

SeisComP3 display showing the focal mechanism for this event.

Jamaseis heliocoder trace of AM.RC8C73.00.SHZ showing the main shock and an aftershock
Distance: 144.5 Deg. 16,100km
Azimuth: 20.6 Deg.

SeisComP3 traces for AM.R8C73.00.SHZ (Exton PA), LD.WUPA.BHZ (West Chester University, West Chester PA). PE.PSUB.HHZ (Penn State Delaware County Campus), and LD.TUPA.HHZ (Temple University Ambler Campus) showing the P wave arrivals.

Jamaseis heliocoder trace of AM.RC8C73.00.SHZ. Notice the high amplitude surface waves in the image. These can be seen in the trace for almost two hours after onset.

Distance: 45.8 Deg. 5,159 km
Azimuth: 92.5 Deg.

Another Jamaseis image (AM.R8C73.00.SHZ, Exton) showing the initial earthquake as well as the magnitude 6.1 aftershock that occurred at 21:15:01 UTC

Here is the trace from LD.WUPA.BHZ at West Chester University about 10 km (6 miles) south of AM.R8C73.00.SHZ. WUPA is a broad-band seismometer which is sensitive down to about .01 Hz, i.e. a period of almost two minutes. Note that the surface waves are even stronger at these lower frequencies, particularly around 10 – 15 seconds per cycle.

SeisComP3 traces for AM.R8C73.00.SHZ (Exton PA), LD.WUPA.BHZ (West Chester University, West Chester PA), PE.PSUB.HHZ (Peen State Delaware County Campus), and LD.TUPA.HHZ (Temple University Ambler Campus) showing the P wave arrivals.

This SeisComP3 screenshot shows the focal mechanism which is typical of a strike-slip fault.

SeisComP3 traces for AM.R8C73.00.SHZ (Exton PA) and LD.WUPA.BHZ (West Chester University, West Chester PA) showing the P wave arrivals. This shows that under the right circumstances, even modest earthquakes can be detected over great distances (over 16,000 km in this case).

Distance: 146.6 deg, 16,301 km

Azimuth: 16.5 deg.

“The August 5, 2018, M 6.9 earthquake in Pulau Lombok, Indonesia, occurred as the result of shallow thrust fault on or near The Flores Back Arc Thrust. Preliminary focal mechanisms for the earthquake indicates slip occurred on either a shallow, south-dipping thrust fault, or on a steep, north dipping reverse fault. At the latitude of this earthquake, the Sunda and Australia plates converge in a north-south direction at a rate of about 70 mm/yr. The location of this earthquake is consistent with it occurring as southward-oriented thrust faulting on the Flores Back Arc Thrust.

At the location of this event, the Sunda plate underthrusts the Indonesian Arc to the south, along the Flores Back Arc Thrust local to this earthquake, and along the Wetar Back Arc Thrust farther to the east. To the south, the Australia plate also underthrusts the arc to the north, along the Java Trench. This Flores region marks the transition between traditional oceanic plate subduction in the west (Australia plate beneath Sunda) to continental collision in the east. As a result, two opposite-verging thrust systems are evident in cross-sections, and the northward subducting slab of the Australia plate exists at depth beneath the Indonesian Islands and the Flores Sea. The focal mechanism solution and depth of this earthquake indicate it is associated with the Flores Back Arc Thrust system, rather than the deeper Australia slab.

In the region surrounding the August 5, 2018 earthquake, there have been six other events of M 6.5 or larger over the previous century. Four of these are likely to have occurred on the back arc thrust system; a M 6.5 in the Bali region to the west of Lombok in July 1976, and three events of M 6.5, M6.5, and M 6.6 in the Sumbawa region to the east of Lombok in November 2007 and November 2009. The Sumbawa earthquakes were associated with several deaths, hundreds of injuries, and hundreds of houses being destroyed.”

SeisComP3 traces for AM.R8C73.00.SHZ (Exton PA) and LD.WUPA.BHZ (West Chester University, West Chester PA).

Distance: 146.5 deg, 16,290 km

Azimuth 16.8 deg

These images are of a M5.7 aftershock that occurred two days later (Aug 9, 2018 @ 05:25:35 UTC).