Chile – M6.4 – June 14, 2019 at 00:19:12 UTC

72km W of Coquimbo, Chile

Latitude Longitude Depth (km) Dist (Deg) Dist (Km) Azimuth
-30.056 -72.082 11.0 70.0 7,766 357.1

 

USGS Information Page

Local SeisComP3 P-wave Arrivals

Pennsylvania – M3.4 – June 13, 2019 at 00:30:57 UTC

18km SSW of Mifflintown, Pennsylvania

Latitude Longitude Depth (km) Dist (Deg) Dist (Km) Azimuth
40.422 -77.506 26.7 1.51 168 104.9

 

USGS Information Page

This small quake was local to our area and showed a strong response on local seismometers, although it was not felt in southeastern PA.

Full waveform at R8C73.00.SHZ

Comparison with LD.WUPA.HHZ 10 km south

SeisComP3 scolv display of this event

Ohio – M4.0 – June 10, 2019 at 14:50:44 UTC

5km NNW of Eastlake, Ohio

Latitude Longitude Depth (km) Dist (Deg) Dist (Km) Azimuth
41.703 -81.475 2.0 4.8 529 108.8

 

USGS Information Page

El Salvador – M6.6 – May 30, 2019 at 09:03:32 UTC

27km SSE of La Libertad, El Salvador

Latitude Longitude Depth (km) Dist (Deg) Dist (Km) Azimuth
13.243 -89.272 65.1 29.3 3,255 21.8

 

USGS Information Page

Dayplot of this earthquake

P to S interval trace (no filter).

Local SeisComP3 P-wave Arrivals

Fault Plane Solution

Alaska – M5.8 – May 27, 2019 at 09:52:21 UTC

89km SSW of Homer, Alaska

Latitude Longitude Depth (km) Dist (Deg) Dist (Km) Azimuth
58.861 -152.351 65.4 50.3 5,588 76.2

 

USGS Information Page

P to S interval trace

Local P-wave Arrivals

Peru – M8.0 – May 26, 2019 at 07:41:14 UTC

75km SSE of Lagunas, Peru

Latitude Longitude Depth (km) Dist (Deg) Dist (Km) Azimuth
-5.796 -75.298 109.9 45.7 5,073 359.6

 

USGS Information Page

Tectonic Summary

From the USGS information page:

The May 26, 2019, M 8.0 northern Peru earthquake occurred as the result of normal faulting at an intermediate depth, approximately 110 km beneath the Earth’s surface within the subducted lithosphere of the Nazca plate. Focal mechanism solutions indicate that rupture occurred on either a north- or south-striking, moderately dipping normal fault. At the location of the earthquake, the Nazca plate moves to the east relative to the South America plate at a velocity of about 70 mm/yr, subducting at the Peru-Chile Trench, to the west of the Peruvian coast and the May 26th earthquake. Earthquakes of northern Peru and most of western South America are due to strains generated by this ongoing subduction; at this latitude, the Nazca plate is seismically active to depths of about 650 km. This earthquake occurred in a segment of the subducted plate that has produced frequent earthquakes with focal depths of 100 to 150 km.

Earthquakes like this event, with focal depths between 70 and 300 km, are commonly termed “intermediate-depth” earthquakes. Intermediate-depth earthquakes represent deformation within subducted slabs rather than at the shallow plate interface between subducting and overriding tectonic plates. They typically cause less damage on the ground surface above their foci than is the case with similar-magnitude shallow-focus earthquakes, but large intermediate-depth earthquakes may be felt at great distance from their epicenters.

While commonly plotted as points on maps, earthquakes of this size are more appropriately described as slip over a larger fault area. Normal events of the size of the May 26, 2019 M 8.0 earthquake are typically about 180×50 km (length x width).

Large intermediate-depth earthquakes are reasonably common in this section of the Nazca slab, and three other intermediate-depth M 7+ events have occurred within 250 km of the September 26th earthquake over the past three decades. A M 7.5 earthquake in September 2005, located at a similar depth but approximately 130 km to the west of the May 26th, 2019 earthquake, caused 5 deaths, about 70 injuries, and significant damage in the surrounding region.

Day plot of this event.

Jamaseis trace of the above.

Trace of Am.R8C73.00.SHZ (no filter) showing a maximum of +/- 8000 counts.

Displacement trace. Displacement was over 30 micrometers.

Local SeisComP3 P-wave Arrivals

Long period SeisComP3 traces of local stations (no filter applied).

Fault Plane Solution for this earthquake