September 11, 2018
Earthquake Research Committee,
Headquarters for Earthquake Research Promotion

Evaluation of Seismic Activities for August 2018

1 Major Seismic Activities

There was no remarkable activity.

2 Nationwide Seismic Activities by Region

(1) Hokkaido Region

There was no remarkable activity.

(2) Tohoku Region

* On August 8, there was a magnitude (M) 5.6 earthquake at a depth of approximately 30 km (due to CMT solution), offshore Sanriku. The focal mechanism showed a normal fault type with a tension axis in a WNW-ESE direction. This event occurred within the Pacific plate.

* On August 11, there was an M5.0 earthquake at a depth of approximately 20 km, offshore Fukushima prefecture. The focal mechanism showed a normal fault type with a tension axis in an NNW-SSE direction. This event occurred within the continental crust.

* On August 24, there was an M5.1 earthquake at a depth of approximately 30 km, offshore east of Aomori prefecture. The focal mechanism showed a reverse fault type with a compression axis in a WNW-ESE direction. This event occurred at the boundary between the Pacific and the continental plates.

(3) Kanto-Chubu Region

* On August 17 at 03:23 (JST), there was an M6.6 earthquake at a depth of approximately 10 km (due to CMT solution) in the ocean area near Ioto Island. The focal mechanism showed a reverse fault type with a compression axis in an E-W direction. This event occurred at the boundary between the Pacific and the Philippine Sea plates. In addition, on the same day at 03:21 (JST), there was an M6.3 earthquake in the neighborhood of the recent event.

(4) Kinki-Chugoku-Shikoku Region

There was no remarkable activity.

(5) Kyushu-Okinawa Region

* On August 22, there was an M4.1 earthquake at a depth of approximately 10 km in the Kumamoto region, Kumamoto prefecture. The focal mechanism showed a normal fault type with a tension axis in an N-S direction. This event occurred within the crust.

(6) Around the Nankai Trough

* There has been observed no unusual change which indicates that the possibility of occurrence of great earthquakes along the Nankai Trough has relatively raised compared to the normal time.

Supplement

* On September 5, there was an M5.5 earthquake offshore Ibaraki prefecture. The focal mechanism showed a reverse fault type with a compression axis in an E-W direction.

* Refer to the other term for the 2018 Hokkaido Eastern Iburi Earthquake.



Supplementary Information to the Evaluation of Seismic Activities for August 2018

September 11, 2018
Earthquake Research Committee

1 Major Seismic Activities

The following are the numbers of earthquakes by magnitude (M) that occurred in Japan and the surrounding area during August 2018.

(reference)

The following events for the period from August 2017 to late July 2018 have been listed as "Major Seismic Activities" in monthly "Evaluation of Seismic Activities."

  – Southern Inland, Akita Prefecture  M5.2 on September 8, 2017
(Depth of approximately 10 km)
  – Offshore Fukushima Prefecture  M5.9 on October 6, 2017
(Depth of approximately 55 km)
  – Near Iriomotejima  M5.6 on March 1, 2018
(Depth of approximately 15 km)
  – Western Shimane Prefecture  M6.1 on April 9, 2018
(Depth of approximately 10 km)
  – Offshore southeast of Nemuro Prninsula  M5.4 on April 14, 2018
(Depth of approximately 55 km)
  – Northern Nagano Prefecture  M5.2 on May 12, 2018
(Depth of approximately 10 km)
  – Northern Nagano Prefecture  M5.2 on May 25, 2018
(Depth of approximately 5km)
  – Southern Gunma Prefecture  M4.6 on June 17, 2018
(Depth of approximately 15 km)
  – Northern Osaka Prefecture  M6.1 on June 18, 2018
(Depth of approximately 15 km)
  – Offshore East of Chiba Prefecture  M6.0 on July 7, 2018
(Depth of approximately 55 km)

2 Nationwide Seismic Activities by Region

(1) Hokkaido Region

There is no supplementary information for Hokkaido region.

(2) Tohoku Region

There is no supplementary information for Tohoku region.

(3) Kanto-Chubu Region

There is no supplementary information for Kanto region.

(4) Kinki-Chugoku-Shikoku Region

There is no supplementary information for Kinki-Chugoku-Shikoku region.

(5) Kyushu-Okinawa Region

–"On August 22, there was an M4.1 earthquake at a depth of approximately 10 km in the Kumamoto region, Kumamoto prefecture. (Excerpted)":
The serial activity of the 2016 Kumamoto Earthquakes in the Kumamoto and Aso regions, Kumamoto prefecture still remains, though it is continually decaying as a whole. The present activity will continue for the time beeing. GNSS observation result shows the slight aftershock deformation still continues.

(6) Around the Nankai Trough

–"There has been observed no unusual change which indicates that the possibility of occurrence of great earthquakes along the Nankai Trough has relatively raised compared to the normal time.":
(This evaluation is in agreement with the views presented at the regular meeting on September 7 of the Assessment Committee for Earthquakes along the Nankai Trough (reference below).)

(Reference)

Recent Crustal Activity Around the Nankai Trough (Seismological and Volcanological Department, Japan Meteorological Agency, September 7, 2018)
"In the present, there has been observed no unusual change which indicates that the possibility of occurrence of great earthquakes along the Nankai Trough has relatively raised compared to the normal time.(Excerpted)"

Reference 1
Earthquakes that are described in the "Evaluation of Seismic Activity" (Monthly Report of Seismic Activity in Japan) have the following features.

  1. Events of M6.0 or greater, or events that have maximum seismic intensity 4 or greater
  2. Onshore events of M4.5 or greater that have maximum seismic intensity 3 or greater
  3. Events under the ocean areas of M5.0 or greater that have maximum seismic intensity 3 or greater

Reference 2
Information that is described in the "Supplementary Information to the Evaluation" includes:

  1. Reference information related to the seismic activity described in the "Evaluation of Seismic Activity"
  2. Recent earthquake activity over the past year related to the events described in "Major Seismic Activity" in the "Evaluation of Seismic Activity"
  3. Seismic activity that has been evaluated, but not included in the "Evaluation of Seismic Activity" because it is within normal bounds and not prominent
  4. A sequence of slow-slip events of estimated M6.0 or greater and accompanying low-frequency earthquakes (tremors)