July 9, 2019
Earthquake Research Committee,
Headquarters for Earthquake Research Promotion

Evaluation of Seismic Activities for June 2019

1 Major Seismic Activities

* On June 18, there was a magnitude (M) 6.7 earthquake offshore Yamagata prefecture. Maximum seismic intensity 6 Upper was observed in Niigata prefecture and damage was caused with injured persons and so on.

2 Nationwide Seismic Activities by Region

(1) Hokkaido Region

There was no remarkable activity.

(2) Tohoku Region

With regard to the earthquake offshore Yamagata prefecture on June 18, refer to another report (Evaluation of Earthquake Offshore Yamagata Prefecture on June 18, 2019).

(3) Kanto-Chubu Region

* On June 1, there was an M4.7 earthquake at a depth of approximately 35 km under the northeastern Chiba prefecture. The focal mechanism showed a normal fault type with a tension axis in a WNW-ESE direction. This event occurred within the Philippine Sea plate. In the vicinity of this event, there was an M5.1 earthquake on May 25.

* On June 4, there was an M6.2 earthquake at a depth of approximately 450 km under the ocean area near Torishima Island. The focal mechanism had a compression axis in the subducting direction of the Pacific plate. This event occurred within the Pacific plate.

* On June 17, there was an M5.1 earthquake at a depth of approximately 75 km under the northern Ibaraki prefecture. The focal mechanism showed a normal fault type with a tension axis in an ENE-WSW direction. This event occurred within the Pacific plate.

* On June 24, there was an M5.2 earthquake at a depth of approximately 60 km, offshore southeast of Chiba prefecture. The focal mechanism showed a reverse fault type with a compression axis in an NNW-SSE direction. This event occurred within the Philippine Sea plate.

* On June 24, there was an M4.1 earthquake at a depth of approximately 10 km, offshore east of the Izu Peninsula. The focal mechanism showed a strike-slip fault type with a compression axis in an NNW-SSE direction. This event occurred within the crust of the Philippine Sea plate.

(4) Kinki-Chugoku-Shikoku Region

There was no remarkable activity.

(5) Kyushu-Okinawa Region

There was no remarkable activity.

(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.



Supplementary Information to the Evaluation of Seismic Activities for June 2019

July 9, 2019
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 June 2019.

(reference)

The following events for the period from June 2018 to late May 2019 have been listed as "Major Seismic Activities" in monthly "Evaluation of Seismic Activities."

  – 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)
  – Middle and Eastern Iburi Regions *  M6.7 on September 6, 2018
(Depth of approximately 35 km)
  – Middle and Eastern Iburi Regions *  M5.2 on October 5, 2018
(Depth of approximately 30 km)
  – Kumamoto Region, Kumamoto Prefecture  M5.1 on January 3, 2019
(Depth of approximately 10 km)
   M4.3 on January 26, 2019
(Depth of approximately 10 km)
  – Middle and Eastern Iburi Regions *  M5.8 on February 21, 2019
(Depth of approximately 35 km)
  – Northern Hyuganada  M6.3 on May 10, 2019
(Depth of approximately 25 km)
  – Northeastern Chiba Prefecture  M5.1 on May 25, 2019
(Depth of approximately 40 km)
  * Seismic activity of the 2018 Hokkaido Eastern Iburi Earthquake

   

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-Chubu region.

(4) Kinki-Chugoku-Shikoku Region

– According to the GNSS observation in the northern Kyushu from 2018 spring, and according to the GNSS and strain observations in the western Shikoku from 2018 autumn, crustal deformations different from the ordinary trend have been observed. These phenomena are considered to be caused by a slow slip at the deeper part of the boundary between the Philippine Sea and the continental plates, which continues at the northern Hyuganada and around the Bungo Channel.

(5) Kyushu-Okinawa Region

There is no supplementary information for Kyushu-Okinawa region.

(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 July 5 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, July 5, 2019)
"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)