December 10, 2009
Earthquake Research Committee,
Headquarters for Earthquake Research Promotion
There was no remarkable activity.
* On November 24, there was a M5.0 earthquake off-shore east of Hokkaido. The focal mechanism showed a reverse fault with a compression axis in a NW-SE direction.
* On November 21, there was a M4.5 earthquake at a depth of approximately 10km near the border between Fukushima and Tochigi prefectures [in northern Tochigi prefecture].
* On November 4, there was a M5.6 earthquake off-shore west of the Ogasawara Islands [under the ocean area near Chichijima].
* There have been no anomalous changes observed in the GPS data for the Tokai region.
There was no remarkable activity.
There was no remarkable activity.
[ ] were the regional names of the epicenters used in the Japan Meteorological Agency announcement.
December 10, 2009
The following are the numbers of earthquakes by magnitude that occurred in Japan and the surrounding area during November 2009.
(reference)
The following regions have been noted as having major seismic activity during the period from November 2008 to the end of October 2009.
– Under Suruga Bay | M6.5 on August 11, 2009 (depth of approximately 25km) | |
– Off-shore East of Hachijojima | M6.6 on August 13, 2009 | |
– Under the Ocean Area near Ishigakijima | M6.7, M6.6 on August 17, 2009 |
– On November 19, there was a M4.2 earthquake at a depth of 5km in the Kitami region, Abashiri subprefecture.
There is no supplementary information for the Tohoku region.
"There have been no anomalous changes observed in the GPS data for the Tokai region.":
(This evaluation is in agreement with the views presented at the procedural meeting on November 30 of the Assessment Committee for Areas under Intensified Measures against Earthquake Disaster. (see reference below))
(reference) "Recent seismic and crustal activity in the Tokai region and its vicinity" (Seismological and Volcanological Department, Japan Meteorological Agency, November 30, 2009)
"So far, there have been no changes of activity which are likely to be associated with the so-called Tokai earthquake.
1. Status of seismicity
The aftershock activity of the earthquake under Suruga Bay on August 11, has been subsiding.
Within the crust under mid-western Shizuoka prefecture, general seismicity has been slightly strong since mid-2005.
There continue to be fewer events within the Philippine Sea plate under the region around Hamana lake.
In other regions, seismic activity is generally at a normal level.
2. Status of crustal movements
There have been no remarkable changes observed over the entire region.
According to the GPS data and leveling results, the trend of long-term subsidence at Omaezaki has been continuing as before."
– On November 22, there were two M3.7 earthquakes at a depth of 10km in the Reinan region, Fukui prefecture. Both focal mechanisms showed reverse faults with compression axes in an E-W direction. These events occurred within the curst.
There is no supplementary information for the Kinki - Chugoku - Shikoku region.
There is no supplementary information for the Kyushu - Okinawa region.
Reference 1
Earthquakes that are described in the "Evaluation of Seismic Activity" (Monthly Report of Seismic Activity in Japan) have the following features.
Reference 2
Information that is described in the "Supplementary Information to the Evaluation" includes: