The following are the numbers of earthquakes by magnitude
that occurred in Japan and the surrounding area during July 2006.
(reference) Average numbers of earthquake occurrences over
the past thirty years (1971 - 2000)
The following regions have been noted as having significant
seismic activity during the period from July 2005 to the end of June
2006.
|
- Northwestern Chiba
prefecture
|
M6.0 on
July 23, 2005(depth approximately 75km) |
|
- Off-shore of
Miyagi prefecture |
M7.2 on August
16, 2005
(depth approximately 40km) |
|
- Chuetsu
region, Niigata
prefecture |
M5.0 on August
21, 2005
(depth approximately 15km) |
|
- Off-shore of
Ibaraki prefecture |
M6.3 on October
19, 2005
(depth approximately 50km) |
|
- Off-shore of
Sanriku |
M7.2 on
November 15, 2005
|
|
- Hyuganada |
M5.5 on March
27, 2006 (depth approximately 35km)
|
|
- Off-shore
east of the Izu Peninsula |
seismic
activity with M5.8 on April 21,
and M4.5 on April 30, 2006 |
|
- Central Oita |
M6.2 on June
12, 2006
(depth approximately 150km) |
to the text
2 Nationwide Seismic Activity by Region
(1) Hokkaido Region
On July 17, there was a M4.0 earthquake at a depth of approximately 85km under central Tokachi subprefecture.":
In this vicinity, there was a M4.7 earthquake on June 13, 2006.
to the text
(2) Tohoku Region
On July 1, there was a M5.3 earthquake at a depth of approximately
40km off-shore of Miyagi prefecture. The focal mechanism showed a
reverse fault with a compression axis in a NW-SE direction. This event
occurred at the boundary between the Pacific and the continental
plates.":
This event occurred near the northern edge of the aftershock region of
the earthquake off-shore of Miyagi prefecture on August 16, 2005 (M7.2).
In this vicinity, there was a M6.1 earthquake on December 17, 2005.
to the text
(3) Kanto-Chubu Region
"On July 6, there was a M4.0 earthquake at a depth of
approximately 50km under southern Ibaraki prefecture.":
In this vicinity, there was a M3.9 earthquake (maximum seismic intensity 3) on July 30.
"The long-term changes that have been observed since 2001
in the continuous GPS data in the Tokai region, are thought to have
stopped already.":
(This evaluation is in agreement with the views presented at the procedural
meeting on July 31 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" (Japan Meteorological Agency, Department of Seismology and Volcanology, July 31, 2006)
" So far, there have been no changes of activity which are likely to
be associated with the so-called Tokai earthquake.
There was no remarkable seismic activity in general. The seismicity remains
at a level lower than normal directly under the area from eastern Hamana
Lake through central Shizuoka prefecture. In other regions, seismic activity
is generally at a normal level.
The long-term crustal movements from the slow slip at the plate boundary
in the Tokai region and its neighboring area, are thought to have stopped
already. "
There was additional activity in the Kanto - Chubu region, as follows.
- On July 9, there was a M4.2 earthquake at a depth of approximately 25km
under Tokyo Bay (maximum seismic intensity 3).
- On July 9, there was a M4.8 earthquake at a depth of approximately 10km
under the ocean area near Niijima and Kozushima Islands (maximum seismic
intensity 4).
to the text
(4) Kinki-Chugoku-Shikoku Region
There is no supplementary information for the Kinki - Chugoku - Shikoku
region.
to the text
(5) Kyushu-Okinawa Region
There is no supplementary information for the Kyushu - Okinawa region.
to the text
Reference 1
Earthquakes that are described in the "Evaluation of Seismic
Activity"(Monthly Report of Seismic Activity in Japan) are events of
M6.0 and greater, or events of M4.0 and greater (M5.0 or greater
off-shore) that have maximum intensity of 3 or greater.
Reference 2
Information that is described in the "Supplementary Information to the
Evaluation" includes:
1) |
Reference information
related
to 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. |
|