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01/24/2021 10:53 AM Weathernews
Last week, the number of earthquakes observed in Japan has been roughly the same as the week before. Two earthquakes with a seismic intensity of 3 or more occurred. Inland earthquakes are a bit more noticeable during this period. (Added from January 18 to January 24 at 10:00)
This is the second time a seismic intensity of 3 or more has been observed in Japan since the maximum seismic intensity of 4 was reached in the earthquake near Niijima and Kozushima that occurred on January 1, shortly after the start of the year.
The area in front of Fukushima prefecture is the area of the aftershock of the great earthquake that occurred in 2011, and it is an area with many earthquakes. In the second half of last year, the occurrence of strong shaking earthquakes has stabilized, and the seismic intensity of 3 or more is the first in about half a year since July 17. Even if the intervals between earthquakes increase slightly, they are only within the margin of error in terms of long-term activities, and there is no change in terms of areas where earthquakes are likely to occur.
Please be sure to prepare for an earthquake regularly.
The epicenter of this time is the active area of the Kumamoto earthquake of 2016, and the earthquake of seismic intensity of 3 or higher that occurred in this area has been since November 3 of last year. Overall activity has definitely stabilized and there was not a last earthquake in 2018 with a strong shaking with a seismic intensity of 4 or more.
A 7.0 magnitude earthquake struck southeast of the island of Mindanao in the Philippines on Thursday 21. Although the scale was large, there was no tsunami because the depth was just under 100 km. Also, the epicenter is relatively far from the ground and there is no damage or impacts from the earthquake.
The epicenter is the region where the Philippine Sea plate is subducting towards the Eurasian plate, and the earthquake mechanism is analyzed as a type of reverse fault with a pressure axis in the east-west direction. There are many plate boundary earthquakes, and in 1969 there is a record of a 7.6 magnitude earthquake about 50 km southwest of the epicenter.
The aftershocks occurred in the area on Friday the 22nd, but all were less than magnitude 5.
This area is the boundary between the Antarctic Plate and a small plate called the Scotia Plate, and sometimes large earthquakes occur. There was a 6.0 magnitude earthquake last November, and there is still a 7.0 magnitude earthquake in 1971.
* Information on the epicenter and seismic intensity in Japan comes from the Japan Meteorological Agency, unless otherwise noted. Information on overseas epicenters comes from the United States Geological Survey (USGS) unless otherwise noted. The epicenter information may differ depending on the issuing organization.