2022/02/27 09:41 Weathernews
Earthquakes on the Pacific side from Kanto to northern Japan and around Okinawa are conspicuous. There are two earthquakes with a seismic intensity of 3 or higher during this period. (Aggregation from February 21st to 27th at 10:00)
Domestic: Earthquake at a depth of 350km in Enshu-nada Epicenter distribution in anomalous seismic area
In the Tokai region near the epicenter, there were no tremors with a seismic intensity of 1 or higher, but there were many places where tremors were observed in the northeastern Kanto region and Fukushima prefecture, which are far from the epicenter. The maximum seismic intensity of 2 was in Namie Town, Fukushima Prefecture and Utsunomiya City, Tochigi Prefecture.
It is a phenomenon that occurs when shaking is transmitted to a distant area along the Pacific plate where seismic waves are easily transmitted in the epicenter distribution called anomalous seismic area. Although named “abnormal,” it is often seen during deep-focus earthquakes.
* The epicenter was off the southeastern coast of Mie prefecture in the preliminary figures, but it has been changed to Enshu-nada in the provisional values.
Many deep-focus earthquakes have occurred in the past
The assumed “Nankai Trough giant earthquake” is an earthquake that occurs near the boundary where the Philippine Sea plate subducts into the Eurasian plate, and the depth of the epicenter is said to be about 10 to 40 km. The mechanism of this earthquake is a different factor from the Nankai Trough giant earthquake.
World: M6.2 human damage in Indonesia
An earthquake with a magnitude of 6.2 and an estimated depth of about 12 km occurred on Sumatra Island, Indonesia on the morning of the 25th (Friday) of Japan time. The mechanism of the earthquake is analyzed as a strike-slip type.
In the vicinity of the epicenter, the revised Mercalli Intensity Class VI-VII was hit by strong shaking, causing damage such as the collapse of the building. According to the Indonesian National Disaster Management Agency, eight people were killed and nearly 100 were injured in the earthquake.
Damage caused by a huge earthquake at the plate boundary is conspicuous around Sumatra Island, but inland earthquakes like this one sometimes occur. In the immediate vicinity of this epicenter, there was a magnitude 6.6 earthquake in 1977. Most of the earthquakes are not so large with a magnitude of 6 units, but since the epicenter is shallow, the shaking around them is large, which leads to damage.
Reference materials, etc.
* Information on the epicenter and seismic intensity in Japan is from the Japan Meteorological Agency unless otherwise stated. Information on overseas epicenters is from the United States Geological Survey (USGS) unless otherwise stated. The epicenter information may differ depending on the issuing organization.