2022/10/02 10:09 Weather News
Earthquakes with epicenters in inland Hokkaido are somewhat conspicuous. There are many earthquakes as usual from the Kanto region to the southern Tohoku region. There were four earthquakes with a seismic intensity of 3 or higher. (September 26th to October 2nd at 10:00)
Japan: Seismic intensity 5 lower in Miyazaki Prefecture Widespread tremors in western Japan
This is the first time that a seismic intensity of 5-lower or higher has been observed in Miyazaki Prefecture since the Hyuga-nada earthquake on January 22nd (magnitude 6.6, maximum seismic intensity 5-upper). The mechanism of the earthquake is analyzed as a reverse fault type with a pressure axis in the northwest-southeast direction.
This is the 13th earthquake with a seismic intensity of 5 lower or more that has occurred in Japan this year.
Occurs near plate boundaries?
This is the first time since 1919, when the Japan Meteorological Agency has detailed statistics, that an earthquake with an epicenter off the east coast of the Osumi Peninsula recorded a seismic intensity of 5 Lower or higher. However, due to the fact that there were few observation points in the past, earthquakes with a magnitude of 6 or more, which are larger than this time, often occur.
In 1948, an earthquake with a magnitude of 6.4 occurred near this epicenter, and a seismic intensity of 4 was observed in Miyazaki City and Kumamoto City.
Looking at the distribution of past hypocenters, in this region, earthquakes were concentrated at depths of 20 to 30 km, which corresponded to the plate boundaries, and deeper.
Japan: Earthquake in the Abashiri region with a seismic intensity of 3
This is the first time since April last year that an earthquake with a seismic intensity of 3 or higher centered in the Abashiri region. There are not many strong earthquakes with epicenters on land in the Abashiri region, except for an earthquake with a magnitude of 5.0 and a maximum seismic intensity of lower 5 in 2015 along the mountains near Lake Akan, south of this epicenter.
There have been earthquakes as large as M6.0 in the past.
Most of the earthquakes are concentrated at a depth of around 10 km even in the depth of the east-west cross section. There are few occurrences at depths of 20 km or more, but there are a few at depths of 100 km or more. Earthquakes that occur near the boundary between the Pacific plate and the Eurasian plate or within the Pacific plate.
Most deep earthquakes are around magnitude 4, but in May 2014, a large earthquake with a magnitude of 6.0 occurred. In this earthquake, a maximum seismic intensity of 5 lower was observed in Chiyoda Ward, Tokyo, and a seismic intensity of 3 to 4 was observed in a wide area of the Kanto region, causing damage such as injuries.
World: Earthquakes frequently occur at the Reykjanes Ridge in the Atlantic Ocean
On the morning of Saturday, October 1, Japan time, an earthquake estimated to have a magnitude of 6.0 and a depth of regarding 10 km occurred near the Reykjanes Ridge in the Atlantic Ocean. The mechanism of the earthquake is analyzed as a reverse fault type with a pressure axis in the east-west direction.
Earthquakes have been occurring frequently around the epicenter since around September 26 (Monday). It is a situation where a rather strong earthquake such as magnitude 5.7 is occurring.
The Reykjanes Ridge is part of the Mid-Atlantic Ridge, which runs through the Atlantic from north to south, and is the boundary between the Eurasian and North American continents. The epicenters are distributed east and west across the ridge, and not only reverse-fault earthquakes but also normal-fault earthquakes have occurred.
Most of the large earthquakes that occur at the ridge are of the strike-slip type around the transform fault that develops in the surrounding area, and in 2015 an earthquake of magnitude 7.1 occurred. There are no records of earthquakes exceeding magnitude 6 in the vicinity of this epicenter, so future activity is attracting attention.
Magnitude 6.5 earthquake hits southern Taiwan
The earthquake mechanism is analyzed as strike-slip type.
Aftershocks followed one following another, and an earthquake of magnitude 5.5 occurred regarding an hour following the first one. There are concerns regarding damage due to strong tremors around the epicenter.
Reference materials, etc.
*Information on earthquake sources and seismic intensity in Japan is from the Japan Meteorological Agency unless otherwise specified. Overseas epicenter information is from the United States Geological Survey (USGS) unless otherwise specified. There may be differences in hypocenter information depending on the publishing organization.