Source:New Report Identifies Risks of an M8 Class Quake in Seas Around
Western Japan
For the first time, Japan’s earthquake also took a long-term look at risks from active faults below the
seabed in the southwestern part of the Sea of Japan.
A new report by the government’s Earthquake Research Committee lays out the risks of an M8 earthquake
on the Richter scale in Japan’s Hyuganada Sea and Nansei Islands.
Nankai Trough, the presumed epicenter of the earthquake, runs about 200 km or 130 miles off the east
coast of Shikoku Island and stretches along the eastern side of southwest Japan. The March 25 report
indicates a broad portion of this area, area including the Hyuganada Sea and Nansei Islands chain in
southwestern Japan, are at risk of damage from both earthquake and tsunamis.
Learning from the Great East Japan Quake
The report does not analyze the risks in other regions of Japan, including the Fukushima area, which
experienced a jarring M7.4 quake off its coast on March 17, 2022.
When the committee first issued a long-term earthquake evaluation for Japan’s southwestern region in
2004, the expert panel had not identified a probability of a quake as large as an M8 magnitude on the
Richter scale. Although the 2011 Great East Japan Earthquake falls outside the study’s regional scope,
the committee has revised its review based on the latest findings of that event.
Areas of Focus
The report identifies three new risk areas for megathrust earthquakes of at least M8.
A long-term evaluation of active faults below the seabed in the southwestern part of the Sea of Japan
for the first time for the 2022 report. The analysis indicates an 8-13% chance of a powerful earthquake
with
a probability of M7 or more occurring over the next 30 years on some of these active undersea faults.
This
is a very high probability for an active fault-triggered temblor.
The area off the Hyuganada Sea east of Kyushu is also at risk, as is the region extending from the
Nansei Island chain to around Yonaguni Island in the far western part of Japan. It is assumed there have
been
earthquakes in the area in the past, the lack of data makes it difficult to estimate the likelihood in
these areas.
A megathrust quake in the M8.5 range is thought to be possible in the Yaeyama Islands (near Ishigaki
Island, Okinawa Prefecture), which suffered a similar earthquake and tsunami that hit the region in
1771. The destruction from that event extended to Yonaguni Island. While the possibility of this type of
event
is in the report, it is excluded from the probabilities assessment because there are too many
unknowns.
Analyzing the Risks
The committee’s long-term projections are intended to forecast the likelihood and scale of earthquakes
occurring either at boundary zones of tectonic plates that cover the Earth or an active fault. A
megathrust
quake occurs when one tectonic plate is pushing under another, and a sudden slippage occurs. These
points are called subduction zones.
Dr. Naoshi Hirata, chairman of the committee and Professor Emeritus at the University of Tokyo’s
Institute
for Earthquake Research said, “It is highly probable that an M8 or stronger quake has occurred in the
past,
and we believe it necessary to assume a similar one will happen in the future.”
According to the committee, chances are greater than 90% within the next 30 years that a major quake of
a M7 to 7.5 will strike in waters off Yonaguni Island. Moreover, the report predicts an 80% chance of
one
of that magnitude happening in the Hyuganada Sea. A major earthquake is also thought possible in the
waters off the Nansei Islands, although there is insufficient data to calculate the likelihood.
The report considers deep-focus, megathrust earthquakes likely to happen in undersea subduction zones,
where one tectonic plate moves under another. It predicts an M6.7-7.4 quake of this type hitting between
Honshu and Shikoku in the oceanic region within the Akinada Sea and Iyonada Sea in the larger Seto
Inland
Sea, and stretching northeast to the Bungo Channel between Shikoku and Kyushu.
The chance drops slightly to around 60% in the northwestern waters off the Nansei Islands.
Overview along the Sea of Japan
Looking at the active undersea faults in the southwestern part of the Sea of Japan off Tottori
Prefecture
and Nagasaki Prefecture, the committee divided the quake-prone region into three areas. There is a 3-7%
risk in the east, 3-6% risk in the central area, and 1-3% risk in the west of an M7 earthquake occurring
within the next 30 years.
The committee has put the quake likelihood for the three areas as a whole at 8-13%, but identifies the
largest fault belt beneath the seabed off the Hoki region of Tottori Prefecture is at risk of a M7.7-8.1
earthquake in that time frame. Fault line in the area extend for an estimated 94 kilometers.
“Given that quakes triggered by active faults are considered striking at an interval of several thousand
years, the occurrence probabilities of those are all significantly high,” Professor Hirata
noted,
Major earthquakes with undersea epicenters often cause massive tsunamis. The committee plans to
expand its analysis to include tsunami-related predictions such as maximum wave height based on the
magnitudes of earthquakes assessed in this latest long-term evaluation report.
南海トラフ巨大地震の想定震源域に隣接する日向灘や南西諸島などで、マグニチュード(M)8級の巨大地震が起き得
るとする新たな長期評価を、政府の地震調査委員会が25日、公表した。平成16年に初公表した同地域の長期評価は
M8級を想定しなかったが、23年の東日本大震災を受け最新の知見で見直した。また日本海南西部の海底活断層の
長期評価も初めて行い、30年以内にM7以上の地震が起きる確率を、活断層としては高い8~13%とした。
長期評価は、地球を覆うプレート(岩板)の境界や活断層で起きる地震の規模や発生確率を予測する。新たに想定され
た巨大地震は三つで、このうち二つは日向灘と、南西諸島周辺から与那国島周辺にかけてで起きるM8程度。過去にも
起きた可能性が高いことなどから想定されたが、データ不足で確率は不明とした。
もう一つは、1771年に与那国島を含む八重山列島を大津波が襲った八重山地震津波のようなM8・5程度のタイプ。
こちらも発生の可能性は認めたが、不明点が多いことから確率評価の対象外となった。
地震調査委の平田直委員長(東京大名誉教授)は「M8級は過去に発生した可能性が高く、将来も起き得るという考え
方で想定した」と語り、警戒を呼び掛けた。
このほか、M7~7・5程度の大地震の発生確率は与那国島周辺で30年以内に90%程度以上、日向灘で80%程度、
南西諸島周辺でも確率は不明だが発生し得るとした。また、陸側プレートの下に沈み込む海側プレートの内部で起きる
やや深い地震は、M6・7~7・4程度が安芸灘から伊予灘、豊後水道にかけてで40%程度、M7~7・5程度が九州中
央部(確率不明)と南西諸島北西沖(60%程度)でそれぞれ起き得ると評価した。
一方、鳥取県-長崎県沖の日本海南西部の海底活断層については三つの領域に分け、30年以内のM7以上の地震
の発生確率は、東部3~7%、中部3~6%、西部1~3%。全体は8~13%とした。領域最大の活断層で、東部にある
全長94キロ程度の伯耆(ほうき)沖断層帯ではM7・7~8・1程度が起きると評価。「活動間隔が数千年以上となる活断
層の地震としては、いずれも高い発生確率と受け止めてほしい」(平田氏)という。
海域が震源の大きな地震は津波を伴うことが多い。今後は今回の長期評価で想定された地震の規模などにに基づき、
津波の高さなどについても予測していく。