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Another official source, tweeted about half an hour ago -- no changes, as I understand it; basically, activity continues, including weak, moderate, and strong pyroclastic flows; watch, wait, be prepared.
...The coastal waters of the Tokara Islands are an area where swarms of earthquakes often occur. This is the first time since June 2024 that more than 10 perceptible earthquakes have been observed in a single day, when the largest earthquake was a magnitude 3.7 earthquake with a maximum seismic intensity of 3.
The activity in May 2023 was a maximum seismic intensity of 5-, and the activity in December 2021 was a maximum seismic intensity of 5-strong. In some cases, the earthquake-prone situation will continue for several weeks or more, so it will be necessary to keep an eye on developments for a while.
The amount of volcanic gas emitted from Shinmoedake in the Kirishima mountain range, which lies on the border between Kagoshima and Miyazaki prefectures, has increased sharply, and the Japan Meteorological Agency, citing further increased volcanic activity, issued a new crater area warning at 6:30 pm on the 23rd and raised the eruption alert level to 3.
It is calling for caution against large volcanic rocks and pyroclastic flows within a 3-kilometer radius of the crater...
-- Source (Japanese)
June 23, 2025, 9:39 p.m., Pacific: I had thought the Tokaras were south of Kikai — and some of them are — but it turns out that frequently active Satsuma volcano, on Kikai’s rim and not close to the probably tectonic seismic swarm, is one of them, and it emitted a white plume today.
Per the Global Volcanism Program Kikai page:
Multiple eruption centers have exhibited recent activity at Kikai, a mostly submerged, 19-km-wide caldera near the northern end of the Ryukyu Islands south of Kyushu. It was the source of one of the world’s largest Holocene eruptions about 6,300 years ago when rhyolitic pyroclastic flows traveled across the sea for a total distance of 100 km to southern Kyushu, and ashfall reached the northern Japanese island of Hokkaido. The eruption devastated southern and central Kyushu, which remained uninhabited for several centuries. Post-caldera eruptions formed Iodake (or Iwo-dake) lava dome and Inamuradake scoria cone, as well as submarine lava domes. Recorded eruptions have occurred at or near Satsuma-Iojima (also known as Tokara-Iojima), a small 3 x 6 km island forming part of the NW caldera rim. Showa-Iojima lava dome (also known as Iojima-Shinto), a small island 2 km E of Satsuma-Iojima, was formed during submarine eruptions in 1934 and 1935. Mild-to-moderate explosive eruptions have occurred during the past few decades from Iodake, a rhyolitic lava dome at the eastern end of Satsuma-Iojima.
Per the Japanese Meteorological Agency, via Volcano News:
Activities of Satsuma Iwo Jima
Crater Area Warning (Eruption Alert Level 2, Crater Area Restrictions)
Interpretive information on the status of the volcano
June 23, Reiwa 7, 16:00 Fukuoka Regional Meteorological Observatory / Kagoshima Regional Meteorological Observatory announcement
Status of volcanic activity
At Iwo-dake crater, a white plume rose up to 400 m above the crater rim.
At night, we occasionally observed the fire with high-sensitivity surveillance cameras.
Volcanic earthquakes have passed in a low number. No volcanic tremor was observed.
In the long term, there is a possibility that an eruption will occur to a degree that affects the area around the crater due to the continued state of increased thermal and plume activity, such as the observation of a fire at night and occasional high plumes.
If there is any connection between Satsuma’s plume/glow and the Tokara seismic swarm — a big and very unlikely “if” — it would probably be that Satsuma was getting ready for another eruption anyway and the shaking either has unsettled it or speeded up the process.
Still, the area is populated and popular with tourists, and Satsuma might go off, so I’ll pin this now — under “Tokara” NOT “Kikai” (which is a whole ‘nother and currently dormant thing). There is no need to mobilize the pop-music contingent.
June 22, 2025, 10:48 p.m., Pacific: Some technical (but unofficial) posts on X suggest to this layperson that the swarm is tectonic, including this one:
...
https://platform.twitter.com/widgets.jsイクスリップ型に近いが、最大のM5.2(22日17:15)とその前のM3.9は正断層型。共通するのは北西・南東伸長のメカニズム。M5.2の次の逆断層に見えるのはCMTの決め間違いかもしれない。 pic.twitter.com/Cdtsfo7F4N
— hacchan9642 (@hacchan9642) June 23, 2025
X translation (emphasis added): “F-net has found many CMT solutions for the earthquakes off the coast of the Tokara Islands, which continue to have a seismic intensity of 1 or higher. Many of them are close to strike-slip type, but the largest M5.2 (17:15 on the 22nd) and the previous M3.9 are normal fault types. What they have in common is a mechanism of northwest-southeast extension. What appears to be a reverse fault following the M5.2 may be a misdetermination of the CMT.”
Extension is something we’ve recently seen in another complicated tectonic setting loaded with volcanoes: the more powerful Amorgos seismic swarm near Santorini and Kolombo in the Aegean Sea
And it settled down without any associated eruption. Perhaps this latest round of Tokara Islands quakes will, too.
Experts analyzed the volcanic ash that fell during the eruption of Shinmoe-dake in the Kirishima Mountains on the 22nd and found that it contained almost no material related to new magma.
While experts said it was likely a "steam eruption," they also pointed out that it is necessary to keep a close eye on future developments...
-- Source (Japanese)