Japan · Caldera
Kikai Caldera
Kikai
- Type
- Caldera
- Elevation
- 704m
- Last eruption
- 2025

- Type
- Caldera
- Country
- Japan
- Region
- Western Pacific / Ryukyu Volcanic Arc
- Elevation
- 704m
- Coordinates
- 30.793, 130.305
- Last eruption
- 2025
- Tectonic setting
- Subduction zone / Oceanic crust (< 15 km)
- Landform
- Caldera
- Major rock type
- Rhyolite
Geological summary
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.
From Wikipedia
Kikai Caldera is a massive, mostly submerged caldera up to 19 kilometres (12 mi) in diameter in the Ōsumi Islands of Kagoshima Prefecture, Japan.
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Eruption history
30 recordedGlossaryDetailed timeline
- 2025VEI 1Observed2025-12-29 – 2025-12-29Iodake Crater
- 2024VEI 1Observed2024-09-01 – 2024-09-03Satsuma Iwo-jima (Iodake Crater)
- 2023VEI ?Observed2023-03-27 – 2023-07-31
- 2020VEI 1Observed2020-04-29 – 2020-04-29
- 2020VEI 1Observed2020-10-06 – 2020-10-06
- 2019VEI 2Observed2019-11-02 – 2019-11-02
- 2013VEI 1Observed2013-06-04 – 2013-06-04Iodake
- 2004VEI 2Observed2004-03-05 – 2004-10-16Iwo-dake
- 2003VEI 2Observed2003-02-16 – 2003-10-16Iwo-dake
- 2002VEI 2Observed2002-05-11 – 2002-07-16Iwo-dake
- 2000VEI 2Observed2000-01-16 – 2000-03-16Iwo-dake
- 2000VEI 1Observed2000-10-16 – 2001-12-16Iwo-dake
- 1998VEI 2Observed1998-04-25 – 1999-08-16Iwo-dake
- 1997VEI 1Observed1997-07-02 – end unknownIwo-dake
- 1988VEI 1Observed1988-01-18 – 1988-01-18Iwo-dake
- 1934VEI 2Observed1934-09-19 – 1935-08-162 km east of Tokara-Iwo-Jima
- 1914VEI ?Method not stated1914-02-13 – end unknownTokara-Iwo-jima
- 1430 (±75 yrs)VEI ?Geological estimate1430 – end unknownIwo-dake
- 1340 (±30 yrs)VEI ?Geological estimate1340 – end unknownIwo-dake
- 1030 (±40 yrs)VEI ?Geological estimate1030 – end unknownIwo-dake
- 1010 (±40 yrs)VEI ?Geological estimate1010 – end unknownIwo-dake
- 830 (±40 yrs)VEI ?Geological estimate830 – end unknownIwo-dake
- 750VEI 3Geological estimate750 – end unknownIwo-dake
- 390 (±100 yrs)VEI 3Geological estimate390 – end unknownIwo-dake
- 280 BCE (±75 yrs)VEI ?Geological estimate280 BCE – end unknownIwo-dake
- 1090 BCE (±100 yrs)VEI 2Geological estimate1090 BCE – end unknownInamura-dake
- 1830 BCE (±75 yrs)VEI ?Geological estimate1830 BCE – end unknownInamura-dake
- 2450 BCE (±840 yrs)VEI ?Geological estimate2450 BCE – end unknownOld Iwo-dake
- 3250 BCE (±75 yrs)VEI ?Geological estimate3250 BCE – end unknownOld Iwo-dake
- 4350 BCEVEI 7Geological estimate4350 BCE – end unknownKikai caldera
Nearby volcanoes
External links
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