Mount Unzen
Unzendake
Complex volcano · Japan · 1483m

- Type
- Complex volcano
- Country
- Japan
- Region
- Western Pacific Volcanic Regions / Nankai Volcanic Arc
- Elevation
- 1483m
- Coordinates
- 32.761, 130.299
- Last eruption
- 1996
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
The massive Unzendake volcanic complex comprises much of the Shimabara Peninsula east of the city of Nagasaki. An E-W graben, 30-40 km long, extends across the peninsula. Three large stratovolcanoes with complex structures, Kinugasa on the north, Fugen-dake at the east-center, and Kusenbu on the south, form topographic highs on the broad peninsula. Fugendake and Mayuyama volcanoes in the east-central portion of the andesitic-to-dacitic volcanic complex have been active during the Holocene. The Mayuyama lava dome complex, located along the eastern coast west of Shimabara City, formed about 4000 years ago and was the source of a devastating 1792 CE debris avalanche and tsunami. Historical eruptive activity has been restricted to the summit and flanks of Fugendake. The latest activity during 1990-95 formed a lava dome at the summit, accompanied by pyroclastic flows that caused fatalities and damaged populated areas near Shimabara City.
From Wikipedia
Mount Unzen is an active stratovolcano of several overlapping small, volcanic cones, near the city of Shimabara, Nagasaki on the island of Kyushu, Japan's southernmost main island.
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Eruption history
Detailed timeline
- 1996VEI 2Observed1996-02-10 – 1996-05-01Fugen-dake
- 1990VEI 1Observed1990-11-17 – 1995-02-16Fugen-dake
- 1798VEI ?Geological estimate1798-11-13 – 1798-12Fugen-dake
- 1792VEI 2Observed1792-02-10 – 1792-07-22Fugen-dake (summit, NNE), Mayu-yama
- 1690VEI ?Geological estimate1690 – 1692
- 1663VEI 2Observed1663-04 – 1663-05Fugen-dake (Tsukumo-jima Pond)
- 1663VEI 2Observed1663-12-11 – 1663-12-27NE flank of Fugen-dake (1200 m)
- 860VEI ?Geological estimate860 – Ongoing
- 1150 BCE (±500 yrs)VEI ?Geological estimateBCE 1150 – OngoingFugendake-Sancho
- 1450 BCE (±500 yrs)VEI ?Geological estimateBCE 1450 – OngoingFugen-dake (Kazaana)
- 2150 BCE (±800 yrs)VEI ?Geological estimateBCE 2150 – OngoingMayu-yama (Tengu-yama)
- 2640 BCE (±500 yrs)VEI ?Geological estimateBCE 2640 – OngoingMayu-yama (Shichimen-zan)
- 2720 BCE (±300 yrs)VEI ?Geological estimateBCE 2720 – OngoingFugen-dake
- 4050 BCE (±3000 yrs)VEI ?Geological estimateBCE 4050 – OngoingFugen-dake (Shimanomine)
External links
⚠ For reference only. Not for emergency response.