Kuju Volcano
Updated: 19. Apr. 2024 12:50 GMT -
stratovolcanoes 1791 m / 5,876 ft
Kyushu, Japan, 33.08°N / 131.25°E
Aktueller Status: normal / ruhend (1 von 5)
Kyushu, Japan, 33.08°N / 131.25°E
Aktueller Status: normal / ruhend (1 von 5)
Kuju (or Kujusan) volcano is a group of active stratovolcanoes and lava domes in the northeastern corner of the large Aso caldera in central Kyushu, Japan.
Its historic eruptions recorded in the 17th and 18th century and as recently as 1995 were phreatic or hydrothermal explosions, caused by overheated ground water. The latest eruption where magma arrived at the surface was about 1600 years ago and formed Kuro-dake lava dome at the eastern end of the complex.
Kuju contains many hot springs and hydrothermal fields and there are 2 geothermal power plants. A particularly active hydrothermal area is Iwoyama on the NE flank of Hossho-zan lava dome, where a fumarole field was mined for sulfur during over 500 years.
Recent studies suggest that Kuju should be considered one of the more hazardous volcanoes in Japan because of its history of producing pyroclastic flows from lava dome collapse.
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Ausbrüche des Kuju: 1995-96, 1738 (?), 1675, 1662, 370 AD ± 40 years (radiocarbon-dated)
Letzte Erdbeben in der Nähe
| Uhrzeit | Mag. / Tiefe | Entfernung / Ort | |||
Beschreibung
The Kuju volcano group consists of 16 andesitic lava domes, 5 andesitic stratovolcanoes, and 1 basaltic cone. Activity at the Kuju group dates back to about 150,000 years. 6 major andesitic-to-dacitic tephra deposits, many associated with the growth of lava domes, have been recorded during the Holocene. Eruptive activity has migrated systematically eastward during the past 5000 years.Volcanic Hazards from Kuju volcano
Kuju volcano has had a near constant eruption rate (0.7–0.4 km3 / 1000 years) over the past 15,000 years, a value comparable to the other volcanoes of the Japanese Arc. It has produced lava domes and associated block and ash flows at roughly 1000 year intervals during the past 5000 years.
The vents from Kuju volcano have migrated systematically eastward in this interval, from the Iwaigodake-Hizengajo domes (5000 years ago), to Danbaru cone (4-5000 years ago), Komekubo crater (2-4000 years ago), and the Kurotake dome (ca. 1600 years ago), the so far latest in the series. The last one, similar to previous eruptions, produced about 1.6 km3 of andesite lava and forming a lava dome, which triggered large block-and-ash flows. This suggests the next magmatic eruption may occur around or east of Kurotake.
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Sources:
- Smithsonian / GVP volcano information
- Kamata, H., Kobayashi, T. (1997) "The eruptive rate and history of Kuju volcano in Japan during the past 15,000 years", Journal of Volcanology and Geothermal Research, v 76 (1-2), pp 163-171
Ausbrüche des Vulkans Kuju
1995 phreatic eruption & seismic unrest
A phreatic eruption began at Kuju volcano on 11 October 1995. 1 month earlier, steam had been detected rising 400 m from a fumarole area on the eastern slope of the Honsho lava dome. There had been 3 vents and fissures in an area about 300 m E-W by 100 m N-S wide.
"Smoke" was seen in the Kuju area around 6pm on 11 October 1995, when the eruption had started. Ash fell as far as 60 km. The eruption came from the same area observed previously, where several vents along a 300 m long fissure had opened.
Vigorous steaming was observed on 12 and 13 November field observers. Another ash eruption occurred on 18 December. Investigations showed that the erupted ash contained about 1% of juvenile rhyolite lava, suggesting that a shallow intrusion had taken place and almost reached the surface.
The eruptions ceased, but intense steaming continued. In addition, tens of thousands of earthquakes were detected over the following 2 years. In January 1996 alone, 861 earthquakes occurred, some of which could be felt. They were horizontally concentrated north of the new vents at depths between 1000 m below sea and 800 m above sea level.
On 10 January 1997, activity peaked with a high of 1,262 earthquakes in a single day and the steam plume reached 700 m height.
The activity started to slowly decrease after 1997. Interesting deformation measurements indicated that the Iwoyama fumarolic area near the summit of Honsho has been steadily deflating over more than 6 years after the eruption.
Sources:
- Smithsonian / GVP monthly reports
- Nakaboh et al (2003) "Continuing deflation by fumaroles at Kuju Volcano, Japan", Geophysical Res. Letters, v. 30 (0), pp.1-5
A phreatic eruption began at Kuju volcano on 11 October 1995. 1 month earlier, steam had been detected rising 400 m from a fumarole area on the eastern slope of the Honsho lava dome. There had been 3 vents and fissures in an area about 300 m E-W by 100 m N-S wide.
"Smoke" was seen in the Kuju area around 6pm on 11 October 1995, when the eruption had started. Ash fell as far as 60 km. The eruption came from the same area observed previously, where several vents along a 300 m long fissure had opened.
Vigorous steaming was observed on 12 and 13 November field observers. Another ash eruption occurred on 18 December. Investigations showed that the erupted ash contained about 1% of juvenile rhyolite lava, suggesting that a shallow intrusion had taken place and almost reached the surface.
The eruptions ceased, but intense steaming continued. In addition, tens of thousands of earthquakes were detected over the following 2 years. In January 1996 alone, 861 earthquakes occurred, some of which could be felt. They were horizontally concentrated north of the new vents at depths between 1000 m below sea and 800 m above sea level.
On 10 January 1997, activity peaked with a high of 1,262 earthquakes in a single day and the steam plume reached 700 m height.
The activity started to slowly decrease after 1997. Interesting deformation measurements indicated that the Iwoyama fumarolic area near the summit of Honsho has been steadily deflating over more than 6 years after the eruption.
Sources:
- Smithsonian / GVP monthly reports
- Nakaboh et al (2003) "Continuing deflation by fumaroles at Kuju Volcano, Japan", Geophysical Res. Letters, v. 30 (0), pp.1-5
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