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Daisetsuzan Volcanic Group

Taisetsuzan

Stratovolcano · Japan · 2291m

Geothermal activity and recent craters occupy the western slope of Asahidake, one of the Daisetsu group volcanoes in central Hokkaido. Taisetsuzan is a complex group of cones and lava domes associated with a 2-km-wide caldera. Asahidake, the highest peak of the complex, was constructed 3 km SW from the caldera center.
Geothermal activity and recent craters occupy the western slope of Asahidake, one of the Daisetsu group volcanoes in central Hokkaido. Taisetsuzan is a complex group of cones and lava domes associated with a 2-km-wide caldera. Asahidake, the highest peak of the complex, was constructed 3 km SW from the caldera center. · Photo: Photo by Ichio Moriya, 1993 (Kanazawa University). · Wikimedia Commons
Type
Stratovolcano
Country
Japan
Region
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Elevation
2291m
Coordinates
43.664, 142.854
Last eruption
1739
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Andesite / Basaltic Andesite
Geological summary

The Taisetsuzan volcano group lies at the northern end of the Taisetsu-Tokachi graben in central Hokkaido. It consists of a complex of stratovolcanoes and lava domes associated with a 2-km-wide caldera. The eight satellitic volcanoes are aligned along a ring fracture that is centered over the eastern rim of the caldera. Asahidake, the highest peak of the complex, was constructed 3 km SW of the center of the caldera. Other stratovolcanoes are located along a NE-SW line cutting through the caldera that trends toward the Tokachi volcano complex to the SW. In contrast to the Tokachi group, no historical eruptions are known, although the latest phreatic eruption took place sometime after 1739 CE. Fumarolic areas are located on Asahidake, where at one time sulfur was mined, and in the caldera.

From Wikipedia

The Daisetsuzan Volcanic Group is a volcanic group of peaks arranged around the 2 kilometres (1.2 mi) wide Ohachi-Daira caldera in Hokkaidō, Japan. In the Ainu language it is known as Nutapukaushipe, Nutaku Kamushupe, or Optateske. These peaks are the highest in Hokkaidō. The group lends its name to the Daisetsuzan National Park in which the volcanic group is located.

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Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
3200 BCE~3002 BCE · 1 eruptions · max VEI ?2805 BCE~2607 BCE · 1 eruptions · max VEI ?1620 BCE~1422 BCE · 1 eruptions · max VEI ?632 BCE~434 BCE · 1 eruptions · max VEI ?1541~1739 · 1 eruptions · max VEI ?3200 BCE2015 BCE829 BCE3561541

Detailed timeline

  1. 1739VEI ?Geological estimate
    1739 – Ongoing
    Asahi-dake
  2. 550 BCE (±500 yrs)VEI ?Geological estimate
    BCE 550 – Ongoing
    Asahi-dake
  3. 1450 BCE (±50 yrs)VEI ?Geological estimate
    BCE 1450 – Ongoing
    Asahi-dake
  4. 2800 BCE (±100 yrs)VEI ?Geological estimate
    BCE 2800 – Ongoing
    Asahi-dake
  5. 3200 BCE (±75 yrs)VEI ?Geological estimate
    BCE 3200 – Ongoing
    Asahi-dake

External links

⚠ For reference only. Not for emergency response.