Daisetsuzan Volcanic Group
Taisetsuzan
Stratovolcano · Japan · 2291m

- 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
Detailed timeline
- 1739VEI ?Geological estimate1739 – OngoingAsahi-dake
- 550 BCE (±500 yrs)VEI ?Geological estimateBCE 550 – OngoingAsahi-dake
- 1450 BCE (±50 yrs)VEI ?Geological estimateBCE 1450 – OngoingAsahi-dake
- 2800 BCE (±100 yrs)VEI ?Geological estimateBCE 2800 – OngoingAsahi-dake
- 3200 BCE (±75 yrs)VEI ?Geological estimateBCE 3200 – OngoingAsahi-dake
External links
⚠ For reference only. Not for emergency response.