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Daisetsuzan Volcanic Group

Taisetsuzan

Stratovulcano · Japan · 2291 m

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. · Foto: Photo by Ichio Moriya, 1993 (Kanazawa University). · Wikimedia Commons
Tipo
Stratovulcano
Paese
Japan
Regione
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Altitudine
2291 m
Coordinate
43.664, 142.854
Ultima eruzione
1739
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

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.

Sintesi da Wikipedia

Riassunto in inglese

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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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
3200 BCE~3002 BCE · 1 eruzioni · VEI max. ?2805 BCE~2607 BCE · 1 eruzioni · VEI max. ?1620 BCE~1422 BCE · 1 eruzioni · VEI max. ?632 BCE~434 BCE · 1 eruzioni · VEI max. ?1541~1739 · 1 eruzioni · VEI max. ?3200 BCE2015 BCE829 BCE3561541

Cronologia dettagliata

  1. 1739VEI ?Stima geologica
    1739 – In corso
    Asahi-dake
  2. 550 a.C. (±500 anni)VEI ?Stima geologica
    BCE 550 – In corso
    Asahi-dake
  3. 1450 a.C. (±50 anni)VEI ?Stima geologica
    BCE 1450 – In corso
    Asahi-dake
  4. 2800 a.C. (±100 anni)VEI ?Stima geologica
    BCE 2800 – In corso
    Asahi-dake
  5. 3200 a.C. (±75 anni)VEI ?Stima geologica
    BCE 3200 – In corso
    Asahi-dake

Link esterni

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