Daisetsuzan Volcanic Group
Taisetsuzan
Stratovulcano · Japan · 2291 m

- Tipo
- Stratovulcano
- Paese
- Japan
- Regione
- Pacifico nord-occidentale / 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.
Storia delle eruzioni
Cronologia dettagliata
- 1739VEI ?Stima geologica1739 – In corsoAsahi-dake
- 550 a.C. (±500 anni)VEI ?Stima geologicaBCE 550 – In corsoAsahi-dake
- 1450 a.C. (±50 anni)VEI ?Stima geologicaBCE 1450 – In corsoAsahi-dake
- 2800 a.C. (±100 anni)VEI ?Stima geologicaBCE 2800 – In corsoAsahi-dake
- 3200 a.C. (±75 anni)VEI ?Stima geologicaBCE 3200 – In corsoAsahi-dake
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.