Tokachi-Mitsumata

sopka (bez známé erupce za posledních ~12 000 let), Japan, Northwestern Pacific Volcanic Regions

Kde

Japan, Northwestern Pacific Volcanic Regions

Typ (GVP)

Caldera

Nadmořská výška

700 m

Poloha

43,520°, 143,150°

Tokachi-Mitsumata, a rhyolitic caldera that was the source of the Muka and Meto pyroclastic flows, was active about 0.6-0.3 million years ago (Nakano et al., 2001-). Ishii et al. (2008) listed dates of around 1 million years ago for formation of the Tokachi-Mitsumata caldera.

Text: Smithsonian Global Volcanism Program.

Údaje o sopce: Smithsonian Global Volcanism Program. Další sopky a průduchy.