Tamagawa

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

1 300 m

Poloha

39,897°, 140,781°

The dacitic and rhyolitic Tamagawa caldera was the source of the Tamagawa Ignimbrite associated with formation of a pre-Yaka-yama caldera. The caldera was active about 2 million and 1 million years ago (Nakano et al., 2001-).

Text: Smithsonian Global Volcanism Program.

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