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Japón · Caldera

Hijiori

Tipo
Caldera
Altitud
552 m
Última erupción
Desconocido
Hijiori volcano, seen from the E, is a small caldera located NE of the Pleistocene Gassan volcano. The town of Hijiori lies in the left foreground along the banks of two rivers through the caldera floor. The low 2.5-km-wide caldera formed during a large eruption between about 9,500 and 11,000 years ago, accompanied by pyroclastic flows and ashfall that extended to the E and reached the Pacific coast.
Hijiori volcano, seen from the E, is a small caldera located NE of the Pleistocene Gassan volcano. The town of Hijiori lies in the left foreground along the banks of two rivers through the caldera floor. The low 2.5-km-wide caldera formed during a large eruption between about 9,500 and 11,000 years ago, accompanied by pyroclastic flows and ashfall that extended to the E and reached the Pacific coast. · Foto: Copyrighted photo by Hiroshi Yagi (Japanese Quaternary Volcanoes database, RIODB, http://riodb02.ibase.aist.go.jp/strata/VOL_JP/EN/index.htm and Geol Surv Japan, AIST, http://www.gsj.jp/).
Tipo
Caldera
País
Japón
Región
Pacífico Noroccidental / Northeast Japan Volcanic Arc
Altitud
552 m
Coordenadas
38.599, 140.162
Última erupción
Desconocido
Contexto tectónico
Zona de subducción / Corteza continental (> 25 km)
Forma volcánica
Caldera
Roca principal
Dacita

Resumen geológico

Original en inglés

Hijiori caldera is a small, inconspicuous caldera located NE of the Pleistocene Gassan stratovolcano.

Extracto del Global Volcanism Program, Smithsonian Institution · Leer el resumen completo en el GVP →

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⚠ Solo como referencia. No apto para respuesta ante emergencias.