Saltar al contenido principal

Toshima (isla)

Toshima

Estratovolcán · Japan · 508 m

Steep cliffs up to 300-m-high surround the small island of Toshima. Toshimamura, the port village of the island, is to the far left in this view from the west. Toshima lies about 20 km W of the main volcanic front of the Izu-Marianas arc. Recent activity occurred between about 8,000 and 40,00 years ago.
Steep cliffs up to 300-m-high surround the small island of Toshima. Toshimamura, the port village of the island, is to the far left in this view from the west. Toshima lies about 20 km W of the main volcanic front of the Izu-Marianas arc. Recent activity occurred between about 8,000 and 40,00 years ago. · Foto: Copyrighted photo by Shun Nakano (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/). · Wikimedia Commons
Tipo
Estratovolcán
País
Japan
Región
Northwestern Pacific Volcanic Regions / Izu Volcanic Arc
Altitud
508 m
Coordenadas
34.520, 139.279
Última erupción
-4550
Contexto tectónico
Subduction zone / Oceanic crust (< 15 km)
Forma volcánica
Composite
Roca principal
Basalt / Picro-Basalt
Resumen geológico

The small 2 x 2.4 km island of Toshima is located in the northern Izu Islands south of Izu-Oshima Island about 20 km W of the main volcanic front. Steep cliffs up to 300 m high ring the basaltic to basaltic andesite island on three sides. The summit is asymmetrically located opposite the more gentle slopes of the northern side of the island, where the village of Toshima is located. The latest known eruption of this stratovolcano occurred sometime between about 9,000 and 4,000 years ago, producing a lava flow from Kajiana crater.

Resumen de Wikipedia

Toshima es una isla volcánica ubicada en las islas Izu (伊豆諸島), el cual se encuentra al sur de Tokio y al este de la península de Izu, en la prefectura de Shizuoka. Toshima forma parte del parque nacional Fuji-Hakone-Izu. Administrativamente comprende la villa de Toshima , como parte de Tokio.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
4550 BCE~4550 BCE · 1 erupciones · VEI máx. 04550 BCE4550 BCE4549 BCE4549 BCE4549 BCE

Línea de tiempo detallada

  1. 4550 a. C. (±2550 años)VEI 0Estimación geológica
    BCE 4550 – En curso
    Kajiana crater

Enlaces externos

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