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Japón · Estratovolcán

Akusekijima

Tipo
Estratovolcán
Altitud
555 m
Última erupción
Desconocido
Akusekijima
Foto: 名古屋太郎 · CC BY-SA 3.0 · Wikimedia Commons
Tipo
Estratovolcán
País
Japón
Región
Pacífico Occidental / Ryukyu Volcanic Arc
Altitud
555 m
Coordenadas
29.465, 129.594
Última erupción
Desconocido
Contexto tectónico
Zona de subducción / Corteza oceánica (< 15 km)
Forma volcánica
Compuesto
Roca principal
Andesita / Andesita basáltica
Resumen geológico

Akusekijima is a small stratovolcano in the southern Ryukyu Islands. Most of the island is surrounded by steep cliffs, and beaches are found only on the SW and SE sides. The andesitic-dacitic volcano consists of two older somma volcanoes, Biroyama and Nakadake. Mitake lava dome forms the high point of the small 2.5 x 3.2 km wide island. The dacitic Omune lava flow on the NE flank was K-Ar dated at less than 80,000 BP; its youthful morphology and lack of overlying tephra layers suggests it could be as young as the Holocene (Furuyama et al., 2002). The lava flow, the youngest product of the volcano, forms a low-angle plateau overlying cliffs forming the northern coast.

Resumen de Wikipedia

Resumen en inglés

Akusekijima is one of the Tokara Islands, a subgroup of the Satsunan Islands belonging to Kagoshima Prefecture, Japan. The island, 7.42 km² in area, has a population of 59 persons. The island can only be reached by boat, as it has no airport; there is a ferry service twice per week to the city of Kagoshima on the mainland. Travel time is about 11 hours. The islanders are dependent mainly on fishing and seasonal tourism.

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