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Japan · Stratovolcano

Akusekijima

Type
Stratovolcano
Elevation
555m
Last eruption
Unknown
Akusekijima
Photo: 名古屋太郎 · CC BY-SA 3.0 · Wikimedia Commons
Type
Stratovolcano
Country
Japan
Region
Western Pacific / Ryukyu Volcanic Arc
Elevation
555m
Coordinates
29.465, 129.594
Last eruption
Unknown
Tectonic setting
Subduction zone / Oceanic crust (< 15 km)
Landform
Composite
Major rock type
Andesite / Basaltic andesite
Geological summary

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.

From Wikipedia

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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Eruption history

Glossary

Detailed timeline

No eruption records available.

Nearby volcanoes

External links

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