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Akusekijima

Stratovolkan · Japan · 555 m

Akusekijima is seen from the N with the Omune lava flow forming a plateau in the foreground. The dacitic lava flow, the youngest featute, has experienced little erosion and lacks overlying tephra layers, suggesting a young age. Akusekijima is located in the southern Ryukyu Islands, and consists of the two older Biroyama and Nakadake edifices. The Mitake lava dome (right) forms the high point of the small 2.5 x 3.2 km island.
Akusekijima is seen from the N with the Omune lava flow forming a plateau in the foreground. The dacitic lava flow, the youngest featute, has experienced little erosion and lacks overlying tephra layers, suggesting a young age. Akusekijima is located in the southern Ryukyu Islands, and consists of the two older Biroyama and Nakadake edifices. The Mitake lava dome (right) forms the high point of the small 2.5 x 3.2 km island. · Foto: Copyrighted photo by Shun Nakano, 2004 (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
Tipe
Stratovolkan
Negara
Japan
Wilayah
Pasifik Barat / Ryukyu Volcanic Arc
Ketinggian
555 m
Koordinat
29.465, 129.594
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Subduction zone / Oceanic crust (< 15 km)
Bentuk lahan
Composite
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

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.

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