Lewati ke konten utama

Jepang · Stratovolkan

Akusekijima

Tipe
Stratovolkan
Ketinggian
555 m
Letusan terakhir
Tidak diketahui
Akusekijima
Foto: 名古屋太郎 · CC BY-SA 3.0 · Wikimedia Commons
Tipe
Stratovolkan
Negara
Jepang
Wilayah
Pasifik Barat / Ryukyu Volcanic Arc
Ketinggian
555 m
Koordinat
29.465, 129.594
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Zona subduksi / Kerak samudra (< 15 km)
Bentuk lahan
Komposit
Batuan utama
Andesit / Andesit basaltik
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.

Ringkasan Wikipedia

Ringkasan Inggris

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.

Wikipedia · CC BY-SA · Baca artikel lengkap →

Riwayat letusan

Glosarium

Garis waktu rinci

Tidak ada catatan letusan.

Gunung api terdekat

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.