Lewati ke konten utama

Vanuatu · Stratovolkan

North Vate

Nguna-Emau

Tipe
Stratovolkan
Ketinggian
589 m
Letusan terakhir
Tidak diketahui
Nguna Island, along with Pele and Emau Islands, lie north of Efate Island (also known as Vate). Submarine calderas of varying dimensions have been hypothesized to occur in the North Vate area, and late-Pleistocene to Holocene eruptions have constructed cones with well-preserved craters.
Nguna Island, along with Pele and Emau Islands, lie north of Efate Island (also known as Vate). Submarine calderas of varying dimensions have been hypothesized to occur in the North Vate area, and late-Pleistocene to Holocene eruptions have constructed cones with well-preserved craters. · Foto: Photo by Karoly Nemeth (Massey University).
Tipe
Stratovolkan
Negara
Vanuatu
Wilayah
Pasifik Barat Daya / Vanuatu Volcanic Arc
Ketinggian
589 m
Koordinat
-17.452, 168.353
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Zona subduksi / Kerak menengah (15-25 km)
Bentuk lahan
Komposit
Batuan utama
Basal / Pikrobasal

Ringkasan geologi

Teks asli bahasa Inggris

The islands of Nguna, Pele, and Emau (or Emao), north of Efaté Island (also known as Vate), have been variously mapped as Pleistocene and Pleistocene to Holocene.

Kutipan dari Global Volcanism Program, Smithsonian Institution · Baca ringkasan lengkap di GVP →

Riwayat letusan

Glosarium

Garis waktu rinci

Tidak ada catatan letusan.

Gunung api terdekat

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.