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Jepang · Kaldera

Kita-Bayonnaise

Tipe
Kaldera
Ketinggian
360 m (bawah laut)
Letusan terakhir
Tidak diketahui
The submarine topography of the 6-7 km Myojin Knoll caldera is seen in this SeaBeam image viewed from the SW. The white line marks the E-W track of the survey vessel. A voluminous deposit of coarse pumice from the caldera-forming eruption mantles the caldera rim and its outer flanks. A post-caldera lava dome rises 250 m above the caldera floor.
The submarine topography of the 6-7 km Myojin Knoll caldera is seen in this SeaBeam image viewed from the SW. The white line marks the E-W track of the survey vessel. A voluminous deposit of coarse pumice from the caldera-forming eruption mantles the caldera rim and its outer flanks. A post-caldera lava dome rises 250 m above the caldera floor. · Foto: Image by Fumitoshi Murakami (Geological Survey of Japan, courtesy of Richard Fiske, Smithsonian Institution).
Tipe
Kaldera
Negara
Jepang
Wilayah
Pasifik Barat Laut / Izu Volcanic Arc
Ketinggian
360 m (bawah laut)
Koordinat
32.100, 139.850
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Zona subduksi / Kerak samudra (< 15 km)
Bentuk lahan
Kaldera
Batuan utama
Riolit

Ringkasan geologi

Teks asli bahasa Inggris

The large submarine Kita-Bayonnaise (North Bayonnaise) submarine caldera, also known as Myojin Knoll, lies between the Aogashima and Myojinsho (also called Beyonesu Rocks) calderas about 300 km SSE of the Izu Peninsula.

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

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