Nikkō Seamount
Nikko
Stratovolkan · Japan · 392 m (bawah laut)

- Tipe
- Stratovolkan
- Negara
- Japan
- Wilayah
- Northwestern Pacific Volcanic Regions / Mariana Volcanic Arc
- Ketinggian
- 392 m (bawah laut)
- Koordinat
- 23.078, 142.326
- Letusan terakhir
- Tidak diketahui
- Kondisi tektonik
- Subduction zone / Crustal thickness unknown
- Bentuk lahan
- Composite
- Batuan utama
- Basalt / Picro-Basalt
Ringkasan geologi
Nikko submarine volcano is a massive seamount that rises from nearly 3 km depth to within 392 m of the ocean surface near the N end of the Mariana Volcanic Arc. Two large cones at the basaltic-to-andesitic volcano have been constructed on the NW and NE rims of a roughly 3-km-wide, flat-floored submarine caldera, whose rim is prominently displayed on the southern side, but largely buried on the north. A smaller cone is present on the SE caldera floor. The larger NW cone lies within a partially buried crater and displays hydrothermal activity. Discolored water was observed in July 1979, but none has been observed during semi-regular seasonal reconnaissance flights since then. Hydrothermal venting was documented during a NOAA expedition.
Ringkasan Wikipedia
Ringkasan InggrisNikkō Seamount is a submarine volcano in the Volcano Islands region of Japan. It is the southernmost volcano of Japan.
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Riwayat letusan
Garis waktu rinci
- 1979VEI 0Perkiraan geologi1979-07-12 – Berlangsung
Tautan eksternal
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