Nikkō Seamount
Nikko
Stratovolcano · Japan · 392m (submarine)

- Type
- Stratovolcano
- Country
- Japan
- Region
- Northwestern Pacific Volcanic Regions / Mariana Volcanic Arc
- Elevation
- 392m (submarine)
- Coordinates
- 23.078, 142.326
- Last eruption
- Unknown
- Tectonic setting
- Subduction zone / Crustal thickness unknown
- Landform
- Composite
- Major rock type
- Basalt / Picro-Basalt
Geological summary
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.
From Wikipedia
Nikkō Seamount is a submarine volcano in the Volcano Islands region of Japan. It is the southernmost volcano of Japan.
Wikipedia · CC BY-SA · Read full article →
Eruption history
Detailed timeline
- 1979VEI 0Geological estimate1979-07-12 – Ongoing
External links
⚠ For reference only. Not for emergency response.