| Monowai Seamount | |
|---|---|
| Summit depth | 132 metres (433 ft)[1] |
| Location | |
| Location | North of the Kermadec Islands; south of Tonga |
| Coordinates | 25°53′13″S 177°11′17″W / 25.887°S 177.188°W |
| Country | New Zealand |
| Geology | |
| Last eruption | 2011 |
Monowai is a volcanic seamount to the north of New Zealand. It is one of the most active volcanoes in the Kermadec volcanic arc.
The most recent eruptions were in 2008[2] and 2011.[3]
The summit is approximately 132 metres (433 ft)[1] below sea level, considerably above the level of the nearby Tonga and Kermadec Trenches. The summit's position and depth changed between 1998 and 2004, due to a landslide and eruptive regrowth. A 1500 metre deep caldera, 13 by 8 km, lies 5–15 km NNE of the seamount's main cone.
| This article about the geography of New Zealand's outlying islands is a stub. You can help Wikipedia by expanding it. |
| This article about a specific oceanic location or ocean current is a stub. You can help Wikipedia by expanding it. |
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)