Havre Seamount Explained
| Havre Seamount |
| Depth: | 720-2NaN-2 |
| Height: | 1030-2NaN-2 |
| Pushpin Map: | Oceania |
| Relief: | yes |
| Location: | South Pacific Ocean |
| Group: | Kermadec Islands |
| Coordinates: | -31.11°N -179°W |
| Country: | New Zealand |
| Type: | Seamount |
| Last Eruption: | July 2012 |
Havre Seamount is an active volcanic seamount lying within the Kermadec Islands group of New Zealand, in the south-west Pacific Ocean, on the Tonga-Kermadec Ridge.[1] Its most recent eruption took place in July 2012.[2]
See also
Notes and References
- Knafelc . J. . Gust . D. . Bryan . S. E. . Anderson . M. . Cathey . H. E. . Petrogenesis of Havre Volcano in the Kermadec Arc: 2012 Eruption of a Chemically Homogeneous Rhyolite . Frontiers in Earth Science . 2022 . 10 . 10.3389/feart.2022.886897 . 2022FrEaS..10.6897K . As most volcanoes in the Kermadec rear-arc are inactive, Havre and Giggenbach are both classified as active rear arc volcanoes . free .
- Havre Seamount. 242005. 2021-06-28.
