To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Havre Seamount

From Wikipedia, the free encyclopedia

Havre Seamount
Satellite image of 2012 eruption
Location of Havre Seamount in Oceania
Summit depth720 m (2,400 ft)
Height1,030 m (3,400 ft)
Location
LocationSouth Pacific Ocean
GroupKermadec Islands
Coordinates31°07′S 179°00′W / 31.11°S 179.00°W / -31.11; -179.00
CountryNew Zealand
Geology
TypeSeamount
Last eruptionJuly 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

References

  1. ^ Knafelc, J.; Gust, D.; Bryan, S. E.; Anderson, M.; Cathey, H. E. (2022). "Petrogenesis of Havre Volcano in the Kermadec Arc: 2012 Eruption of a Chemically Homogeneous Rhyolite". Frontiers in Earth Science. 10. Bibcode:2022FrEaS..10.6897K. doi:10.3389/feart.2022.886897. As most volcanoes in the Kermadec rear-arc are inactive, Havre and Giggenbach are both classified as active rear arc volcanoes
  2. ^ "Havre Seamount". Global Volcanism Program. Smithsonian Institution. Retrieved 28 June 2021.


This page was last edited on 20 December 2023, at 02:04
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.