Return to the Main Page
 
http://www.huttoncommentaries.com/Bulletins/images/THCEmailLogo580.gif
July 15, 2010
http://www.huttoncommentaries.com/Bulletins/images/Subscriber_bar190.jpg
http://www.huttoncommentaries.com/Bulletins/images/Volcano_bar190.jpg
http://www.huttoncommentaries.com/Bulletins/images/PoleMotion_bar190.jpg

A LONG OVERDUE ERUPTION
OF
TAUPO COULD BE
DEVASTATING TO NEW ZEALAND



 http://www.virtualoceania.net/newzealand/maps/volcanoes.gif
Recent scientific work indicates that the Earth's crust below the Taupo Volcanic Zone may be as little as 16 kilometres thick. A film of magma 50 kilometres (30 mi) wide and 160 kilometres (100 mi) long lies 10 kilometres under the surface.  The geological record indicates that some of the volcanoes in the area erupt infrequently but have large, violent and destructive eruptions when they do. There is also some possible rifting in the Taupo Volcanic Zone.



http://www.new-zealand-travel.org/images/north-island/lake-taupo-lrg.jpg


Lake Taupo is situated in a volcanic region of the north island and is steeped in Maori heritage and tradition. The lake was produced as a result of the most ferocious volcanic eruption in the past 5000 years - its ash drifted as far as Europe and China. Maori tradition explains the lake's origins differently - they believe that Ngatoirangi, the chief priest of the Arawa people, discovered the basin dry and caused it to flood into a lake when he attempted to plant a forest through hurling a tree at the ground. The lake itself and its surrounding areas boast a wide range of activities for tourists to enjoy including exploration of the volcanoes (including Mount Ngauruhoe which featured as Mount Doom in the 'Lord of the Rings' trilogy), participating in some world-class fishing, or adventurous and energetic watersports such as white water rafting, jet boating and parasailing.

More follows, however...




The remainder of this Hutton Commentaries Bulletin may contain copyrighted material, and only registered subscribers are allowed to view its full contents.

If you are a registered subscriber and are seeing this message, it most likely means that you are not yet logged into the website. Please use the Log-in button below to log into the site and then click on the bulletin link again.

If you would like to become a subscriber, so that you too can have access to potentially copyrighted portions of these bulletins, please go to our registration page.

   
Subscribers:  

Login