Return to the Main Page
 
http://www.huttoncommentaries.com/Bulletins/images/THCEmailLogo580.gif
February 22, 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

WAS SOUFRIERE HILLS ACTIVITY OF FEBRUARY 11 THE SIGNAL?


THC is still waiting for a signal for the beginning of a sequence of earthquakes and their effects predicted to occur in the western states, and also elsewhere in the southern hemisphere.
If there are the greater activities in the Vesuvius, or Pelee, then the southern coast of California - and the areas between Salt Lake and the southern portions of Nevada - may expect, within the three months following same, an inundation by the earthquakes.

But these, as we find, are to be more in the southern than in the northern hemisphere.


(270-35; January 21, 1936)
And considering that the volcanoes of Vesuvius and Pelee (on the Caribbean island of Martinique) are dormant, perhaps Soufriere Hills volcano, about 140 miles from Martinique, is a surrogate for Pelee.

Was the recent strong activity of Soufriere Hills the signal that THC has been anticipating? Maybe not. 

The activity on February 11 was related mainly to a collapse of the volcano dome on Montserrat.  But this collapse was produced by the extreme activities of the vulcanian eruptions of the day.  What produced them?  Deeper magma-flow activities.  What could such deeper flows imply? That Earth's crust at the eastern edge of the Caribbean tectonic plate is beginning to respond to deep magma flow, and that such flow there might lead to deep magma flows and earthquakes along weak spots in the crust elsewhere. Thus, this volcano may be a sign for the reactivation of Earth's magma surge channels, as discussed on pages 98-102 of our book, Earth's Catastrophic Past and Future, Universal Publishers, 2004.

Here below is the latest on the degree of "greater activities" at Soufriere Hills. 

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