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ZetaTalk: Folding Pacific

Written November 20, 2010

Could you explain a little more about the pacific 'folding' ? It's a big ocean. Will it 'fold' more or less the same from the northern to southern hemisphere and does the folding process create events unique to itself or will these be minor compared to the shift events.

We addressed the fact that the Pacific plate is not one plate, as assumed. In fact, it is at least four plates. The rise and incident of islands from Kamchatka to Hawaii to the Society Islands shows this to be a plate boundary, down the center of the Pacific. Call that land to the east of this plate boundary the East Pacific Plate. There is also a triangle of a plate between the points of Hawaii, West Samoa, and the Society Islands. Call this the West Pacific Plate. Below the Society Islands is a plate which could be called the South Pacific Plate. And the portion of the Pacific Plate pushing under Japan and pushing under the Philippine Plate could be called the North Pacific Plate. All these plates are folding now, as a close examination of the live seismographs shows. Take a look at where magma sloshing is ongoing!

What we refer to as the folding Pacific is more than this, however. It is primarily the plates abutting Asia. The Mariana Trench will collapse against the tiny Mariana Plate which will tilt and fold to push under the Philippine Plate. The Philippine Plate is likewise tilting to fold and push under the tongue holding Indonesia, which is itself buckling and sinking. Where the Pacific plates are almost constantly adjusting, the north and west Pacific plates riding over the east and south Pacific plates, this is silent and virtually unnoticed by man, who cannot place his monitors under the deep sea. Hawaii is known to be steadily rising, however, as a result of this. Thus, when we refer to a folding Pacific, we are referring to the plates tilting and folding against Indonesia and Japan.

Written November 27, 2010

I was hoping to know a little more detail regarding "the folding of the pacific". It seems the Mariana Trench as the most likely point where this "Fold" occurs. Will this folding cause the Philippine Plate to rise on its eastern side? Seems a lot of elevation in the Philippines eastern ridge - would these rise further or will the drop in the tongue as described prevail - nullifying the folding effect?

The folding of the Pacific plates that accompany the sinking of Indonesia during the 7 of 10 scenarios involves, as we have explained, the Mariana and Philippine plates tilting and flattening westward. This is nothing more than an existing trend, so is just a matter of the plates moving along faster in the direction they are already going. The Mariana Trench is a zone where the Pacific Plate is subducting under the Mariana Plate. The Pacific Plate curves down at this point, plunging under the Mariana Islands which ride on the Mariana Plate. The trench will be suddenly closed, so that rather than a trench there will be the Pacific Plate scraping along the Mariana Plate, and giving the Mariana Islands a temporary boost up as the plate tilts during this process. The Mariana Plate, thus tilted, will slide its western edge down along the Philippine Plate, as the Mariana Plate subducts under the Philippine Plate and this process will now be accelerating. The Philippine Plate likewise tilts its eastern side up, dropping its western side down. The exaggerated tilt accelerates the subduction of the Mariana Plate, and also accelerates the subduction of the Philippine Plate under the tongue holding Indonesia. The tilting of the Philippine Plate give the Philippine Islands a temporary boost up also, as these islands ride on the eastern edge of the tongue holding Indonesia. Meanwhile, the tongue holding Indonesia has been plunged down, ultimately pulling both the Mariana and Philippine plates down as they fold so the Mariana Islands do not have a permanent boost in elevation. Nancy has explained this as a deck of cards, scattered on a table top, being pulled together into a deck. The plates are folded against one another.

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