Seismic stations located on islands in the Pacific Ocean are increasingly showing signs of continuous harmonic tremors, an indication of sloshing magma.  While explainable as an isolated occurrence on a single heliplot, when five different stations in the central Pacific Ocean report similar activity at the same time, it is worth noting.

The Zetas have explained that the Pacific Plate consists of not one, but four distinct plates.  These plates boundaries as illustrated below are based on the Zetas descriptions.

"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!" ZetaTalk: Folding Pacific

Johnston Island, Pacific Ocean (current heliplot)

Kiritimati Island, Republic of Kiribati (current heliplot)

Wake Island, Pacific Ocean (current heliplot)

Midway Island, Pacific Ocean (current heliplot)

Pitcairn Island, South Pacific (current heliplot)

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Comment by Howard on January 5, 2013 at 10:20pm

Analysis of the 15 tsunami buoys triggered into event mode from today's severe quake in Alaska shows a plate adjustment  that primarily affected what the Zetas have defined as the East Pacific Plate.

"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."

Although the quake epicenter was located near the coastal British Columbia border, the most volatile water displacements were reported at 3 buoys that comprise a triangle on the northern half of the East Pacific Plate.  If Alaska is being pulled toward Mexico causing the diagonal stress across N. America, the rock strata that formerly supported this bowing stress has yielded to some extent as a result of today's quake.  It would stand to reason that some of this bowing stress has likewise been transferred further eastward, increasing the stress along the weak points in the New Madrid and St. Lawrence Seaway.

It should also be noted that the last time this many tsunami buoys were in event mode, which included buoys in both the Pacific and Atlantic Oceans, was the great 9.5 quake in Japan during March 2011, which was called a 7.9 by USGS until it became patently obvious that the resulting devastation would clearly refute such a conspicuous downgrade.

Station 51407 (Hawaii)

Station 46413 (Alaska)

Station 46404 (Oregon)

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