icon Antartic Ice Fractures

On Nov 27, 2004 the Zetas described the Earth wobble that had begun in 2004 as a result of Planet X pushing daily at the magnetic N Pole of Earth.

The polar wobble that began in November is the first sign of the Earth’s participation in the slow 270° Roll that Planet X does to position itself, magnetically, above the Ecliptic rather than below the Ecliptic. It is caused, as we explained, by the magnetic N. Pole of Earth avoiding any exposure to the emerging N. Pole of Planet X. As the Earth normally rotates around its geographic N. Pole, the magnetic N. Pole is exposed for half the day, and then hidden for the other half of the day. This initially results in a Drunken Lurch to push the magnetic N. Pole out of view, a twice a day polar wobble, but rapidly evolves into twirl. This is due to the magnetic N. Pole being either to the right or left of the geographic N. Pole as the globe turns, responding to the emerging hose of magnetic particles from the N. Pole of Planet X as it turns about, in place.
ZetaTalk Twirling into Darkness, written Nov 27, 2004

Where the Figure 8 of the daily wobble was documented by observation of the position of constellations and the Azimuth of sunrise and sunset locations, there are other indicators of the increasing force of the daily polar wobble. For instance the twice daily fracture quakes in the Antartica ice. Note that per the Zetas Planet X arrived into the inner solar system in 2003, and these twice daily ice quakes have been occurring since 2003.

Something's Shaking in Antarctica
June 4, 2008
Scientists have discovered massive, slow-motion "ice quakes" trembling twice a day through the West Antarctic Ice Sheet, an Alaska-sized swath of Antarctica. Detective work has traced the source of the shaking to the Whillans Ice Stream, a glacier 100 kilometers across and 1 kilometer thick, which flows from the ice sheet's interior. It may seem strange that magnitude-7 quakes went unnoticed for so long--a temblor of similar size leveled entire towns and killed at least 15,000 in Turkey in 1999--but people standing on the Whillans Ice Stream never notice the shaking. Finding the causes of ice quakes--which also occur in Greenland--could lead to better understanding glacial movement and improved models of how glaciers will respond to climate change, says Robert Bindschadler, a glaciologist at NASA Goddard Space Flight Center in Greenbelt, Maryland, who first reported the twice-daily surges of the Whillans Ice Stream in 2003. "What has come from these discoveries is a realization that glaciers have other modes of behavior than we have thought of previously," says Göran Ekström, a seismologist with Columbia University.