
14-November-2008, 08:51 PM
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Established Member
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Join Date: Aug 2008
Posts: 133
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Quote:
Originally Posted by dmr81
I didn't see anything about sunspots in that paper. Could you please quote the section to which you referred above?
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http://www.holoscience.com/news.php?article=36uyr9nx
Quote:
The missing link between the sunspots and earthquakes is the fact that the electric discharges to the Sun that cause sunspots can also affect the Earth's ionosphere. The ionosphere forms one "plate" of a capacitor, while the Earth forms the other. Changes of voltage on one plate will induce movement of charge on the other. But unlike a capacitor, the Earth also has charge distributed in rock beneath the surface. And if the subsurface rock has become semi-conducting because of stress, there is an opportunity for sudden electrical breakdown to occur through that rock. We should expect similar processes to occur underground as is found in atmospheric lightning. There will be precursor electromagnetic effects due to the small-scale travelling of charge – rather like "stepped leaders" between cloud and ground. That may be the limit of activity in small tremors. But in a large earthquake, the entire circuit may be involved, from below the Earth, through the atmosphere to the ionosphere. This would explain the massive disturbance of the ionosphere over a large area accompanying a major earthquake.
The mystery of the source of the current is solved – it comes from a charged Earth. And the link with sunspots via the ionosphere is exposed. Subterranean lightning causes earthquakes! Seismic waves are the rumble of underground thunder. The energy released may be equivalent to the detonation of many atomic bombs but only a small proportion need come from the release of strain in the rocks. Most of it comes from the Earth's stored internal electrical energy.
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Quote:
Originally Posted by dmr81
In which post?
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The Expansion of Ganymede
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"The most likely site for error is in the most fundamental of our beliefs." -- Samuel Warren Carey, geologist, 1988
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