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Aorounga Crater 3DPlanetary and Space Science Centre (PASSC) University of New Brunswick, Canada
Image by: Dr. Carlos Roberto de Souza Filho

Nov 16, 2006
Aorounga Crater

Satellite radar images of the Sahara desert north of Chad have revealed the presence of craters not easily noticed in normal aerial photographs. But the cause of these formations may lie outside the lexicon of standard geology today.

The Aorounga crater in the three-dimensional image above is almost 19 miles (31 kilometers) in diameter. And it does not stand alone in the Saharan desert. Its coordinates are, N 19° 6' E 19° 15', while the Kebira structure we discussed earlier can be found at N 24° 30' E 25° 0'. Both craters lie within an area of chaotic terrain that closely resembles the surface of Mars. (See Google Map) Another formation, the Oasis crater, can be seen slightly west of Kebira in the satellite image.

Some of the more interesting aspects of Aorounga are the "implausible" parallel grooves and ridges that run through the surrounding landscape, as well as through the crater itself. Wallace Thornhill and other advocates of the "Electric Universe" see these as one of the more common signatures of electrical arcing on rocky bodies in the solar system. The deep gouges and scalloped cliffs are reminiscent of Martian features that electrical theorists identify as scars left by electric arcs. The crater pattern is also eerily similar to the unexplained “pedestal craters” on Mars imaged by NASA orbiters—even the floors of many such craters stand higher the surrounding terrain. (Example from the Mars Global Surveyor seen here.)

The press release from Boston University listed the Kebira formation as “millions of years old”, corresponding to the dates fixed for other areas of the Gilf Kebir Plateau. But, is that the case? Could intense electromagnetic bombardment influence the apparent age accepted by the scientific community?

The most common dating method is by measuring the isotopic ratios of particular elements. For example, uranium 235 decays into lead 207 with a half-life of 700 million years. That means, when the rock was first formed, it contained a fixed quantity of uranium 235 and every 700 million years thereafter it will exhibit half the amount of uranium 235 and an increasing amount of lead 207.

Because a mineral sample’s age depends on that sample existing today exactly as when it was initially formed, if it has been affected by radioactivity, or heat, or a blast or electricity, any measurement of its age will be inaccurate. Therefore, if a multi-billion joule electric discharge, sufficient to excavate a crater 19 miles in diameter were to strike the earth, the gamma and x-ray pulses would drastically alter the decay rate, the isotopic ratios and, perhaps, form new elements within the rocks.

For these and other reasons presented in these Pictures of the Day, it is not unreasonable to ask if Kebira and its surrounding craters may be the remains of electrical events, perhaps occurring in a more recent past than geologists have previously imagined.

By Stephen Smith

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The Electric Sky and The Electric Universe available now!


Authors David Talbott and Wallace Thornhill introduce the reader to an age of planetary instability and earthshaking electrical events in ancient times. If their hypothesis is correct, it could not fail to alter many paths of scientific investigation.

More info

Professor of engineering Donald Scott systematically unravels the myths of the "Big Bang" cosmology, and he does so without resorting to black holes, dark matter, dark energy, neutron stars, magnetic "reconnection", or any other fictions needed to prop up a failed theory.

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In language designed for scientists and non-scientists alike, authors Wallace Thornhill and David Talbott show that even the greatest surprises of the space age are predictable patterns in an electric universe.

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David Talbott, Wallace Thornhill
Steve Smith, Mel Acheson
  CONTRIBUTING EDITORS: Dwardu Cardona, Ev Cochrane,
C.J. Ransom, Don Scott, Rens van der Sluijs, Ian Tresman
  WEBMASTER: Brian Talbott

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