Wednesday, June 25, 2008
New Study Confirms More Aspects of Mars Tidal Model
As you’ll recall, in 2001 Richard Hoagland and I published the Mars Tidal Model. In this extensive paper we argued that Mars was not a planet at all, but rather a moon of a now missing member of the solar system commonly called Planet V. We cited numerous lines of evidence supporting our hypothesis, including the existence of bands in Mars magnetic field comprised of alternating polarities. We argued that this magnetic banding was caused by multiple (and devastating) impacts to the Martian surface from high velocity debris released by the destruction of Planet V, Mars’ tidal locked parent body. In our scenario, the alternating bands of magnetic material were the result of standing P and S waves reverberating within the molten sea of material that made up the southern hemisphere of Mars below the line of dichotomy.
Now, new computer models have confirmed this aspect of our research. In several major news articles published today, three separate computer studies agree that the magnetic banding was caused by an asteroid impact. They argue that it was a single impact, rather than multitudes of them as our model suggests, but this is a minor point.
The news articles also maintain that this event took place at the dawn of the solar system, but this time frame is based on a bias that the more cratered southern hemisphere is older. According to the conventional geologic models of Mars’ formation, most impact events took place back in this time period because there was far more accretion debris in the solar system back then. Our model says exactly the opposite; that the more crated southern highlands below the line of dichotomy are a result of the pile-up of debris from the recent (65 MYA) destruction of Planet V.
This is just the latest in a series of observations and peer reviewed papers that have confirmed various aspects of the Mars Tidal Model.
More on the Mars Tidal Model can be found here.