Meta Research Bulletin ©2006
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Evidence that Mars is a former moon |
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Much less massive than any planet not itself
suspected of being a former moon |
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Orbit has eccentricity of near 10%, as would be
expected for an escaped moon. |
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Spin is slower than larger planets, except
where a massive moon has intervened (Mercury escaped from Venus; Moon robbed
Earth of original 2-4 hour spin rate.) |
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Large offset of center of figure from center of
mass – common for moons, not for planets |
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Shape not in equilibrium with spin, indicating
reshaping by some cataclysm |
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South hemisphere is saturated with craters, the
north has sparse cratering – indicates either a removal mechanism in the
north or a massive cratering event in the south |
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The crustal dichotomy boundary is nearly a
great circle – indicates that something nearby but external to Mars and
short-lived devastated half the planet |
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North hemisphere has smooth, 1-km-thick crust;
rough southern crust is up to 20-km thick – suggests massive bombardment of
the south half from a planet-sized source |
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Crustal thickness in south decreases gradually
toward hemisphere edges – consistent with external event, but not a local one |
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Lobate scarps occur near hemisphere divide,
compressed perpendicular to boundary – indicates that impacts near the
hemisphere boundary were extreme grazers |
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Huge volcanoes
arose where uplift pressure from mass redistribution following pole change is
maximal – consistent with present shape not being in equilibrium |
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Sudden 90° geographic pole shift occurred – as
would happen if a great mass were added to one hemisphere centered on Mars
equator, causing planet to tip over |
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Much of original atmosphere has been lost – as
would result from a major cataclysm |
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A sudden, massive flood with no obvious source
occurred – cataclysm may have brought the water from oceans on the source
body |
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Xe129, a fission product of massive
explosions, has an excess abundance on Mars |
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Crustal magnetization in southern highlands is
weak to absent in northern lowlands |
The box summarizes
evidence that Mars was not an original planet, but rather a moon of a
now-exploded planet occupying that approximate orbit. Many of these points are
the expected consequences of having a massive planet blow up nearby, thereby blasting
the facing hemisphere and leaving the shielded hemisphere relatively unscathed.
Especially significant in this regard is the fact that half of Mars is
saturated with craters, and half is only sparsely cratered. Moreover, the
crustal thickness has apparently been augmented over one hemisphere by up to 20
km or so, gradually tapering off near the hemisphere boundaries. This “crustal
dichotomy” is also readily seen in Martian elevation maps, such as in Figure
11 (source: [[19]]).