posted on Oct, 5 2003 @ 01:36 PM
One theory that is bounced around astronomy circles (and one I find very interesting) regarding the origin of Mars moons involves a paleo-surface
impact of an asteroid.
Somewhere around 1 billion years ago, Mars contained a far denser atmosphere than currently. (Currenly, Mars has 1/100 Earth normal atmospheric
presure, almost a hard vaccuum. About 1 billion years ago, it is estimated to have had 1/3 to 1/2 earth normal atmospheric pressure. Also, judging
from the presence of "red bed" iron oxide formations known to exist on mars, it is assumed that this early atmosphere contained a far higher
concentration of oxygen)
According to the asteroid-impact theory, an asteroid impacted at a very oblique angle (flatter than 45 degrees). The resulting shock wave would have
ripped a significant percentage of the atmosphere out into orbit. In this model, Phobos and/or Deimos are thought to potentially be either large
chunks of crust that were flung out into orbit by the impact, or possibly portions of the original impactor.
The question comes up, if this is the case, where is the impact crater? An impact of such magnitude could easily penetrate the crust, releasing a
large quantity of magma, creating a "mare", filling in any possible impact features.