Orca wrote:But honestly, how many Mars-like objects could just be flying around? Anything that large, I would think, would have had to have formed in a stable orbit from which it would not likely stray too far.
Orca wrote:My instinct tells me that the Mars-crash is unlikely. I realize that in science my instinct isn't worth a flying dingo's kidney; however, I just can't shake the feeling.
But honestly, how many Mars-like objects could just be flying around? Anything that large, I would think, would have had to have formed in a stable orbit from which it would not likely stray too far.
Chris Peterson wrote:Orca wrote:My instinct tells me that the Mars-crash is unlikely. I realize that in science my instinct isn't worth a flying dingo's kidney; however, I just can't shake the feeling.
I would think a flying dingo would be worth a lot- even just its kidney, maybe.
http://en.wikipedia.org/wiki/Goofy wrote:
<<The Goofy holler is a stock sound effect that is used frequently in Disney cartoons and films.
It is the cry Goofy makes when falling or being launched into the air,
which could be transcribed as "yaaaaaaa-hoo-hoo-hoo-hooey!!"
The holler was originally recorded by yodeller Hannès Schrolle for the 1941 short The Art of Skiing.
Some sources claim that Schrolle was not paid for the recording.>>
http://www.youtube.com/watch?v=YOjOD1OmioY
Chris Peterson wrote:In the early Solar System nothing was in stable orbits (nothing is in a truly stable orbit even now). There is strong evidence that planets were moving in an out, swapping positions, and that collisions between large bodies were common. The idea that a Mars-sized planet collided with the Earth during this early chaotic period is pretty reasonable.
Orca wrote:Well perhaps "stable" was not a good word. I meant, "formed and solid enough that they'd [the planets] collected the local material around them. The point that they wouldn't be crossing orbits with other similar-sized objects.
But then it all goes back to the amount of mass in the early-formed solar system compared with the mass of the system today. Of course the current total has to be much smaller than the initial nebula and also smaller in the total number of objects in the early years after formation compared to today.
Aren't there examples of moons forming along side their parent planets...such as in the Jovian and Saturnian systems? It would appear that there are several mechanisms that can create moons.

How old is the Moon? Almost the entire Solar System formed 4.6 billion years ago, when the solar nebula collapsed. But astronomers think that the Moon formed later than that, when a Mars-sized protoplanet smashed into the Earth. The debris from the collision splashed into orbit around the Earth and then reformed into the Moon, which still orbits us today.
So when did this happen?
Astronomers think this collision happened about 4.53 billion years ago, about 30-50 million years after the rest of the Solar System formed. This was relatively soon after the formation of the Solar System, and well before the time when life formed on Earth. Our planet was probably still mostly a molten ball of rock, and the impact of the Moon did little to change that. This is the dominant theory of how the Moon formed, but there are others. It's possible that the Moon was captured by the Earth's gravity, or it just formed in place around the Earth after the formation of the Solar System.
Orca wrote:However, what about the argument of the density of the Moon? The idea is, if I understand it, that the since the Moon has a lower average density, it might be made of the surface material ejecta from the Earth during the impact. However, wouldn't the density of the still-liquid Earth be more uniform than it is today, what with all the churning convection going on throughout the planet? I am sure much of the heavy material would have sank to the center, but still, I'd guess that the Moon would have actually had an average density closer to our own.
As for the idea that the Moon might have formed simultaneously, wouldn't the local cloud from which they both formed lean in density toward the biggest pocket - the one that formed the Earth - thus making its average density higher? In other words, the big bit would get most of the heavy material and thus form a planet with higher average density. But then, Chris, you'd guess the Earth and Moon would not have formed that way? Granted, we don't see any other examples...
bystander wrote:Age of the Moon
Universe Today - October 13, 2008How old is the Moon? Almost the entire Solar System formed 4.6 billion years ago, when the solar nebula collapsed. But astronomers think that the Moon formed later than that, when a Mars-sized protoplanet smashed into the Earth. The debris from the collision splashed into orbit around the Earth and then reformed into the Moon, which still orbits us today.
So when did this happen?
Astronomers think this collision happened about 4.53 billion years ago, about 30-50 million years after the rest of the Solar System formed. This was relatively soon after the formation of the Solar System, and well before the time when life formed on Earth. Our planet was probably still mostly a molten ball of rock, and the impact of the Moon did little to change that. This is the dominant theory of how the Moon formed, but there are others. It's possible that the Moon was captured by the Earth's gravity, or it just formed in place around the Earth after the formation of the Solar System.
dougettinger wrote:How is it possible that the collisional material created by the Earth and a hypothetical body the size of Mars could possibly accrete to form the Moon? Would not most of this material eventually fall back to Earth, be collected at Lagrangian points, or simply remain as collisional material in orbit much like the Asteroid Belt?
dougettinger wrote: Would not most of this material eventually fall back to Earth,
be collected at Lagrangian points
or simply remain as collisional material in orbit much like the Asteroid Belt?
dougettinger wrote:I wish to address issues with the Asteroid Belt once again. If Jupiter's gravity field perturbs and prevents the asteroids from combining, then why did Saturn in the next adjacent orbit form without being disturbed by Jupiter's gravity field?
Why did not other secondary planets occur at other Lagrangian points - especially Jupiter and Saturn? Why have not the asteriods at Jupiter's Lagrangian points been perturbed and collided with Jupiter?
What was the nature of the perturbation that caused the impactor to move toward and collide with Earth?
Would not the impactor's glancing blow have knocked Earth away from its orbit as predicted by Bode-Titius Rule?
Why are the bulk composites of the Moon and Earth quite different when they supposely formed from the same region of the solar nebula?
dougettinger wrote:Obviously, I am having difficulties with the impactor's origin.
Chris Peterson wrote:It is likely that there were other planets formed early in the development of the Solar System. This was a chaotic environment, with planets perturbing each other, transferring angular momentum, shifting orbital radii, changing position, and being flung out of the Solar System entirely. I think there was plenty of material to allow for collisions like that believed to have created the Moon.
Wayne wrote:The leading hypothesis is a formation in L4 or L5 of the Earth-Sun system. No chaotic orbits needed. Just a simple case of a body becoming too large to be stable in L4/L5.
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