Good point. Does anyone know?The question I'd have for a recent collision is how likely that makes the current configuration; in particular, how circular is Charon's orbit (or rather, the mutual orbit) as well as how long it would take for the two to become tidally locked after such a collision.
Good point. Does anyone know?
On another matter, surely the relative recency of the end-Cretaceous impact, which involved a body a mere few miles in diameter, tells us nothing about the probability of a recent much larger impact, splitting a dwarf planet apart to produce Charon, which must have involved a vastly larger impactor.
Good point. Does anyone know?
The question I'd have for a recent collision is how likely that makes the current configuration; in particular, how circular is Charon's orbit (or rather, the mutual orbit) as well as how long it would take for the two to become tidally locked after such a collision.
While I am by no means an expert, I don't think so. All of the angular momentum of the bodies needs to be dissipated; especially in a glancing collision I'd think the collision would add angular momentum to the individual bodies, not remove it.Gawdzilla Sama said:The question I'd have for a recent collision is how likely that makes the current configuration; in particular, how circular is Charon's orbit (or rather, the mutual orbit) as well as how long it would take for the two to become tidally locked after such a collision.
It could have happened immediately?
The question I'd have for a recent collision is how likely that makes the current configuration; in particular, how circular is Charon's orbit (or rather, the mutual orbit) as well as how long it would take for the two to become tidally locked after such a collision.
According to this article, once Charon has coalesced from the collision debris, it would have take for Charon only 50 years (no, not a typo) to become tide-locked, and several million years for Pluto to become also tide-locked.
An eyeblink on the scale of Solar System.
It's evidence against it, but not proof. It may not have been completely melted--chunks of it may have been, but other chunks may have been blasted off before they could have melted.Mark6 said:Some of Pluto's terrain appears to be billions of years old.
I find that most improbable. A very large moon is created by the disruption of a dwarf planet; but the impact leaves some mountains on that body (composed of water ice!) looking perfectly normal and undisturbed.It's evidence against it, but not proof. It may not have been completely melted--chunks of it may have been, but other chunks may have been blasted off before they could have melted.
I find that most improbable. A very large moon is created by the disruption of a dwarf planet; but the impact leaves some mountains on that body (composed of water ice!) looking perfectly normal and undisturbed.
What I'm thinking is this: Something (possibly the moon) smashes into the planet. Bits of both are blown into space--and some of them are pretty large, because the material is pretty weak (it's ice). While the stuff condenses into the Pluto/moon system, some of the chunks fall back into the system and are large enough to survive the impact.
It would explain the mountain in a moat: a chunk of material hit th planet and stuck. It may explain the dischordant facets of the planet as well.
Unlikely? Sure. But not impossible. Planets don't blow up uniformely, and if there were fractures (if Pluto had been softened up previously by collisions with things orbiting the impactor, perhaps?) they could easily be re-activated, lessing the amount of stress necessary to toss the chunk into space wholesale.
Cool. It's especially interesting to see the moons become worlds in their own right, when prior to this they were just single pixels in images.