We now have the first density estimate of it from Cassini -- and it appears
that we have yet ANOTHER icy rubble pile. The estimate: 0.6 grams/cc.
Also, the surface is now officially recognized as very weird, in a way that
suggests that it is in no way a solid world:
http://ciclops.org/view.php?id=1192
Obviously Hoagland is calling the wrong moon an alien artifact
Actually, those strange, small, relatively uniformly-sized and dark-centered craters on Hyperion bear a disturbing resemblance to the similar surface pits observed on Helene in Charles Sheffield's novel "The Ganymede Club" -- in which Helene turns out to be a Sinister Alien Artifact that does Horrible Things to the investigating astronauts.
The real problem with landing on Hyperion, however -- as pointed out by Poul Anderson in his story "Scarecrow" -- is that, given its chaotic rotation, its surface will be sliding around horizontally undeneath a descending lander at entirely unpredictable speeds and directions. (The main subject of the story, believe it or not, is the development of religion among intelligent machines.)
At any rate, now we know: Hyperion's non-spherical shape comes not from (as so many of us assumed) the fact that it's a solid moon that has had big chunks knocked off it by impacts, but from the fact that the whole moon is a
loosely bound and tidally distorted clump of small debris like Saturn's
innermost moons. Obvious question: where did the debris that accreted to
make Hyperion come from? Is it the finely shattered remnants of a single
solid moon that was originally near that orbit? Or have complex gravitational
interactions (mostly from Titan) caused debris from elsewhere in the Saturn
system to accumulate in a 3:4 resonance orbit with Titan and re-accrete
there into a rubble-pile moon?
Ok here's one that might be hard to swallow.
I think Hyperion is a captured comet.
If we're accepting *any* captures as the origin of outer planetary moons (as opposed to a mini solar accretion disk) then surely comet/cometoid bodies are quite likely to be captured - there's lots of 'em, and they have orbits which mess with the gas giants on a regular basis (bet the Jovian Trojans are cometoids!). We saw evidence in the Jupiter system of crater chains from disrupted comets, as well as an actual disrupted comet impact, and as for the first port of call when Cassini hit Saturn's outer suburbs...
...but - and it's a b-i-g BUT: wouldn't we preferentially see these guys on the outer fringes of the systems which they've come to inhabit, not slam-bang up against the planets? The orbital mechanics surrounding a d-i-s-t-a-n-t capture are going to be much more benign than something just above the clouds (well, almost!).
Maybe there's a size thing going on, with some ancient KBO population being captured and preserved in almost the inner Solar System while their brethren were gradually pumped out - or in - and only standard-sized comets were left...
What about disintegrative capture? If, several billion years ago, an unassuming icy planetesimal on its way through the Saturn system happened to pass within Titan's Roche limit, would Titan have been able to break it up?
From what I remember of disintegrative capture, the fragments of the disrupted body end up leaving the vicinity of the primary body (here Titan) with a pretty large velocity distribution. There is also a lot of dissipation due to internal friction and gravitational interaction of the fragments during the breakup, which means that any debris trapped in Saturnian orbit wouldn't necessarily end up crossing Titan again. One would expect that at least _some_ of the debris would end up in the 4:3 resonance. (Any stuff that didn't end up in a stable resonance would probably end up beating the heck out of Titan and Saturn's other moons.)
The debris that would be "slowed down" the most during the disintegration would be the stuff on the Titan facing side. If Titan's upper atmosphere got involved this effect would of course be even more pronounced. If the planetesimal was differentiated this could in part explain the low density of the material captured by Saturn... it would be mostly ice.
I have absolutely no idea whether this hypothesis is even remotely feasible from a dynamical standpoint. (Hope I'm not getting any of the basic facts about disintegrative capture wrong. It's been about seven or eight years since I last read up on it.)
Cheers
Rob
Rob:
Seems reasonable - and presumably would also work in other gas-giant systems with large moons. I'd still like it if some o-o-o-o-ld material could have survived!
I still wonder about the Jovian Trojan Asteroids...
Bob Shaw
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