T
tdamskov
Guest
Hm. I think you're right that things might be complicated but perhaps in even more interesting ways. How about this... Here's a moon that's primarily composed of H2O and CO2 ice. Very high albedo as seen towards the poles. Along comes disintegrated carbonaceous object / or Saturnian primordial ring which deposits a fairly thick pile of dust on one side, mainly on the equator. This stuff is almost like tarry sand. Subsequent cratering of the equatorial dustpile (evident from the images) ballistically disperses quite a bit of this dusty material further towards the poles, primarily collecting in hollows of craters. Perhaps the tarry dust/sand material tends to stick together slightly when it's heated by the sun? That might account for the sharp black/white edges. It might even bake out gases (Vogon's colouring agent) which would expand around the dust puddles.<br /><br />The subsequent dispersal of the dusty material would also account for the extremely rounded and soft terrain around the equator. However, what worries me is the fact that I see no "revealing" craters on higher latitudes where the impacts have dug away the dust to show pure ice below. Then again, impacts into the ice would create temporary clouds of gas (vaporized ice and co2) and the resulting winds might be able to carry enough dust to partially cover the recent crater with a thin layer.